FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2776466115> ?p ?o ?g. }

• W2776466115 endingPage "1730" @default.
• W2776466115 startingPage "1720" @default.
• W2776466115 abstract "The 2010 Mw7.2 El Mayor-Cucapah earthquake provides a unique target of postseismic study as deformation extends across several distinct geological provinces, including the cold Mesozoic arc crust of the Peninsular Ranges and newly formed, hot, extending lithosphere within the Salton Trough. We use five years of global positioning system measurements to invert for afterslip and constrain a 3-D finite-element model that simulates viscoelastic relaxation. We find that afterslip cannot readily explain far-field displacements (more than 50 km from the epicentre). These displacements are best explained by viscoelastic relaxation of a horizontally and vertically heterogeneous lower crust and upper mantle. Lower viscosities beneath the Salton Trough compared to the Peninsular Ranges and other surrounding regions are consistent with inferred differences in the respective geotherms. Our inferred viscosity structure suggests that the depth of the Lithosphere/Asthenosphere Boundary (LAB) is ∼65 km below the Peninsular Ranges and ∼32 km beneath the Salton Trough. These depths are shallower than the corresponding seismic LAB. This suggests that the onset of partial melting in peridotite may control the depth to the base of the mechanical lithosphere. In contrast, the seismic LAB may correspond to an increase in the partial melt percentage associated with the change from a conductive to an adiabatic geotherm." @default.
• W2776466115 created "2018-01-05" @default.
• W2776466115 creator A5001510524 @default.
• W2776466115 creator A5028594811 @default.
• W2776466115 creator A5033563191 @default.
• W2776466115 creator A5051538825 @default.
• W2776466115 creator A5054964856 @default.
• W2776466115 creator A5058475164 @default.
• W2776466115 date "2017-12-18" @default.
• W2776466115 modified "2023-10-03" @default.
• W2776466115 title "Inferred rheological structure and mantle conditions from postseismic deformation following the 2010 Mw 7.2 El Mayor-Cucapah Earthquake" @default.
• W2776466115 cites W1663438417 @default.
• W2776466115 cites W1938551673 @default.
• W2776466115 cites W1964340600 @default.
• W2776466115 cites W1976870970 @default.
• W2776466115 cites W1982926192 @default.
• W2776466115 cites W1983786019 @default.
• W2776466115 cites W1988497895 @default.
• W2776466115 cites W1995741527 @default.
• W2776466115 cites W1996561698 @default.
• W2776466115 cites W2008568398 @default.
• W2776466115 cites W2012177214 @default.
• W2776466115 cites W2024982969 @default.
• W2776466115 cites W2035214985 @default.
• W2776466115 cites W2050480893 @default.
• W2776466115 cites W2052398390 @default.
• W2776466115 cites W2072726855 @default.
• W2776466115 cites W2094713134 @default.
• W2776466115 cites W2098499896 @default.
• W2776466115 cites W2100613167 @default.
• W2776466115 cites W2106744270 @default.
• W2776466115 cites W2118741753 @default.
• W2776466115 cites W2120794222 @default.
• W2776466115 cites W2126336964 @default.
• W2776466115 cites W2142680641 @default.
• W2776466115 cites W2148674466 @default.
• W2776466115 cites W2156402670 @default.
• W2776466115 cites W2170409103 @default.
• W2776466115 cites W2513478303 @default.
• W2776466115 cites W2532091368 @default.
• W2776466115 cites W2552141328 @default.
• W2776466115 cites W2775235778 @default.
• W2776466115 cites W3016180305 @default.
• W2776466115 cites W4233532201 @default.
• W2776466115 doi "https://doi.org/10.1093/gji/ggx546" @default.
• W2776466115 hasPublicationYear "2017" @default.
• W2776466115 type Work @default.
• W2776466115 sameAs 2776466115 @default.
• W2776466115 citedByCount "7" @default.
• W2776466115 countsByYear W27764661152019 @default.
• W2776466115 countsByYear W27764661152020 @default.
• W2776466115 countsByYear W27764661152022 @default.
• W2776466115 crossrefType "journal-article" @default.
• W2776466115 hasAuthorship W2776466115A5001510524 @default.
• W2776466115 hasAuthorship W2776466115A5028594811 @default.
• W2776466115 hasAuthorship W2776466115A5033563191 @default.
• W2776466115 hasAuthorship W2776466115A5051538825 @default.
• W2776466115 hasAuthorship W2776466115A5054964856 @default.
• W2776466115 hasAuthorship W2776466115A5058475164 @default.
• W2776466115 hasBestOaLocation W27764661152 @default.
• W2776466115 hasConcept C122959257 @default.
• W2776466115 hasConcept C127313418 @default.
• W2776466115 hasConcept C13495919 @default.
• W2776466115 hasConcept C139719470 @default.
• W2776466115 hasConcept C162324750 @default.
• W2776466115 hasConcept C165205528 @default.
• W2776466115 hasConcept C16942324 @default.
• W2776466115 hasConcept C2776698055 @default.
• W2776466115 hasConcept C32239851 @default.
• W2776466115 hasConcept C67236022 @default.
• W2776466115 hasConcept C77928131 @default.
• W2776466115 hasConcept C79572550 @default.
• W2776466115 hasConcept C8058405 @default.
• W2776466115 hasConcept C84372278 @default.
• W2776466115 hasConceptScore W2776466115C122959257 @default.
• W2776466115 hasConceptScore W2776466115C127313418 @default.
• W2776466115 hasConceptScore W2776466115C13495919 @default.
• W2776466115 hasConceptScore W2776466115C139719470 @default.
• W2776466115 hasConceptScore W2776466115C162324750 @default.
• W2776466115 hasConceptScore W2776466115C165205528 @default.
• W2776466115 hasConceptScore W2776466115C16942324 @default.
• W2776466115 hasConceptScore W2776466115C2776698055 @default.
• W2776466115 hasConceptScore W2776466115C32239851 @default.
• W2776466115 hasConceptScore W2776466115C67236022 @default.
• W2776466115 hasConceptScore W2776466115C77928131 @default.
• W2776466115 hasConceptScore W2776466115C79572550 @default.
• W2776466115 hasConceptScore W2776466115C8058405 @default.
• W2776466115 hasConceptScore W2776466115C84372278 @default.
• W2776466115 hasIssue "3" @default.
• W2776466115 hasLocation W27764661151 @default.
• W2776466115 hasLocation W27764661152 @default.
• W2776466115 hasLocation W27764661153 @default.
• W2776466115 hasOpenAccess W2776466115 @default.
• W2776466115 hasPrimaryLocation W27764661151 @default.
• W2776466115 hasRelatedWork W1980996103 @default.
• W2776466115 hasRelatedWork W2005516122 @default.
• W2776466115 hasRelatedWork W2023835615 @default.
• W2776466115 hasRelatedWork W2052508457 @default.

• next