1,461,255
edits
(Created page with "{ "OpenAlex": { "id": "https://openalex.org/A5007764926", "orcid": "https://orcid.org/0000-0002-7760-7236", "display_name": "Alison R. Duvall", "display_name_alternatives": [ "A. R. Duvall", "Allen Duvall", "A. Duvall", "Alison R. Duvall", "Alison Duvall" ], "works_count": 85, "cited_by_count": 2337, "summary_stats": { "2yr_mean_citedness": 1.4444444444444444, "h_index": 17, "i10_index": 18...") |
No edit summary |
||
Line 1,224: | Line 1,224: | ||
"created_date": "2023-07-21", | "created_date": "2023-07-21", | ||
"_id": "https://openalex.org/A5007764926" | "_id": "https://openalex.org/A5007764926" | ||
}, | |||
"ORCID": { | |||
"@context": "http://schema.org", | |||
"@type": "Person", | |||
"@id": "https://orcid.org/0000-0002-7760-7236", | |||
"mainEntityOfPage": "https://orcid.org/0000-0002-7760-7236", | |||
"givenName": "Alison", | |||
"familyName": "Duvall", | |||
"alumniOf": { | |||
"@type": "Organization", | |||
"name": "University of California Santa Barbara", | |||
"alternateName": "Department of Earth Science", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "RINGGOLD", | |||
"value": "8786" | |||
} | |||
}, | |||
"@reverse": { | |||
"creator": [ | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1785/0120230079", | |||
"name": "Evidence of Seattle Fault Earthquakes from Patterns in Deep-Seated Landslides", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1785/0120230079" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1029/2023gl105066", | |||
"name": "The Lasting Legacy of Megaflood Boulder Deposition in Mountain Rivers", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1029/2023gl105066" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.5194/egusphere-egu23-3684", | |||
"name": "Are spatial and temporal patterns of landslide triggering events reflected in topography and sediment dynamics?", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.5194/egusphere-egu23-3684" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1029/2021tc006704", | |||
"name": "Multiphase Topographic and Thermal Histories of the Wallowa and Elkhorn Mountains, Blue Mountains Province, Oregon, USA", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1029/2021tc006704" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1038/s41467-021-27587-9", | |||
"name": "Existence of a continental-scale river system in eastern Tibet during the late Cretaceous\u2013early Palaeogene", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1038/s41467-021-27587-9" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.5194/egusphere-egu21-3281", | |||
"name": "Landscape Records 25 Million Years of Tectonic Evolution at an Oblique Convergent Margin, Marlborough Fault System, New Zealand", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.5194/egusphere-egu21-3281" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1126/sciadv.aba6790", | |||
"name": "Rainfall triggers more deep-seated landslides than Cascadia earthquakes in the Oregon Coast Range, USA", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1126/sciadv.aba6790" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1029/2018tc005268", | |||
"name": "The Timing and Style of Oblique Deformation Within New Zealand's Kaik\u014dura Ranges and Marlborough Fault System Based on Low\u2010Temperature Thermochronology", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1029/2018tc005268" | |||
} | |||
}, | |||
{ | |||
"@type": "CreativeWork", | |||
"@id": "https://doi.org/10.1029/2018gl080045", | |||
"name": "The Role of Near\u2010Fault Relief Elements in Creating and Maintaining a Strike\u2010Slip Landscape", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "doi", | |||
"value": "10.1029/2018gl080045" | |||
} | |||
} | |||
] | |||
} | |||
} | } | ||
} | } |