1,461,255
edits
(Created page with "{ "OpenAlex": { "id": "https://openalex.org/A5013434425", "orcid": "https://orcid.org/0000-0003-2015-6419", "display_name": "Rebecca Carey", "display_name_alternatives": [ "R. J. Carey", "Rebecca J. Carey", "R. Carey", "Rebecca Jane Carey", "Rebecca Carey" ], "works_count": 132, "cited_by_count": 2081, "summary_stats": { "2yr_mean_citedness": 1.4545454545454546, "h_index": 26, "i10_index":...") |
No edit summary |
||
Line 1,297: | Line 1,297: | ||
"created_date": "2023-07-21", | "created_date": "2023-07-21", | ||
"_id": "https://openalex.org/A5013434425" | "_id": "https://openalex.org/A5013434425" | ||
}, | |||
"ORCID": { | |||
"@context": "http://schema.org", | |||
"@type": "Person", | |||
"@id": "https://orcid.org/0000-0003-2015-6419", | |||
"mainEntityOfPage": "https://orcid.org/0000-0003-2015-6419", | |||
"givenName": "Rebecca", | |||
"familyName": "Carey", | |||
"affiliation": { | |||
"@type": "Organization", | |||
"@id": "https://doi.org/10.13039/501100009193", | |||
"name": "Marsden Fund", | |||
"alternateName": "Earth Sciences and Astronomy Panel" | |||
}, | |||
"@reverse": { | |||
"funder": { | |||
"@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" | |||
} | |||
] | |||
}, | |||
"creator": [ | |||
{ | |||
"@type": "CreativeWork", | |||
"name": "Reconceptualising'community'to identify place-based disaster management needs in Tasmania" | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.3389/feart.2019.00001", | |||
"name": "Characteristics and deposit stratigraphy of submarine-erupted silicic ash, havre volcano, kermadec arc, New Zealand", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.3389/feart.2019.00001" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85062193501" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1029/2018gl081609", | |||
"name": "Decrease in Seismic Velocity Observed Prior to the 2018 Eruption of K\u012blauea Volcano With Ambient Seismic Noise Interferometry", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85064079215" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1029/2018gl081609" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2018.11.011", | |||
"name": "Eruption and fountaining dynamics of selected 1985\u20131986 high fountaining episodes at K\u012blauea volcano, Hawai'i, from quantitative vesicle microtexture analysis", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2018.11.011" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85057085614" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g46033c.1", | |||
"name": "Physical constraints for effective magma-water interaction along volcanic conduits during silicic explosive eruptions", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g46033c.1" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85065543802" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g45657.1", | |||
"name": "Unusual fluidal behavior of a silicic magma during fragmentation in a deep subaqueous eruption, Havre volcano, southwestern Pacific Ocean", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g45657.1" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85065533939" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.epsl.2018.04.053", | |||
"name": "Dynamics of a powerful deep submarine eruption recorded in H<inf>2</inf>O contents and speciation in rhyolitic glass: The 2012 Havre eruption", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85047098846" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.epsl.2018.04.053" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.3389/feart.2018.00147", | |||
"name": "The eruption of submarine rhyolite lavas and domes in the deep ocean \u2013 Havre 2012, Kermadec Arc", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85057099797" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.3389/feart.2018.00147" | |||
} | |||
] | |||
}, | |||
{ | |||
"@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.2018.02.025", | |||
"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/10.1016/j.jvolgeores.2018.04.001", | |||
"name": "Total grain-size distribution of four subplinian\u2013Plinian tephras from Hekla volcano, Iceland: Implications for sedimentation dynamics and eruption source parameters", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85045567876" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2018.04.001" | |||
} | |||
] | |||
}, | |||
{ | |||
"@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", | |||
"name": "New Frontiers and Technologies in Submarine Volcanism Research" | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-017-1120-1", | |||
"name": "High magma decompression rates at the peak of a violent caldera-forming eruption (Lower Pumice 1 eruption, Santorini, Greece)", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-017-1120-1" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85019092216" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1002/2017jb014783", | |||
"name": "Permeability During Magma Expansion and Compaction", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1002/2017jb014783" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85039147813" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2017.05.034", | |||
"name": "The initiation and development of a caldera-forming Plinian eruption (172\u00a0ka Lower Pumice 2 eruption, Santorini, Greece)", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85021068970" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2017.05.034" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-016-1059-7", | |||
"name": "Dispersal of key subplinian\u2013Plinian tephras from Hekla volcano, Iceland: implications for eruption source parameters", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84986302053" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-016-1059-7" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g37423.1", | |||
"name": "Stronger or longer: Discriminating between Hawaiian and Strombolian eruption styles", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84962696884" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g37423.1" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"name": "Dynamics of reticulite-producing fountains from ring fractures in Kilauea Caldera ca. 1500 CE" | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1002/9781118872079.ch19", | |||
"name": "Onset of a basaltic explosive eruption: Halema'uma'u 2008", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1002/9781118872079.ch19" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84982216244" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1002/9781118872079", | |||
"name": "Hawaiian Volcanoes", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1002/9781118872079" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.epsl.2014.10.045", | |||
"name": "Dynamics of an open basaltic magma system: The 2008 activity of the Halema'uma'u Overlook vent, K\u012blauea Caldera", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.epsl.2014.10.045" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84915820735" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"name": "Preface", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85023749590" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/b978-0-12-385938-9.00034-1", | |||
"name": "Pyroclastic Fall Deposits", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/b978-0-12-385938-9.00034-1" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1002/9781118872079.ch16", | |||
"name": "Reticulite\u2010producing fountains from ring fractures in k\u0131 \u0304lauea caldera ca. 1500 ce", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1002/9781118872079.ch16" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-85027867829" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-014-0836-4", | |||
"name": "Deposition and generation of multiple widespread fall units from the c. AD 1314 Kaharoa rhyolitic eruption, Tarawera, New Zealand", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84904522722" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-014-0836-4" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1002/2014eo190001", | |||
"name": "Discovery of the largest historic silicic submarine eruption", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84900869154" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1002/2014eo190001" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1038/ncomms4660", | |||
"name": "On the fate of pumice rafts formed during the 2012 Havre submarine eruption", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1038/ncomms4660" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84899101202" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g35400.1", | |||
"name": "The 1800a Taupo eruption: \"Ill wind\" blows the ultraplinian type event down to Plinian", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g35400.1" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84898856408" | |||
} | |||
] | |||
}, | |||
{ | |||
"@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/10.1016/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/10.1130/g34146.1", | |||
"name": "Pushing the volcanic explosivity index to its limit and beyond: Constraints from exceptionally weak explosive eruptions at Kilauea in 2008", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g34146.1" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-84878191178" | |||
} | |||
] | |||
}, | |||
{ | |||
"@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/10.1016/j.jvolgeores.2011.04.009", | |||
"name": "A model for syn-eruptive groundwater flow during the phreatoplinian phase of the 28-29 March 1875 Askja volcano eruption, Iceland", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-79957929908" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2011.04.009" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g31509.1", | |||
"name": "Pigeonholing pyroclasts: Insights from the 19 March 2008 explosive eruption of K\u012blauea volcano", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-79951715431" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g31509.1" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1130/g30573.1", | |||
"name": "\"Inheritance\": An influence on the particle size of pyroclastic deposits", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-77954163938" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1130/g30573.1" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2010.06.002", | |||
"name": "Diverse patterns of ascent, degassing, and eruption of rhyolite magma during the 1.8ka Taupo eruption, New Zealand: Evidence from clast vesicularity", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-77955055631" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2010.06.002" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-009-0317-3", | |||
"name": "Tephra dispersal and eruption dynamics of wet and dry phases of the 1875 eruption of Askja Volcano, Iceland", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-009-0317-3" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-77952799887" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2009.04.003", | |||
"name": "Abrupt shifts between wet and dry phases of the 1875 eruption of Askja Volcano: Microscopic evidence for macroscopic dynamics", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2009.04.003" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-67649506209" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"name": "Eruption mechanisms during the climax of the Tarawera 1886 basaltic Plinian eruption inferred from microtextural characteristics-of the deposits", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-78649539918" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2007.11.020", | |||
"name": "Contrasting styles of welding observed in the proximal Askja 1875 eruption deposits I: Regional welding", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2007.11.020" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-40849095792" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2007.11.017", | |||
"name": "Contrasting styles of welding observed in the proximal Askja 1875 eruption deposits II: Local welding", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2007.11.017" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-40849106317" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-007-0117-6", | |||
"name": "Contrasting grain size and componentry in complex proximal deposits of the 1886 Tarawera basaltic Plinian eruption", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-34447520218" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-007-0117-6" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1007/s00445-006-0057-6", | |||
"name": "Complex proximal sedimentation from Plinian plumes: The example of Tarawera 1886", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1007/s00445-006-0057-6" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-33746276127" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1016/j.jvolgeores.2004.05.009", | |||
"name": "The influence of conduit processes on changes in style of basaltic Plinian eruptions: Tarawera 1886 and Etna 122 BC", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1016/j.jvolgeores.2004.05.009" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "eid", | |||
"value": "2-s2.0-17644362678" | |||
} | |||
] | |||
} | |||
] | |||
}, | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "Scopus Author ID", | |||
"value": "24738905600" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "ResearcherID", | |||
"value": "A-5381-2013" | |||
} | |||
] | |||
} | } | ||
} | } |