Item talk:Q139781
From geokb
{
"OpenAlex": {
"id": "https://openalex.org/A5040980912",
"orcid": "https://orcid.org/0000-0003-3286-4682",
"display_name": "Michael Manga",
"display_name_alternatives": [
"M. M. Manga",
"Manga Michael",
"Michael Manga",
"M. Manga",
"M Mai Manga",
"Michael M. Manga",
"Miachel Manga"
],
"works_count": 800,
"cited_by_count": 21265,
"summary_stats": {
"2yr_mean_citedness": 2.0285714285714285,
"h_index": 75,
"i10_index": 300
},
"ids": {
"openalex": "https://openalex.org/A5040980912",
"orcid": "https://orcid.org/0000-0003-3286-4682",
"scopus": "http://www.scopus.com/inward/authorDetails.url?authorID=7006760316&partnerID=MN8TOARS"
},
"affiliations": [
{
"institution": {
"id": "https://openalex.org/I4210087453",
"ror": "https://ror.org/007nzgd38",
"display_name": "Expedition (United Kingdom)",
"country_code": "GB",
"type": "company",
"lineage": [
"https://openalex.org/I4210087453"
]
},
"years": [
2024
]
},
{
"institution": {
"id": "https://openalex.org/I95457486",
"ror": "https://ror.org/01an7q238",
"display_name": "University of California, Berkeley",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I95457486"
]
},
"years": [
2024,
2023,
2022,
2021,
2020,
2019,
2018,
2017,
2016,
2015
]
},
{
"institution": {
"id": "https://openalex.org/I1302918504",
"ror": "https://ror.org/05vvg9554",
"display_name": "Planetary Science Institute",
"country_code": "US",
"type": "nonprofit",
"lineage": [
"https://openalex.org/I1302918504"
]
},
"years": [
2024,
2023,
2022,
2021,
2020,
2019,
2018,
2017,
2016,
2015
]
},
{
"institution": {
"id": "https://openalex.org/I4210154444",
"ror": "https://ror.org/05a18r864",
"display_name": "International Ocean Discovery Program",
"country_code": "NO",
"type": "other",
"lineage": [
"https://openalex.org/I4210154444"
]
},
"years": [
2024
]
},
{
"institution": {
"id": "https://openalex.org/I134446601",
"ror": "https://ror.org/02xewxa75",
"display_name": "Berkeley College",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I134446601"
]
},
"years": [
2024,
2023,
2013,
2009
]
},
{
"institution": {
"id": "https://openalex.org/I2803209242",
"ror": "https://ror.org/00pjdza24",
"display_name": "University of California System",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I2803209242"
]
},
"years": [
2023,
2015,
2009
]
},
{
"institution": {
"id": "https://openalex.org/I8204097",
"ror": "https://ror.org/05591te55",
"display_name": "Ludwig-Maximilians-Universit\u00e4t M\u00fcnchen",
"country_code": "DE",
"type": "education",
"lineage": [
"https://openalex.org/I8204097"
]
},
"years": [
2022
]
},
{
"institution": {
"id": "https://openalex.org/I122411786",
"ror": "https://ror.org/05dxps055",
"display_name": "California Institute of Technology",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I122411786"
]
},
"years": [
2021
]
},
{
"institution": {
"id": "https://openalex.org/I32971472",
"ror": "https://ror.org/03v76x132",
"display_name": "Yale University",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I32971472"
]
},
"years": [
2021
]
},
{
"institution": {
"id": "https://openalex.org/I130238516",
"ror": "https://ror.org/017zqws13",
"display_name": "University of Minnesota",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I130238516"
]
},
"years": [
2021
]
}
],
"last_known_institutions": [
{
"id": "https://openalex.org/I1302918504",
"ror": "https://ror.org/05vvg9554",
"display_name": "Planetary Science Institute",
"country_code": "US",
"type": "nonprofit",
"lineage": [
"https://openalex.org/I1302918504"
]
},
{
"id": "https://openalex.org/I95457486",
"ror": "https://ror.org/01an7q238",
"display_name": "University of California, Berkeley",
"country_code": "US",
"type": "education",
"lineage": [
"https://openalex.org/I95457486"
]
}
],
"topics": [
{
"id": "https://openalex.org/T10406",
"display_name": "Exploration and Study of Mars",
"count": 102,
"subfield": {
"id": "https://openalex.org/subfields/3103",
"display_name": "Astronomy and Astrophysics"
},
"field": {
"id": "https://openalex.org/fields/31",
"display_name": "Physics and Astronomy"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10325",
"display_name": "Formation and Evolution of the Solar System",
"count": 81,
"subfield": {
"id": "https://openalex.org/subfields/3103",
"display_name": "Astronomy and Astrophysics"
},
"field": {
"id": "https://openalex.org/fields/31",
"display_name": "Physics and Astronomy"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10110",
"display_name": "Seismicity and Tectonic Plate Interactions",
"count": 80,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10001",
"display_name": "Tectonic and Geochronological Evolution of Orogens",
"count": 74,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10413",
"display_name": "Mantle Dynamics and Earth's Structure",
"count": 43,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10017",
"display_name": "Climate Change and Paleoclimatology",
"count": 41,
"subfield": {
"id": "https://openalex.org/subfields/1902",
"display_name": "Atmospheric Science"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T12424",
"display_name": "Study of Earthquake Precursor Phenomena",
"count": 40,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10995",
"display_name": "Anaerobic Methane Oxidation and Gas Hydrates",
"count": 37,
"subfield": {
"id": "https://openalex.org/subfields/2304",
"display_name": "Environmental Chemistry"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13018",
"display_name": "Machine Learning for Earthquake Early Warning Systems",
"count": 35,
"subfield": {
"id": "https://openalex.org/subfields/1702",
"display_name": "Artificial Intelligence"
},
"field": {
"id": "https://openalex.org/fields/17",
"display_name": "Computer Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11786",
"display_name": "Magnetosome Formation in Prokaryotes",
"count": 33,
"subfield": {
"id": "https://openalex.org/subfields/1312",
"display_name": "Molecular Biology"
},
"field": {
"id": "https://openalex.org/fields/13",
"display_name": "Biochemistry, Genetics and Molecular Biology"
},
"domain": {
"id": "https://openalex.org/domains/1",
"display_name": "Life Sciences"
}
},
{
"id": "https://openalex.org/T10965",
"display_name": "Sedimentary Processes in Earth's Geology",
"count": 25,
"subfield": {
"id": "https://openalex.org/subfields/1904",
"display_name": "Earth-Surface Processes"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T14214",
"display_name": "Space Suit Design and Ergonomics for EVA",
"count": 23,
"subfield": {
"id": "https://openalex.org/subfields/2202",
"display_name": "Aerospace Engineering"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10399",
"display_name": "Characterization of Shale Gas Pore Structure",
"count": 23,
"subfield": {
"id": "https://openalex.org/subfields/2211",
"display_name": "Mechanics of Materials"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11757",
"display_name": "High-Resolution Seismic Noise Tomography",
"count": 21,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13177",
"display_name": "Geological Evolution of South China Sea",
"count": 18,
"subfield": {
"id": "https://openalex.org/subfields/1907",
"display_name": "Geology"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10535",
"display_name": "Landslide Hazards and Risk Assessment",
"count": 16,
"subfield": {
"id": "https://openalex.org/subfields/2308",
"display_name": "Management, Monitoring, Policy and Law"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10894",
"display_name": "Groundwater Flow and Transport Modeling",
"count": 13,
"subfield": {
"id": "https://openalex.org/subfields/2305",
"display_name": "Environmental Engineering"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10271",
"display_name": "Seismic Waveform Inversion in Geophysics",
"count": 12,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10635",
"display_name": "Hydraulic Fracturing in Shale Gas Reservoirs",
"count": 12,
"subfield": {
"id": "https://openalex.org/subfields/2210",
"display_name": "Mechanical Engineering"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13067",
"display_name": "Geological Modeling and Uncertainty Analysis",
"count": 11,
"subfield": {
"id": "https://openalex.org/subfields/1906",
"display_name": "Geochemistry and Petrology"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10644",
"display_name": "Impacts of Climate Change on Glaciers and Water Availability",
"count": 11,
"subfield": {
"id": "https://openalex.org/subfields/1902",
"display_name": "Atmospheric Science"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10360",
"display_name": "Turbulent Flows and Vortex Dynamics",
"count": 11,
"subfield": {
"id": "https://openalex.org/subfields/2206",
"display_name": "Computational Mechanics"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13404",
"display_name": "Geodynamics of the Northern Andes and Caribbean Region",
"count": 10,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11302",
"display_name": "Carbon Dioxide Sequestration in Geological Formations",
"count": 10,
"subfield": {
"id": "https://openalex.org/subfields/2305",
"display_name": "Environmental Engineering"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13200",
"display_name": "Cryogenic Fluid Storage and Management",
"count": 10,
"subfield": {
"id": "https://openalex.org/subfields/2202",
"display_name": "Aerospace Engineering"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
}
],
"topic_share": [
{
"id": "https://openalex.org/T10406",
"display_name": "Exploration and Study of Mars",
"value": 0.0002993,
"subfield": {
"id": "https://openalex.org/subfields/3103",
"display_name": "Astronomy and Astrophysics"
},
"field": {
"id": "https://openalex.org/fields/31",
"display_name": "Physics and Astronomy"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13018",
"display_name": "Machine Learning for Earthquake Early Warning Systems",
"value": 0.0002438,
"subfield": {
"id": "https://openalex.org/subfields/1702",
"display_name": "Artificial Intelligence"
},
"field": {
"id": "https://openalex.org/fields/17",
"display_name": "Computer Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10110",
"display_name": "Seismicity and Tectonic Plate Interactions",
"value": 0.0002166,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T14214",
"display_name": "Space Suit Design and Ergonomics for EVA",
"value": 0.0001729,
"subfield": {
"id": "https://openalex.org/subfields/2202",
"display_name": "Aerospace Engineering"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13404",
"display_name": "Geodynamics of the Northern Andes and Caribbean Region",
"value": 0.0001591,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10001",
"display_name": "Tectonic and Geochronological Evolution of Orogens",
"value": 0.0001539,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10325",
"display_name": "Formation and Evolution of the Solar System",
"value": 0.0001353,
"subfield": {
"id": "https://openalex.org/subfields/3103",
"display_name": "Astronomy and Astrophysics"
},
"field": {
"id": "https://openalex.org/fields/31",
"display_name": "Physics and Astronomy"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11786",
"display_name": "Magnetosome Formation in Prokaryotes",
"value": 0.0001289,
"subfield": {
"id": "https://openalex.org/subfields/1312",
"display_name": "Molecular Biology"
},
"field": {
"id": "https://openalex.org/fields/13",
"display_name": "Biochemistry, Genetics and Molecular Biology"
},
"domain": {
"id": "https://openalex.org/domains/1",
"display_name": "Life Sciences"
}
},
{
"id": "https://openalex.org/T11302",
"display_name": "Carbon Dioxide Sequestration in Geological Formations",
"value": 0.0001262,
"subfield": {
"id": "https://openalex.org/subfields/2305",
"display_name": "Environmental Engineering"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10413",
"display_name": "Mantle Dynamics and Earth's Structure",
"value": 0.0001244,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T12424",
"display_name": "Study of Earthquake Precursor Phenomena",
"value": 0.0001058,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11225",
"display_name": "Geothermal Energy Technology and Applications",
"value": 9.75e-05,
"subfield": {
"id": "https://openalex.org/subfields/2105",
"display_name": "Renewable Energy, Sustainability and the Environment"
},
"field": {
"id": "https://openalex.org/fields/21",
"display_name": "Energy"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10965",
"display_name": "Sedimentary Processes in Earth's Geology",
"value": 9.52e-05,
"subfield": {
"id": "https://openalex.org/subfields/1904",
"display_name": "Earth-Surface Processes"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10864",
"display_name": "Bioreactor Scale-up and Oxygen Transfer in Microbial Processes",
"value": 7.73e-05,
"subfield": {
"id": "https://openalex.org/subfields/2204",
"display_name": "Biomedical Engineering"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13177",
"display_name": "Geological Evolution of South China Sea",
"value": 7.22e-05,
"subfield": {
"id": "https://openalex.org/subfields/1907",
"display_name": "Geology"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10894",
"display_name": "Groundwater Flow and Transport Modeling",
"value": "7e-05",
"subfield": {
"id": "https://openalex.org/subfields/2305",
"display_name": "Environmental Engineering"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10017",
"display_name": "Climate Change and Paleoclimatology",
"value": 6.32e-05,
"subfield": {
"id": "https://openalex.org/subfields/1902",
"display_name": "Atmospheric Science"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10995",
"display_name": "Anaerobic Methane Oxidation and Gas Hydrates",
"value": 6.18e-05,
"subfield": {
"id": "https://openalex.org/subfields/2304",
"display_name": "Environmental Chemistry"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T12063",
"display_name": "Heat Transfer in Porous Media and Packed Beds",
"value": 5.87e-05,
"subfield": {
"id": "https://openalex.org/subfields/2206",
"display_name": "Computational Mechanics"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10615",
"display_name": "Dynamics of Granular Flow Systems",
"value": 5.85e-05,
"subfield": {
"id": "https://openalex.org/subfields/2206",
"display_name": "Computational Mechanics"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T12821",
"display_name": "Tectonic Evolution of Carpathian-Pannonian Region",
"value": 5.7e-05,
"subfield": {
"id": "https://openalex.org/subfields/1908",
"display_name": "Geophysics"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T10535",
"display_name": "Landslide Hazards and Risk Assessment",
"value": 5.68e-05,
"subfield": {
"id": "https://openalex.org/subfields/2308",
"display_name": "Management, Monitoring, Policy and Law"
},
"field": {
"id": "https://openalex.org/fields/23",
"display_name": "Environmental Science"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11382",
"display_name": "Dynamics of Drop Impact on Surfaces",
"value": 5.59e-05,
"subfield": {
"id": "https://openalex.org/subfields/2206",
"display_name": "Computational Mechanics"
},
"field": {
"id": "https://openalex.org/fields/22",
"display_name": "Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T11379",
"display_name": "Rheology of Complex Fluids and Polymers",
"value": 5.59e-05,
"subfield": {
"id": "https://openalex.org/subfields/1507",
"display_name": "Fluid Flow and Transfer Processes"
},
"field": {
"id": "https://openalex.org/fields/15",
"display_name": "Chemical Engineering"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
},
{
"id": "https://openalex.org/T13067",
"display_name": "Geological Modeling and Uncertainty Analysis",
"value": 5.35e-05,
"subfield": {
"id": "https://openalex.org/subfields/1906",
"display_name": "Geochemistry and Petrology"
},
"field": {
"id": "https://openalex.org/fields/19",
"display_name": "Earth and Planetary Sciences"
},
"domain": {
"id": "https://openalex.org/domains/3",
"display_name": "Physical Sciences"
}
}
],
"x_concepts": [
{
"id": "https://openalex.org/C127313418",
"wikidata": "https://www.wikidata.org/wiki/Q1069",
"display_name": "Geology",
"level": 0,
"score": 92.6
},
{
"id": "https://openalex.org/C86803240",
"wikidata": "https://www.wikidata.org/wiki/Q420",
"display_name": "Biology",
"level": 0,
"score": 77.5
},
{
"id": "https://openalex.org/C121332964",
"wikidata": "https://www.wikidata.org/wiki/Q413",
"display_name": "Physics",
"level": 0,
"score": 72.4
},
{
"id": "https://openalex.org/C151730666",
"wikidata": "https://www.wikidata.org/wiki/Q7205",
"display_name": "Paleontology",
"level": 1,
"score": 58.1
},
{
"id": "https://openalex.org/C165205528",
"wikidata": "https://www.wikidata.org/wiki/Q83371",
"display_name": "Seismology",
"level": 1,
"score": 55.4
},
{
"id": "https://openalex.org/C127413603",
"wikidata": "https://www.wikidata.org/wiki/Q11023",
"display_name": "Engineering",
"level": 0,
"score": 47.5
},
{
"id": "https://openalex.org/C17409809",
"wikidata": "https://www.wikidata.org/wiki/Q161764",
"display_name": "Geochemistry",
"level": 1,
"score": 46.1
},
{
"id": "https://openalex.org/C205649164",
"wikidata": "https://www.wikidata.org/wiki/Q1071",
"display_name": "Geography",
"level": 0,
"score": 43.3
},
{
"id": "https://openalex.org/C97355855",
"wikidata": "https://www.wikidata.org/wiki/Q11473",
"display_name": "Thermodynamics",
"level": 1,
"score": 33.4
},
{
"id": "https://openalex.org/C120806208",
"wikidata": "https://www.wikidata.org/wiki/Q8072",
"display_name": "Volcano",
"level": 2,
"score": 30.3
},
{
"id": "https://openalex.org/C62520636",
"wikidata": "https://www.wikidata.org/wiki/Q944",
"display_name": "Quantum mechanics",
"level": 1,
"score": 29.8
},
{
"id": "https://openalex.org/C185592680",
"wikidata": "https://www.wikidata.org/wiki/Q2329",
"display_name": "Chemistry",
"level": 0,
"score": 27.9
},
{
"id": "https://openalex.org/C1276947",
"wikidata": "https://www.wikidata.org/wiki/Q333",
"display_name": "Astronomy",
"level": 1,
"score": 27.3
},
{
"id": "https://openalex.org/C192562407",
"wikidata": "https://www.wikidata.org/wiki/Q228736",
"display_name": "Materials science",
"level": 0,
"score": 26.5
},
{
"id": "https://openalex.org/C8058405",
"wikidata": "https://www.wikidata.org/wiki/Q46255",
"display_name": "Geophysics",
"level": 1,
"score": 26.3
},
{
"id": "https://openalex.org/C41008148",
"wikidata": "https://www.wikidata.org/wiki/Q21198",
"display_name": "Computer science",
"level": 0,
"score": 24.4
},
{
"id": "https://openalex.org/C87355193",
"wikidata": "https://www.wikidata.org/wiki/Q411",
"display_name": "Astrobiology",
"level": 1,
"score": 23.4
},
{
"id": "https://openalex.org/C187320778",
"wikidata": "https://www.wikidata.org/wiki/Q1349130",
"display_name": "Geotechnical engineering",
"level": 1,
"score": 22.3
},
{
"id": "https://openalex.org/C153294291",
"wikidata": "https://www.wikidata.org/wiki/Q25261",
"display_name": "Meteorology",
"level": 1,
"score": 21.9
},
{
"id": "https://openalex.org/C57879066",
"wikidata": "https://www.wikidata.org/wiki/Q41217",
"display_name": "Mechanics",
"level": 1,
"score": 21.1
},
{
"id": "https://openalex.org/C159985019",
"wikidata": "https://www.wikidata.org/wiki/Q181790",
"display_name": "Composite material",
"level": 1,
"score": 20.4
}
],
"counts_by_year": [
{
"year": 2024,
"works_count": 31,
"cited_by_count": 1967
},
{
"year": 2023,
"works_count": 18,
"cited_by_count": 2750
},
{
"year": 2022,
"works_count": 25,
"cited_by_count": 3119
},
{
"year": 2021,
"works_count": 45,
"cited_by_count": 3766
},
{
"year": 2020,
"works_count": 28,
"cited_by_count": 3159
},
{
"year": 2019,
"works_count": 40,
"cited_by_count": 2702
},
{
"year": 2018,
"works_count": 39,
"cited_by_count": 2309
},
{
"year": 2017,
"works_count": 29,
"cited_by_count": 1843
},
{
"year": 2016,
"works_count": 37,
"cited_by_count": 1701
},
{
"year": 2015,
"works_count": 40,
"cited_by_count": 1854
},
{
"year": 2014,
"works_count": 37,
"cited_by_count": 1637
},
{
"year": 2013,
"works_count": 34,
"cited_by_count": 1346
},
{
"year": 2012,
"works_count": 45,
"cited_by_count": 1285
}
],
"works_api_url": "https://api.openalex.org/works?filter=author.id:A5040980912",
"updated_date": "2024-08-21T20:51:36.193207",
"created_date": "2023-07-21",
"_id": "https://openalex.org/A5040980912"
},
"ORCID": {
"@context": "http://schema.org",
"@type": "Person",
"@id": "https://orcid.org/0000-0003-3286-4682",
"mainEntityOfPage": "https://orcid.org/0000-0003-3286-4682",
"givenName": "Michael",
"familyName": "Manga",
"alumniOf": [
{
"@type": "Organization",
"name": "McGill University",
"identifier": {
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "5620"
}
},
{
"@type": "Organization",
"name": "Harvard University",
"identifier": {
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "1812"
}
}
],
"affiliation": [
{
"@type": "Organization",
"name": "University of California Berkeley",
"alternateName": "Earth and Planetary Science",
"identifier": {
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "1438"
}
},
{
"@type": "Organization",
"name": "CIFAR",
"identifier": {
"@type": "PropertyValue",
"propertyID": "ROR",
"value": "https://ror.org/01sdtdd95"
}
}
],
"@reverse": {
"funder": [
{
"@type": "Organization",
"name": "National Aeronautics and Space Administration",
"alternateName": "UNIVERSITY OF CALIFORNIA AT BERKELEY TIDALLY-DRIVEN FRACTURES ON EUROPA Arcuate features on Europa, called cycloids, are thought to be cracks formed in response to tidal stress; models for cycloids can thus be used to constrain the orbital and rotational",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "3997"
},
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "nnx09au78h"
}
]
},
{
"@type": "Organization",
"name": "National Aeronautics and Space Administration",
"alternateName": "Consequences of a Layered Mantle and Melt Generation on the Evolution of the Martian Interior and Surface The evolution of a planet's interior is reflected in its volcanic history and preserved in its crust. Modeling of the planetary interior can thus be",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "3997"
},
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "nnx08an13g"
}
]
},
{
"@type": "Organization",
"name": "National Aeronautics and Space Administration",
"alternateName": "UNIVERSITY OF CALIFORNIA-BERKELEY THE MAGMATIC HISTORY OF THARSIS: INSIGHT FROM THERMAL,MECHANICAL AND MAGNETIC FIELD MODELING We propose to develop and utilize physical models for magma transport, thermal evolution and thermal demagnetization in the crus",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "RINGGOLD",
"value": "3997"
},
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "nnx09an18g"
}
]
},
{
"@type": "Organization",
"@id": "https://doi.org/10.13039/501100009193",
"name": "Marsden Fund",
"alternateName": "Turbulent killers - how do volcanic eruptions become ferocious?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "proposal_id",
"value": "MFP-19-MAU-103"
},
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "mfp-mau1902"
}
]
},
{
"@type": "Organization",
"@id": "https://doi.org/10.13039/501100009193",
"name": "Marsden Fund",
"alternateName": "Digging into the biggest explosive submarine eruption ever \"seen\" to understand seafloor volcanism",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "mfp-uoo1616"
},
{
"@type": "PropertyValue",
"propertyID": "proposal_id",
"value": "MFP-16-UOO-134"
}
]
},
{
"@type": "Organization",
"@id": "https://doi.org/10.13039/501100009193",
"name": "Marsden Fund",
"alternateName": "Earthquake hydrology: seismic pumps or broken pipes?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "proposal_id",
"value": "MFP-12-GNS-003"
},
{
"@type": "PropertyValue",
"propertyID": "grant_number",
"value": "mfp-gns1202"
}
]
}
],
"creator": [
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1073/pnas.2409983121",
"name": "Liquid water in the Martian mid-crust",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1073/pnas.2409983121"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2024gc011476",
"name": "Water Geochemistry and Stable Isotope Changes Record Groundwater Mixing After a Regional Earthquake in Northeast India",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2024gc011476"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00410-024-02126-z",
"name": "Stressful crystal histories recorded around melt inclusions in volcanic quartz",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00410-024-02126-z"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2024.118689",
"name": "The evolution of a young ocean within Mimas",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2024.118689"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/s41561-024-01392-7",
"name": "Hazardous explosive eruptions of a recharging multi-cyclic island arc caldera",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/s41561-024-01392-7"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.3390/w16060868",
"name": "Using the Tidal Response of Groundwater to Assess and Monitor Caprock Confinement in CO2 Geological Sequestration",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.3390/w16060868"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2023jb027970",
"name": "Long\u2010 and Short\u2010Term Effects of Seismic Waves and Coseismic Pressure Changes on Fractured Aquifers",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2023jb027970"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.30909/vol.06.02.437445",
"name": "gas-tight shock tube apparatus for laboratory volcanic lightning under varying atmospheric conditions",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.30909/vol.06.02.437445"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2023jb026775",
"name": "Pre\u2010Eruptive Outgassing and Pressurization, and Post\u2010Fragmentation Bubble Nucleation, Recorded by Vesicles in Breadcrust Bombs From Vulcanian Activity at Guagua Pichincha Volcano, Ecuador",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2023jb026775"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2023gc010988",
"name": "The Relation Between Decadal Droughts and Eruptions of Steamboat Geyser in Yellowstone National Park, USA",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2023gc010988"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2023gl103904",
"name": "Snow Suppresses Seismic Signals From Steamboat Geyser",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2023gl103904"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/egusphere-egu23-3622",
"name": "Topographic signatures and statistics of different tectonic regimes and application to terrestrial planets",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/egusphere-egu23-3622"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.3390/w15071327",
"name": "Changes in Tidal and Barometric Response of Groundwater during Earthquakes\u2014A Review with Recommendations for Better Management of Groundwater Resources",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.3390/w15071327"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022jb025809",
"name": "Experimental Measurement of Enhanced and Hindered Particle Settling in Turbulent Gas\u2010Particle Suspensions, and Geophysical Implications",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022jb025809"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022gl101175",
"name": "Thumping Cycle Variations of Doublet Pool in Yellowstone National Park, USA",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022gl101175"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022gl100852",
"name": "Electric Discharge in Erupting Mud",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022gl100852"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022gl101239",
"name": "Violent Groundwater Eruption Triggered by a Distant Earthquake",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022gl101239"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022je007539",
"name": "Lithology, Pore\u2010Filling Media, and Pore Closure Depth Beneath InSight on Mars Inferred From Shear Wave Velocities",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022je007539"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1101/2022.11.17.516901",
"name": "Autotrophic biofilms sustained by deeply-sourced groundwater host diverse CPR bacteria implicated in sulfur and hydrogen metabolism",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1101/2022.11.17.516901"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022wr033272",
"name": "Changes of Hydraulic Transmissivity Orientation Induced by Tele\u2010Seismic Waves",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022wr033272"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022jb024390",
"name": "The Influence of Grain Size Distribution on Laboratory\u2010Generated Volcanic Lightning",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022jb024390"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022gl099250",
"name": "A Minimally Cemented Shallow Crust Beneath InSight",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022gl099250"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2022gl098061",
"name": "The History of Water in Martian Magmas From Thorium Maps",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2022gl098061"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/egusphere-egu22-1851",
"name": "The reactivation and monitoring of Steamboat geyser, the tallest geyser on Earth",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/egusphere-egu22-1851"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/egusphere-egu22-2223",
"name": "Trees Talk Tremor—Wood Anatomy and δ13C Content Reveal Contrasting Tree-Growth Responses to Earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/egusphere-egu22-2223"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2021gl094421",
"name": "Cooling Crusts Create Concomitant Cryovolcanic Cracks",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2021gl094421"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s10035-021-01169-4",
"name": "Microstructural differences between naturally-deposited and laboratory beach sands",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s10035-021-01169-4"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2021gl095202",
"name": "Some Lava Flows May Not Have Been as Thick as They Appear",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2021gl095202"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2021jg006385",
"name": "Trees Talk Tremor\u2014Wood Anatomy and Content Reveal Contrasting Tree\u2010Growth Responses to Earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2021jg006385"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10507565.1",
"name": "Some lava flows may not have been as thick as they appear",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10507565.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2020wr028874",
"name": "Bayesian Detection of Streamflow Response to Earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2020wr028874"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10507084.1",
"name": "Some lava flows may not have been as thick as they appear",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10507084.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1073/pnas.2102338118",
"name": "Widespread deep seismicity in the Delaware Basin, Texas, is mainly driven by shallow wastewater injection",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1073/pnas.2102338118"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2021gl093127",
"name": "No Cryosphere\u2010Confined Aquifer Below InSight on Mars",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2021gl093127"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10506780.1",
"name": "Trees talk tremor - Wood anatomy and \u03b413C content reveal contrasting tree-growth responses to earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10506780.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2020je006518",
"name": "Analyzing Low Frequency Seismic Events at Cerberus Fossae as Long Period Volcanic Quakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2020je006518"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/s41561-021-00709-0",
"name": "Brittle fragmentation by rapid gas separation in a Hawaiian fountain",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/s41561-021-00709-0"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.enggeo.2020.105982",
"name": "Can artesian groundwater and earthquake-induced aquifer leakage exacerbate the manifestation of liquefaction?",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.enggeo.2020.105982"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10505246.1",
"name": "LIP flows may not have been as thick as they appear",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10505246.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2020jb019711",
"name": "Origin and Properties of Hydrothermal Tremor at Lone Star Geyser, Yellowstone National Park, USA",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2020jb019711"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2020gl089871",
"name": "Yellowstone's Old Faithful Geyser Shut Down by a Severe Thirteenth Century Drought",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2020gl089871"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2020gl087908",
"name": "Radiocarbon Dating of Silica Sinter and Postglacial Hydrothermal Activity in the El Tatio Geyser Field",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2020gl087908"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.tecto.2020.228458",
"name": "The effect of slab gaps on subduction dynamics and mantle upwelling",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.tecto.2020.228458"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/egusphere-egu2020-1315",
"name": "Explosive mud volcano eruptions and rafting of mud breccia blocks",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/egusphere-egu2020-1315"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/esurf-8-195-2020",
"name": "Large wood as a confounding factor in interpreting the width of spring-fed streams",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/esurf-8-195-2020"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019gl085705",
"name": "Elevated Seismic Hazard in Kansas Due to High\u2010Volume Injections in Oklahoma",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019gl085705"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019gl086768",
"name": "Ongoing Dispersal of the 7 August 2019 Pumice Raft From the Tonga Arc in the Southwestern Pacific Ocean",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019gl086768"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019ea000876",
"name": "Rheology of Natural Sediments and Its Influence on the Settling of Dropstones in Hemipelagic Marine Sediment",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019ea000876"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10501930.1",
"name": "The Chemistry and Mineralogy of Sinter Deposits From two Large Geysers in the Upper Geyser Basin, Yellowstone National Park",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10501930.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/s41550-019-0958-x",
"name": "Cascading parallel fractures on Enceladus",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/s41550-019-0958-x"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/esurf-2019-60-supplement",
"name": "Supplementary material to "Woody debris as a confounding factor in interpreting the width of spring-fed streams"",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/esurf-2019-60-supplement"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/esurf-2019-60",
"name": "Woody debris as a confounding factor in interpreting the width of spring-fed streams",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/esurf-2019-60"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019gl083619",
"name": "Volcanoes Erupt Stressed Quartz Crystals",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019gl083619"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1073/pnas.1819225116",
"name": "Pore-pressure diffusion, enhanced by poroelastic stresses, controls induced seismicity in Oklahoma",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1073/pnas.1819225116"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019wr025166",
"name": "Capillary Effects on Groundwater Response to Earth Tides",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019wr025166"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019wr025219",
"name": "Multiscale Digital Porous Rock Reconstruction Using Template Matching",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019wr025219"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019wr024871",
"name": "Coseismic Groundwater Drawdown Along Crustal Ruptures During the 2016 Mw 7.0 Kumamoto Earthquake",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019wr024871"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019wr025341",
"name": "Earthquake Hydrogeology",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019wr025341"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019gl082658",
"name": "Maximum Solid Phase Concentration in Geophysical Turbulent Gas\u2010Particle Flows: Insights From Laboratory Experiments",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019gl082658"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2019gl082892",
"name": "Squeezing Marsquakes Out of Groundwater",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2019gl082892"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2019.03.025",
"name": "Hydraulic properties of injection formations constrained by surface deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85063404235"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2019.03.025"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/essoar.10500972.1",
"name": "Squeezing Marsquakes out of groundwater",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/essoar.10500972.1"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2018jb016454",
"name": "Geometry of Geyser Plumbing Inferred From Ground Deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2018jb016454"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85060778449"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g45436.1",
"name": "Transition of eruptive style: Pumice raft to dome-forming eruption at the Havre submarine volcano, southwest Pacific Ocean",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g45436.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85057584289"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.marpetgeo.2017.12.031",
"name": "An alternative review of facts, coincidences and past and future studies of the Lusi eruption",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.marpetgeo.2017.12.031"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85047468107"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2018gl078621",
"name": "Stronger Peak Ground Motion, Beyond the Threshold to Initiate a Response, Does Not Lead to Larger Stream Discharge Responses to Earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2018gl078621"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85050558359"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2017jb014986",
"name": "Subsurface Structure of Long Valley Caldera Imaged With Seismic Scattering and Intrinsic Attenuation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85051071548"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2017jb014986"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2018jb015530",
"name": "Experimental Measurement of the Solid Particle Concentration in Geophysical Turbulent Gas\u2010Particle Mixtures",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2018jb015530"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85047815589"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2018.02.025",
"name": "The pumice raft-forming 2012 Havre submarine eruption was effusive",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2018.02.025"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85042938955"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/sciadv.1701536",
"name": "Monitoring reservoir response to earthquakes and fluid extraction, Salton Sea geothermal field, California",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/sciadv.1701536"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85042202334"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/sciadv.1701121",
"name": "The largest deep-ocean silicic volcanic eruption of the past century",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85042198554"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/sciadv.1701121"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2018.03.031",
"name": "A hybrid origin of the Martian crustal dichotomy: Degree-1 convection antipodal to a giant impact",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2018.03.031"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85044438827"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/s41467-018-05293-3",
"name": "Controls on explosive-effusive volcanic eruption styles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85050590470"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/s41467-018-05293-3"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00024-018-1923-9",
"name": "Hydrological, Geochemical and Geophysical Changes Related to Earthquakes and Slow-Slip Events: Introduction",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85050803419"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00024-018-1923-9"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2018.07.007",
"name": "Hydrothermal discharge from the El Tatio basin, Atacama, Chile",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85051539620"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2018.07.007"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00410-018-1479-9",
"name": "Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85050212168"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00410-018-1479-9"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2018.07.002",
"name": "Pyroclast cooling and saturation in water",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85052976622"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2018.07.002"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-018-1232-2",
"name": "Revisiting short-term earthquake triggered volcanism",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-018-1232-2"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85048271468"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/nature26144",
"name": "Timing of oceans on Mars from shoreline deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85044641140"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/nature26144"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2017jb014777",
"name": "Dynamic Triggering of Mud Volcano Eruptions During the 2016\u20132017 Central Italy Seismic Sequence",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85034250579"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2017jb014777"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016wr020007",
"name": "Thermal effect of climate change on groundwater\u2010fed ecosystems",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85018878327"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016wr020007"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g39256.1",
"name": "Evenly spaced columns in the Bishop Tuff (California, USA) as relicts of hydrothermal cooling",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85032282472"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g39256.1"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2016.10.009",
"name": "Formation of lenticulae on Europa by saucer-shaped sills",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85008893172"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2016.10.009"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1785/0220170017",
"name": "Induced seismicity in Oklahoma affects shallow groundwater",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85021718460"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1785/0220170017"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2016.11.013",
"name": "Regional changes in streamflow after a megathrust earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2016.11.013"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85003728155"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/b31448.1",
"name": "Submarine deposits from pumiceous pyroclastic density currents traveling over water: An outstanding example from offshore Montserrat (IODP 340)",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/b31448.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85015145903"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1146/annurev-earth-063016-015605",
"name": "The Fascinating and Complex Dynamics of Geyser Eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85027987893"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1146/annurev-earth-063016-015605"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2016.11.055",
"name": "Trapped bubbles keep pumice afloat and gas diffusion makes pumice sink",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2016.11.055"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85006758055"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/b31645.1",
"name": "Triggering of the largest Deccan eruptions by the Chicxulub impact: Reply",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/b31645.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85009774820"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2016.09.035",
"name": "Volatiles and the tempo of flood basalt magmatism",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2016.09.035"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85003683127"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016gl071268",
"name": "Increased stream discharge after the 3 September 2016 Mw 5.8 Pawnee, Oklahoma earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85003914714"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016gl071268"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016gc006472",
"name": "An experimental study of the role of subsurface plumbing on geothermal discharge",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016gc006472"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84987754288"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-016-1053-0",
"name": "Ash production and dispersal from sustained low-intensity Mono-Inyo eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84982719985"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-016-1053-0"
}
]
},
{
"@type": "CreativeWork",
"name": "Continental-scale water-level response to a large earthquake",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85019495129"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.2166/wst.2016.451",
"name": "Effect of filter media thickness on the performance of sand drying beds used for faecal sludge management",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.2166/wst.2016.451"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85029718219"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016jb013263",
"name": "Effect of particle entrainment on the runout of pyroclastic density currents",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84988355074"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016jb013263"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015wr018204",
"name": "Evaluating geothermal and hydrogeologic controls on regional groundwater temperature distribution",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84959266134"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015wr018204"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2015.12.052",
"name": "Geometry and spatial distribution of lenticulae on Europa",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84957836899"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2015.12.052"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016wr018893",
"name": "Large earthquakes create vertical permeability by breaching aquitards",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016wr018893"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84982812612"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.tecto.2016.01.037",
"name": "Long- and short-term triggering and modulation of mud volcano eruptions by earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.tecto.2016.01.037"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84959214564"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-016-1071-y",
"name": "MeMoVolc report on classification and dynamics of volcanic explosive eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-016-1071-y"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84993953207"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2016.06.026",
"name": "Physical and hydraulic properties of modern sinter deposits: El Tatio, Atacama",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84978069364"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2016.06.026"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016gl068560",
"name": "Primordial metallic melt in the deep mantle",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016gl068560"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84968754916"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016gc006439",
"name": "Quantifying melt production and degassing rate at mid-ocean ridges from global mantle convection models with plate motion history",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84979743438"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016gc006439"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/science.aag0262",
"name": "Surface uplift and time-dependent seismic hazard due to fluid injection in eastern Texas",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/science.aag0262"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84989853121"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2016je004998",
"name": "The eruptibility of magmas at Tharsis and Syrtis Major on Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84978042249"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2016je004998"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015gc006053",
"name": "The relationship between eruptive activity, flank collapse, and sea level at volcanic islands: A long-term (>1 Ma) record offshore Montserrat, Lesser Antilles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015gc006053"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84978431844"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-015-0971-6",
"name": "Ascent and emplacement dynamics of obsidian lavas inferred from microlite textures",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84942155342"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-015-0971-6"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015gl064571",
"name": "Ascent velocity and dynamics of the Fiumicino mud eruption, Rome, Italy",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84940446732"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015gl064571"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2015.02.004",
"name": "Bubble mobility in mud and magmatic volcanoes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2015.02.004"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84928334452"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g36514.1",
"name": "Campanian Ignimbrite volcanism, climate, and the final decline of the Neanderthals",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84929465931"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g36514.1"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/gfl.12099",
"name": "Continental-scale water-level response to a large earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84923119156"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/gfl.12099"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015gl064576",
"name": "Deep and shallow sources for the Lusi mud eruption revealed by surface deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84938149550"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015gl064576"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2015.01.002",
"name": "Dynamics within geyser conduits, and sensitivity to environmental perturbations: Insights from a periodic geyser in the El Tatio geyser field, Atacama Desert, Chile",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2015.01.002"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84922377504"
}
]
},
{
"@type": "CreativeWork",
"name": "Earthquake Hydrology",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85029493939"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015jb012364",
"name": "Geyser eruption intervals and interactions: Examples from El Tatio, Atacama, Chile",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84955199631"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015jb012364"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015gl065310",
"name": "Influence of seismicity on the Lusi mud eruption",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015gl065310"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84945186905"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/ngeo2472",
"name": "Initiation of the Lusi mudflow disaster",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/ngeo2472"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84934291529"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2015.08.012",
"name": "Mechanism of co-seismic water level change following four great earthquakes - insights from co-seismic responses throughout the Chinese mainland",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84939810799"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2015.08.012"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/ncomms8597",
"name": "New streams and springs after the 2014 Mw6.0 South Napa earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/ncomms8597"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84943258644"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015jb011877",
"name": "Organic matter maturation in the contact aureole of an igneous sill as a tracer of hydrothermal convection",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015jb011877"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84931024561"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015jb012061",
"name": "Permeability and pressure measurements in Lesser Antilles submarine slides: Evidence for pressure-driven slow-slip failure",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84957843143"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015jb012061"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2015gl064519",
"name": "Rapid onset of mafic magmatism facilitated by volcanic edifice collapse",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2015gl064519"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84948717129"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g36261.1",
"name": "Shaking water out of soil",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g36261.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84923271067"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014gc005652",
"name": "Submarine record of volcanic island construction and collapse in the Lesser Antilles arc: First scientific drilling of submarine volcanic island landslides by IODP Expedition 340",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84922567262"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014gc005652"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014je004774",
"name": "The Syrtis Major volcano, Mars: A multidisciplinary approach to interpreting its magmatic evolution and structural development",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014je004774"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84945464555"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/b31167.1",
"name": "Triggering of the largest Deccan eruptions by the Chicxulub impact",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/b31167.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84946926754"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2014.01.048",
"name": "Comparison of hydrological responses to the Wenchuan and Lushan earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84894031217"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2014.01.048"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2013je004558",
"name": "Domes, pits, and small chaos on Europa produced by water sills",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84898678279"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2013je004558"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2013je004526",
"name": "Double ridges on Europa accommodate some of the missing surface contraction",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2013je004526"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84898677134"
}
]
},
{
"@type": "CreativeWork",
"name": "Earthquakes: Hydrogeochemical precursors",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84947226448"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014jb011009",
"name": "El Cobreloa: A geyser with two distinct eruption styles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014jb011009"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84906836463"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014jb011526",
"name": "Eruptions at Lone Star geyser, Yellowstone National Park, USA: 2. Constraints on subsurface dynamics",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84921449128"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014jb011526"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/978-3-319-00972-8_7",
"name": "Geomechanical characterization of submarine volcano-flank sediments, martinique, lesser antilles arc",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/978-3-319-00972-8_7"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84925625422"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2014.08.005",
"name": "Geyser preplay and eruption in a laboratory model with a bubble trap",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84906821872"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2014.08.005"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1146/annurev-earth-060313-055016",
"name": "How did early earth become our modern world?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1146/annurev-earth-060313-055016"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84902184550"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014gc005402",
"name": "Late Pleistocene stratigraphy of IODP Site U1396 and compiled chronology offshore of south and south west Montserrat, Lesser Antilles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014gc005402"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84906308930"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/tc-8-537-2014",
"name": "Near-surface permeability in a supraglacial drainage basin on the Llewellyn Glacier, Juneau Icefield, British Columbia",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84924569339"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/tc-8-537-2014"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1103/physreve.90.032208",
"name": "Penetration of spherical projectiles into wet granular media",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1103/physreve.90.032208"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84907267717"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-014-0808-8",
"name": "Pre-eruptive storage conditions and eruption dynamics of a small rhyolite dome: Douglas Knob, Yellowstone volcanic field, USA",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-014-0808-8"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84894087739"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014gc005442",
"name": "The ability of rock physics models to infer marine in situ pore pressure",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014gc005442"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84920942072"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2014gc005355",
"name": "The role of magmatically driven lithospheric thickening on arc front migration",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84905172336"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2014gc005355"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00410-013-0961-7",
"name": "Thermal and rheological controls on the formation of mafic enclaves or banded pumice",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00410-013-0961-7"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84891896488"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/2013jb010803",
"name": "Triggering and modulation of geyser eruptions in Yellowstone National Park by earthquakes, earth tides, and weather",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/2013jb010803"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84905692096"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/tcd-7-5281-2013",
"name": "Near-surface permeability in a supraglacial drainage basin on the Llewellyn glacier, Juneau Ice Field, British Columbia",
"identifier": {
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/tcd-7-5281-2013"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/grl.50738",
"name": "Basin-scale transport of heat and fluid induced by earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84881131588"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/grl.50738"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g33685.1",
"name": "Convection in a volcanic conduit recorded by bubbles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g33685.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84875517769"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/jgre.20085",
"name": "Demagnetization by basin-forming impacts on early Mars: Contributions from shock, heat, and excavation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/jgre.20085"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84882742688"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2013.04.001",
"name": "Effects of thermal quenching on mechanical properties of pyroclasts",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2013.04.001"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84877800904"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/jgrb.50251",
"name": "Eruptions at Lone Star Geyser, Yellowstone National Park, USA: 1. Energetics and eruption dynamics",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84883633187"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/jgrb.50251"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/grl.50189",
"name": "Evolution and future of the Lusi mud eruption inferred from ground deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/grl.50189"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84876942830"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/jgrf.20135",
"name": "Meander formation in supraglacial streams",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/jgrf.20135"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84887848586"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2013.07.012",
"name": "Measuring pressure in the source region for geysers, Geyser Valley, Kamchatka",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2013.07.012"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84883640853"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2012.11.034",
"name": "Seasonal melting and the formation of sedimentary rocks on Mars, with predictions for the Gale Crater mound",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2012.11.034"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84872259039"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/jgre.20105",
"name": "Time history of the Martian dynamo from crater magnetic field analysis",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84882784894"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/jgre.20105"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2013.04.004",
"name": "Wind driven capillary-gravity waves on Titan's lakes: Hard to detect or non-existent?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2013.04.004"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84877321866"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g33027.1",
"name": "Bubble geobarometry: A record of pressure changes, degassing, and regassing at Mono Craters, California",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g33027.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84866175788"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/ngeo1453",
"name": "Caldera size modulated by the yield stress within a crystal-rich magma reservoir",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84861683920"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/ngeo1453"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2011rg000382",
"name": "Changes in permeability caused by transient stresses: Field observations, experiments, and mechanisms",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84861181393"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2011rg000382"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2012je004166",
"name": "Effects of anisotropic viscosity and texture development on convection in ice mantles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84869396695"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2012je004166"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2012.02.011",
"name": "Experimental study of turbulence, sedimentation, and coignimbrite mass partitioning in dilute pyroclastic density currents",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84858723578"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2012.02.011"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2012jb009496",
"name": "Externally triggered renewed bubble nucleation in basaltic magma: The 12 October 2008 eruption at Halemaumau Overlook vent, Klauea, Hawai'i, USA",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84869479675"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2012jb009496"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2012gl052383",
"name": "Frequency dependence of mud volcano response to earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2012gl052383"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84864444663"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/ngeo1524",
"name": "Granular disruption during explosive volcanic eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/ngeo1524"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84864550912"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2012gc004260",
"name": "Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2012gc004260"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84865511490"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1080/00288306.2012.680474",
"name": "Hydrological effects of the M <inf>w</inf> 7.1 Darfield (Canterbury) earthquake, 4 September 2010, New Zealand",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84866975766"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1080/00288306.2012.680474"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.5194/nhess-12-3377-2012",
"name": "Large historical eruptions at subaerial mud volcanoes, Italy",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.5194/nhess-12-3377-2012"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84875381570"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2012gl054012",
"name": "Mechanics of old faithful Geyser, Calistoga, California",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2012gl054012"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84871556803"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2011.12.015",
"name": "Shell tectonics: A mechanical model for strike-slip displacement on Europa",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2011.12.015"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84855894775"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2012.06.056",
"name": "The effects of outgassing on the transition between effusive and explosive silicic eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84864566890"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2012.06.056"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g3914.1",
"name": "The viscous-brittle transition of crystal-bearing silicic melt: Direct observation of magma rupture and healing",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g3914.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84864292238"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g32565.1",
"name": "Transient change in groundwater temperature after earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84863229818"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g32565.1"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2011gl050192",
"name": "Wet surface and dense atmosphere on early Mars suggested by the bomb sag at Home Plate, Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84855579925"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2011gl050192"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/j.1468-8123.2011.00341.x",
"name": "A permeability-change model for water-level changes triggered by teleseismic waves",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/j.1468-8123.2011.00341.x"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-80051578678"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2011.05.037",
"name": "A prediction of the longevity of the Lusi mud eruption, Indonesia",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79960015765"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2011.05.037"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2010je003792",
"name": "Chaos terrain, storms, and past climate on Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-80054027770"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2010je003792"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1088/0004-637x/743/1/41",
"name": "Climate instability on tidally locked exoplanets",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1088/0004-637x/743/1/41"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-81855228802"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2011gl048235",
"name": "Cryoclastic origin of particles on the surface of Enceladus",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2011gl048235"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-80052009201"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g32226.1",
"name": "Effects of topography on pyroclastic density current runout and formation of coignimbrites",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-80955139367"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g32226.1"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.enggeo.2011.03.010",
"name": "Fluid transport properties and estimation of overpressure at the Lusi mud volcano, East Java Basin (Tanikawa et al., 2010)",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79959280725"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.enggeo.2011.03.010"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1002/9781444394900.ch14",
"name": "Hydrologic Responses to Earthquakes and a General Metric",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1002/9781444394900.ch14"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84886215976"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2010je003783",
"name": "Localized precipitation and runoff on Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79960496097"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2010je003783"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-010-0411-6",
"name": "Rounding of pumice clasts during transport: Field measurements and laboratory studies",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-010-0411-6"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79955699717"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2010.11.002",
"name": "Strike-slip fault patterns on Europa: Obliquity or polar wander?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2010.11.002"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-78650949320"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jcp.2010.07.002",
"name": "A lattice Boltzmann model for coupled diffusion",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jcp.2010.07.002"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77955512129"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2010.07.018",
"name": "Constraints on Europa's rotational dynamics from modeling of tidally-driven fractures",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2010.07.018"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-78049528697"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/978-3-642-00810-8_1",
"name": "Earthquakes influenced by water",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-75749154028"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/978-3-642-00810-8_1"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2010.05.007",
"name": "Heat transfer coefficients of natural volcanic clasts",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77954539266"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2010.05.007"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2009je003516",
"name": "How strong are lunar crustal magnetic fields at the surface?: Considerations from a reexamination of the electron reflectometry technique",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79151473047"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2009je003516"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/j.1468-8123.2009.00270.x",
"name": "Hydrologic responses to earthquakes and a general metric",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/j.1468-8123.2009.00270.x"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77953743776"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.pepi.2010.02.013",
"name": "Low-viscosity mantle blobs are sampled preferentially at regions of surface divergence and stirred rapidly into the mantle",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77952554104"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.pepi.2010.02.013"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2009.10.003",
"name": "Magma chamber stability in arc and continental crust",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2009.10.003"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-75749105332"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2010je003686",
"name": "Mars without the equilibrium rotational figure, Tharsis, and the remnant rotational figure",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2010je003686"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79251556868"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2010jb007737",
"name": "Mud volcano response to the 4 April 2010 El Mayor-Cucapah earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2010jb007737"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-79251583163"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.marpetgeo.2010.01.019",
"name": "Sawolo et al. (2009) the Lusi mud volcano controversy: Was it caused by drilling?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.marpetgeo.2010.01.019"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77954659780"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2009je003556",
"name": "Study of impact demagnetization at Mars using Monte Carlo modeling and multiple altitude data",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2009je003556"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77955645234"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1088/0004-637x/718/2/596",
"name": "Thermodynamic limits on magnetodynamos in rocky exoplanets",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1088/0004-637x/718/2/596"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-78049513933"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1093/petrology/egq003",
"name": "Two competing effects of volatiles on heat transfer in crystal-rich magmas: Thermal insulation vs defrosting",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-77952722366"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1093/petrology/egq003"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2009gl039852",
"name": "Changes in permeability caused by dynamic stresses in fractured sandstone",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2009gl039852"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-72149086399"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2008.12.007",
"name": "Demagnetization of crust by magmatic intrusion near the Arsia Mons volcano: Magnetic and thermal implications for the development of the Tharsis province, Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2008.12.007"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-67650439468"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00410-008-0327-8",
"name": "Diffusion-controlled spherulite growth in obsidian inferred from H<inf>2</inf>O concentration profiles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00410-008-0327-8"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-57849145094"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1017/cbo9781139021562.004",
"name": "Dynamics of magma ascent in the volcanic conduit",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84899668767"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1017/cbo9781139021562.004"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.marpetgeo.2009.01.019",
"name": "Earthquake triggering of mud volcanoes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.marpetgeo.2009.01.019"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-68449089231"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00410-008-0340-y",
"name": "Erratum: Diffusion-controlled spherulite growth in obsidian inferred from H2O concentration profiles (Contributions to Mineralogy and Petrology 10.1007/s00410-008-0327-8)",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00410-008-0340-y"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-57849117817"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2008.10.010",
"name": "Fracture penetration in planetary ice shells",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-58649091303"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2008.10.010"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1088/0004-637x/700/2/1732",
"name": "Geodynamics and rate of volcanism on massive earth-like planets",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1088/0004-637x/700/2/1732"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-70549083930"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2008je003287",
"name": "Giant impacts on early mars and the cessation of the martian dynamo",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-67650433407"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2008je003287"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2009.03.029",
"name": "Homogenization processes in silicic magma chambers by stirring and mushification (latent heat buffering)",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-67349144398"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2009.03.029"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2009jb006339",
"name": "Organization of volcanic plumbing through magmatic lensing by magma chambers and volcanic loads",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2009jb006339"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-72049123465"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/j.1468-8123.2009.00250.x",
"name": "Response of Alum Rock springs to the October 30, 2007 Alum Rock earthquake and implications for the origin of increased discharge after earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/j.1468-8123.2009.00250.x"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-68449094336"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/j.1468-8123.2009.00254.x",
"name": "Spring temperatures in the Sagehen Basin, Sierra Nevada, CA: Implications for heat flow and groundwater circulation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/j.1468-8123.2009.00254.x"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-68449096142"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.euromechflu.2008.11.001",
"name": "Steady shape of a miscible bubble rising below an inclined wall at low Reynolds numbers",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-62349084213"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.euromechflu.2008.11.001"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2008jb006216",
"name": "Transport capacity of pyroclastic density currents: Experiments and models of substrate-flow interaction",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-72049084726"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2008jb006216"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2009.01.040",
"name": "True Polar Wander driven by late-stage volcanism and the distribution of paleopolar deposits on Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2009.01.040"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-62549136046"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2007.09.032",
"name": "An improved crustal magnetic field map of Mars from electron reflectometry: Highland volcano magmatic history and the end of the martian dynamo",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2007.09.032"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-40849126608"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2007.10.017",
"name": "Equilibrium rotational stability and figure of Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-40849111864"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2007.10.017"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/science.1156630",
"name": "Formation of Box Canyon, Idaho, by megaflood: Implications for seepage erosion on earth and mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-44449127707"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/science.1156630"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2007jb005555",
"name": "In situ production of ash in pyroclastic flows",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2007jb005555"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-56449088651"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.ijheatfluidflow.2008.05.002",
"name": "Lattice Boltzmann model for melting with natural convection",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-51649121483"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.ijheatfluidflow.2008.05.002"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2008gl034338",
"name": "Rapid decrease in Martian crustal magnetization in the Noachian era: Implications for the dynamo and climate of early Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2008gl034338"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-53749103219"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2008.02.043",
"name": "Suspension rheology under oscillatory shear and its geophysical implications",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-43249085662"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2008.02.043"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2008.05.029",
"name": "The East Java mud volcano (2006 to present): An earthquake or drilling trigger?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-48149103199"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2008.05.029"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1111/j.1468-8123.2008.00208.x",
"name": "The influence of poorly interconnected fault zone flow paths on spring geochemistry",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1111/j.1468-8123.2008.00208.x"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-44349105386"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2007.07.020",
"name": "Transition between fragmentation and permeable outgassing of low viscosity magmas",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-36749045703"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2007.07.020"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1007/s00445-006-0081-6",
"name": "An experimental facility for investigating hydromagmatic eruptions at high-pressure and high-temperature with application to the importance of magma porosity for magma-water interaction",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1007/s00445-006-0081-6"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33846805975"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2007eo180009",
"name": "Did an earthquake trigger the May 2006 eruption of the Lusi mud volcano?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34347235874"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2007eo180009"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/b978-044452748-6.00074-2",
"name": "Earthquake Hydrology",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84882860391"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/b978-044452748-6.00074-2"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/nature05873",
"name": "Evidence for an ancient martian ocean in the topography of deformed shorelines",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/nature05873"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34250343436"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2006jb004910",
"name": "Littoral blasts: Pumice-water heat transfer and the conditions for steam explosions when pyroclastic flows enter the ocean",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-38349189101"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2006jb004910"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2007gl029297",
"name": "Pressurized oceans and the eruption of liquid water on Europa and Enceladus",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2007gl029297"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34250733536"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1146/annurev.fluid.39.050905.110207",
"name": "The fluid mechanics inside a volcano",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1146/annurev.fluid.39.050905.110207"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33846813717"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2007gl030565",
"name": "Thermal demagnetization of Martian upper crust by magma intrusion",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-35948943446"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2007gl030565"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2006gl027471",
"name": "Can freezing cause floods on Mars?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2006gl027471"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33845683799"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2005jb004132",
"name": "Influence of decompression rate on the expansion velocity and expansion style of bubbly fluids",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34547887704"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2005jb004132"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1785/0120050019",
"name": "Liquefaction limit during earthquakes and underground explosions: Implications on ground-motion attenuation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1785/0120050019"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33644527559"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2006je002710",
"name": "Long-period seismology on Europa: 1. Physically consistent interior models",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2006je002710"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34250769429"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2006je002712",
"name": "Long-period seismology on Europa: 2. Predicted seismic response",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2006je002712"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-34447509386"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2005.09.008",
"name": "Martian landslides in Valles Marineris: Wet or dry?",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2005.09.008"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-30744458617"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2006.01.004",
"name": "Origins and implications of zigzag rift patterns on lava lakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2006.01.004"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33744529799"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2005je002447",
"name": "Rotational stability of dynamic planets with elastic lithospheres",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2005je002447"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33645645327"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1146/annurev.earth.34.031405.125125",
"name": "Seismic triggering of eruptions in the far field: Volcanoes and geysers",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1146/annurev.earth.34.031405.125125"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33744948300"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2005gl024905",
"name": "Unusual magnetic signature of the Hadriaca Patera Volcano: Implications for early Mars",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2005gl024905"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33645817010"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.jvolgeores.2004.09.018",
"name": "Bubble suspension rheology and implications for conduit flow",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.jvolgeores.2004.09.018"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-19944380202"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2005.01.038",
"name": "Continental insulation, mantle cooling, and the surface area of oceans and continents",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-20344371195"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2005.01.038"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/0-8137-2396-5.47",
"name": "Deformation of flow bands by bubbles and crystals",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/0-8137-2396-5.47"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84874992275"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.icarus.2004.12.003",
"name": "Floods on Mars released from groundwater by impact",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-18144382276"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.icarus.2004.12.003"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2005.04.031",
"name": "Flow banding in obsidian: A record of evolving textural heterogeneity during magma deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2005.04.031"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-22144475795"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/0-8137-2396-5.v",
"name": "Geological Society of America: Preface",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/0-8137-2396-5.v"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-73949111033"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2005.07.021",
"name": "Nonequilibrium magma degassing: Results from modeling of the ca. 1340 A.D. eruption of Mono Craters, California",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-26944450074"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2005.07.021"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2004gc000828",
"name": "Quantifying magmatic, crustal, and atmospheric helium contributions to volcanic aquifers using all stable noble gases: Implications for magmatism and groundwater flow",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-27744492425"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2004gc000828"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2005.02.045",
"name": "Response of a bubble bearing viscoelastic fluid to rapid decompression: Implications for explosive volcanic eruptions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2005.02.045"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-22144451075"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/nature03620",
"name": "Seismological constraints on a possible plume root at the core-mantle boundary",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/nature03620"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-20444499401"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2005gl023165",
"name": "Vertical segregation in granular mass flows: A shear cell study",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-22444444810"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2005gl023165"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2005gl024029",
"name": "Vesiculation rates of obsidian domes inferred from H<inf>2</inf>O concentration profiles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2005gl024029"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-29344475975"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/g20753.1",
"name": "Coseismic release of water from mountains: Evidence from the 1999 (M<inf>w</inf> = 7.5) Chi-Chi, Taiwan, earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/g20753.1"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-4744338711"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2003jb002855",
"name": "Depth dependence of permeability in the Oregon Cascades inferred from hydrogeologic, thermal, seismic, and magmatic modeling constraints",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-3242789342"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2003jb002855"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2004jb002978",
"name": "Did melting glaciers cause volcanic eruptions in eastern California? Probing the mechanics of dike formation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-10044242747"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2004jb002978"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2004rg000164",
"name": "Erratum: \"Links between long-lived hot spots, mantle plumes, D\", and plate tectonics\" (Review of Geophysics vol. 42 (2004) 10.1029/2003RG00144)",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2004rg000164"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-14344254247"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2004je002249",
"name": "Formation of bands and ridges on Europa by cyclic deformation: Insights from analogue wax experiments",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2004je002249"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-11144329498"
}
]
},
{
"@type": "CreativeWork",
"name": "Interpreting the temperature of water at cold springs and the importance of gravitational potential energy",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-2942735343"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2003rg000144",
"name": "Links between long-lived hot spots, mantle plumes, D\u2033, and plate tectonics",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2003rg000144"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-7044259795"
}
]
},
{
"@type": "CreativeWork",
"name": "Martian floods at Cerberus Fossae can be produced by groundwater discharge",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-2442516065"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/j.epsl.2004.07.021",
"name": "Modulation of mantle plumes and heat flow at the core mantle boundary by plate-scale flow: Results from laboratory experiments",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-4544328751"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/j.epsl.2004.07.021"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1117/12.578430",
"name": "Multiple Instrument Distributed Aperture Sensor (MIDAS) for planetary remote sensing",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1117/12.578430"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-20344406814"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1117/12.565710",
"name": "Multiple Instrument Distributed Aperture Sensor (MIDAS) for remote sensing",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-20144389730"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1117/12.565710"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1117/12.560290",
"name": "Remote sensing space science enabled by the Multiple Instrument Distributed Aperture Sensor (MIDAS) concept",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1117/12.560290"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-20144384853"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2004gl020124",
"name": "Streamflow increase due to rupturing of hydrothermal reservoirs: Evidence from the 2003 San Simeon, California, earthquake",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-4143143065"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2004gl020124"
}
]
},
{
"@type": "CreativeWork",
"name": "Tharsis as a consequence of Mars' dichotomy and layered mantle",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-2542437758"
}
},
{
"@type": "CreativeWork",
"name": "Variation in the relationship between snowmelt runoff in Oregon and ENSO and PDO",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-4544284372"
}
},
{
"@type": "CreativeWork",
"name": "A mechanism for sustained groundwater pressure changes induced by distant earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0345376075"
}
},
{
"@type": "CreativeWork",
"name": "A technique for measuring 3D crystal-size distributions of prismatic microlites in obsidian",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0141785416"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/science.1083623",
"name": "Deep origin of hotspots -The mantle plume model",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/science.1083623"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0038670243"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0273(02)00487-0",
"name": "Determining flow type, shear rate and shear stress in magmas from bubble shapes and orientations",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0273(02)00487-0"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0242669983"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1023/a:1022312927606",
"name": "Effects of bubbles on the hydraulic conductivity of porous materials - Theoretical results",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037411022"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1023/a:1022312927606"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/nature02138",
"name": "Explosive volcanism may not be an inevitable consequence of magma fragmentation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0345414148"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/nature02138"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0169-555x(02)00335-5",
"name": "Field measurements of drag coefficients for model large woody debris",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037456683"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0169-555x(02)00335-5"
}
]
},
{
"@type": "CreativeWork",
"name": "Pumice-pumice collisions and the effect of the impact angle",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0347413662"
}
},
{
"@type": "CreativeWork",
"name": "Response of streamflow to multiple earthquakes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0042200446"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0012-821x(03)00418-7",
"name": "Seismicity induced by seasonal groundwater recharge at Mt. Hood, Oregon",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0141631699"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0012-821x(03)00418-7"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1126/science.1082980",
"name": "Streamflow and water well responses to earthquakes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1126/science.1082980"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037595560"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1006/jcis.2002.8292",
"name": "Bubble shapes and orientations in low Re simple shear flow",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1006/jcis.2002.8292"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0036353039"
}
]
},
{
"@type": "CreativeWork",
"name": "Causes, characteristics and consequences of convective diapirism on Europa",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0036956161"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1103/physreve.65.056131",
"name": "Continuum percolation for randomly oriented soft-core prisms",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-39749105807"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1103/physreve.65.056131"
}
]
},
{
"@type": "CreativeWork",
"name": "Dynamics and longevity of an initially stratified mantle",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037095936"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0012-821x(02)00559-9",
"name": "Dynamics of obsidian flows inferred from microstructures: Insights from microlite preferred orientations",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0036076208"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0012-821x(02)00559-9"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0257(02)00013-7",
"name": "Effects of bubble deformation on the viscosity of dilute suspensions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037140360"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0257(02)00013-7"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/nature00979",
"name": "The influence of a chemical boundary layer on the fixity, spacing and lifetime of mantle plumes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0037102163"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/nature00979"
}
]
},
{
"@type": "CreativeWork",
"name": "The influence of interior mantle temperature on the structure of plumes: Heads for Venus, tails for the Earth",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-35549013964"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1063/1.1345719",
"name": "Boundary-layer thickness and instabilities in B\u00e9nard convection of a liquid with a temperature-dependent viscosity",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1063/1.1345719"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0035276040"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2000gl012215",
"name": "Interaction of rising and sinking mantle plumes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2000gl012215"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0034744795"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0012-821x(01)00289-8",
"name": "Numerical models of the onset of yield strength in crystal-melt suspensions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0034988939"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0012-821x(01)00289-8"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/2000gl012481",
"name": "Origin of postseismic streamflow changes inferred from baseflow recession and magnitude-distance relations",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/2000gl012481"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0035874460"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1038/35074235",
"name": "Shaken, not stirred",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1038/35074235"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0035953542"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0273(00)00317-6",
"name": "The yield strength of subliquidus basalts - Experimental results",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0035361651"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0273(00)00317-6"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1146/annurev.earth.29.1.201",
"name": "Using springs to study groundwater flow and active geologic processes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0034979839"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1146/annurev.earth.29.1.201"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0273(00)00239-0",
"name": "Viscosity of magmas containing highly deformable bubbles",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0035100391"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0273(00)00239-0"
}
]
},
{
"@type": "CreativeWork",
"name": "Stress partitioning in streams by large woody debris",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0033868411"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1023/a:1006697532629",
"name": "The motion of long bubbles in a network of tubes",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0033913515"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1023/a:1006697532629"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0022-1694(00)00303-6",
"name": "The use of temperature and the isotopes of O, H, C, and noble gases to determine the pattern and spatial extent of groundwater flow",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0022-1694(00)00303-6"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0034715368"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/0091-7613(1999)027<0823:cditoc>2.3.co;2",
"name": "CO <inf>2</inf> degassing in the Oregon Cascades",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/0091-7613(1999)027<0823:cditoc>2.3.co;2"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0033378212"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/0091-7613(1999)027<0823:cditoc<2.3.co;2",
"name": "CO<inf>2</inf>degassing in the Oregon Cascades",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85045784620"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/0091-7613(1999)027<0823:cditoc<2.3.co;2"
}
]
},
{
"@type": "CreativeWork",
"name": "Experimental study of non-Boussinesq Rayleigh-B\u00e9nard convection at high Rayleigh and Prandtl numbers",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0001331517"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0022-1694(99)00044-x",
"name": "On the timescales characterizing groundwater discharge at springs",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0033052369"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0022-1694(99)00044-x"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/1998gl900256",
"name": "Permeability-porosity relationship in vesicular basalts",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/1998gl900256"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0032926473"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1130/0091-7613(1998)026<0799:ahtblt>2.3.co;2",
"name": "Advective heat transport by low-temperature discharge in the Oregon Cascades",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-84879888794"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1130/0091-7613(1998)026<0799:ahtblt>2.3.co;2"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/1998gl900023",
"name": "Erratum: High Rayleigh number thermo-chemical models of a dense boundary layer in D (Geophysical Research Letters (1998) 25:13 (2345-2348))",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/1998gl900023"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-33947528743"
}
]
},
{
"@type": "CreativeWork",
"name": "High Rayleigh number thermo-chemical models of a dense boundary layer in D\u2033",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0032125374"
}
},
{
"@type": "CreativeWork",
"name": "Non-equilibrium and unsteady fluid degassing during slow decompression",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0032534904"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0273(98)00084-5",
"name": "Orientation distribution of microlites in obsidian",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0032467474"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0273(98)00084-5"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0377-0273(98)00091-2",
"name": "Rheology of bubble-bearing magmas",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0377-0273(98)00091-2"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0002217286"
}
]
},
{
"@type": "CreativeWork",
"name": "The low-Reynolds number spreading of axisymmetric drops and gravity currents along a free surface",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-2042445466"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/s0012-821x(98)00111-3",
"name": "Transitions in the style of mantle convection at high Rayleigh numbers",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0032448737"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/s0012-821x(98)00111-3"
}
]
},
{
"@type": "CreativeWork",
"name": "A model for discharge in spring-dominated streams and implications for the transmissivity and recharge of quaternary volcanics in the Oregon Cascades",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030747804"
}
},
{
"@type": "CreativeWork",
"name": "Interactions between mantle diapirs",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0031200976"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/gm101p0017",
"name": "Temperature distribution in the laser-heated diamond cell",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-85040130181"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/gm101p0017"
}
]
},
{
"@type": "CreativeWork",
"name": "Thermal conductivity of corundum and periclase and implications for the lower mantle",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030792758"
}
},
{
"@type": "CreativeWork",
"name": "Axial temperature gradients in dielectric samples in the laser-heated diamond cell",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030186116"
}
},
{
"@type": "CreativeWork",
"name": "Dynamics of drops in branched tubes",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030131260"
}
},
{
"@type": "CreativeWork",
"name": "Dynamics of drops in cavity flows: Aggregation of high viscosity ratio drops",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029671952"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/96wr01238",
"name": "Hydrology of spring-dominated streams in the Oregon cascades",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/96wr01238"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029663827"
}
]
},
{
"@type": "CreativeWork",
"name": "Implications of a metal-bearing chemical boundary layer in D\" for mantle dynamics",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030292011"
}
},
{
"@type": "CreativeWork",
"name": "Mixing of heterogeneities in the mantle: Effect of viscosity differences",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029729544"
}
},
{
"@type": "CreativeWork",
"name": "Neutrally buoyant diapirs: A model for venus coronae",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029731124"
}
},
{
"@type": "CreativeWork",
"name": "Waves of bubbles in basaltic magmas and lavas",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0030423429"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1017/s0022112095003673",
"name": "Collective Hydrodynamics of Deformable Drops and Bubbles in Dilute Low Reynolds Number Suspensions",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1017/s0022112095003673"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029415932"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1017/s0022112095000954",
"name": "Low reynolds number motion of bubbles, drops and rigid spheres through fluid-fluid interfaces",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029104074"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1017/s0022112095000954"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1029/95gl02012",
"name": "The tectosphere and postglacial rebound",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1029/95gl02012"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0029473551"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/0377-0273(94)90079-5",
"name": "Interactions between bubbles in magmas and lavas: effects of bubble deformation",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0028583535"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/0377-0273(94)90079-5"
}
]
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1017/s0022112093002915",
"name": "Buoyancy-Driven Interactions Between Two Deformable Viscous Drops",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0001206701"
},
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1017/s0022112093002915"
}
]
},
{
"@type": "CreativeWork",
"name": "The interaction of plume heads with compositional discontinuities in the Earth's mantle",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0027834931"
}
},
{
"@type": "CreativeWork",
"name": "Boundary integral methods for viscous free-boundary problems: deformation of single and multiple fluid-fluid interfaces",
"identifier": {
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0027001590"
}
},
{
"@type": "CreativeWork",
"@id": "https://doi.org/10.1016/0031-9201(91)90003-z",
"name": "Remelting mechanisms for shallow source regions of mare basalts",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "doi",
"value": "10.1016/0031-9201(91)90003-z"
},
{
"@type": "PropertyValue",
"propertyID": "eid",
"value": "2-s2.0-0026273093"
}
]
}
]
},
"url": "http://seismo.berkeley.edu/~manga",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "Loop profile",
"value": "654395"
},
{
"@type": "PropertyValue",
"propertyID": "Scopus Author ID",
"value": "7006760316"
}
]
}
}
