FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W234830331> ?p ?o ?g. }

• W234830331 startingPage "9683" @default.
• W234830331 abstract "The May 12, 2008 Wenchuan earthquake (Mw7.9) took place at the transition between the mountainous chain of Shan and the basin of Sichuan along the Longmen Shan Fault zone (31.1oN, 103.3oE; USGS). With a magnitude of 7.9 and a depth of ∼19 km the earthquake produced a 300-km-long fault rupture. It was the largest earthquake recorded in the region during the last centuries. It claimed more than 69,000 lives, induced widespread destruction over the region and raised concern about seismic hazard and source characterization for the Sichuan province. In the frame of our study, we selected 40 broadband waveforms (IRIS Consortium, USA) with good quality and satisfactory azimuthal coverage. Body waveforms were prepared for inversion using Kikuchi and Kanamori’s method [1] to obtain the spatiotemporal slip distribution of a finite rupture model (length=300 km, strike=229o, dip=33o, width=60 km). The slip distribution model obtained was used to determine the coseismic deformation and the stress change distribution using the Coulomb 3.0 software [2]. Our coseismic deformation results was compared with data from GPS stations located near the fault rupture. Results show that directions of coseismic deformations are consistent with GPS observations close to the fault. Finally, we compare aftershock hypocenters that occurred during one month after the main shock with the Coulomb stress changes caused by this shock in the region. We observed that most aftershocks are located along the main fault plane without any noticeable clustering in the areas of increased stress. Our results suggest the rupture of the 2008 Wenchuan earthquake was essentially unilateral, from SW to NE (N49E), covering a 260km length and with duration about 105 sec. The strongest moment release occurred about 85km from the hypocenter, ∼30sec after the start of the rupture. Motions are dominated by thrust mechanism, but the superficial section of the second half of the rupture also shows a significant strike-slip component." @default.
• W234830331 created "2016-06-24" @default.
• W234830331 creator A5016137386 @default.
• W234830331 creator A5020785034 @default.
• W234830331 creator A5026068506 @default.
• W234830331 creator A5042461715 @default.
• W234830331 date "2010-05-01" @default.
• W234830331 modified "2023-09-22" @default.
• W234830331 title "Slip distribution, coseismic deformation and Coulomb stress change for the 12 May 2008 Wenchuan (China, Mw7.9) earthquake" @default.
• W234830331 cites W2275750751 @default.
• W234830331 hasPublicationYear "2010" @default.
• W234830331 type Work @default.
• W234830331 sameAs 234830331 @default.
• W234830331 citedByCount "0" @default.
• W234830331 crossrefType "journal-article" @default.
• W234830331 hasAuthorship W234830331A5016137386 @default.
• W234830331 hasAuthorship W234830331A5020785034 @default.
• W234830331 hasAuthorship W234830331A5026068506 @default.
• W234830331 hasAuthorship W234830331A5042461715 @default.
• W234830331 hasConcept C121332964 @default.
• W234830331 hasConcept C127313418 @default.
• W234830331 hasConcept C13280743 @default.
• W234830331 hasConcept C156801008 @default.
• W234830331 hasConcept C165205528 @default.
• W234830331 hasConcept C175551986 @default.
• W234830331 hasConcept C195268267 @default.
• W234830331 hasConcept C97355855 @default.
• W234830331 hasConceptScore W234830331C121332964 @default.
• W234830331 hasConceptScore W234830331C127313418 @default.
• W234830331 hasConceptScore W234830331C13280743 @default.
• W234830331 hasConceptScore W234830331C156801008 @default.
• W234830331 hasConceptScore W234830331C165205528 @default.
• W234830331 hasConceptScore W234830331C175551986 @default.
• W234830331 hasConceptScore W234830331C195268267 @default.
• W234830331 hasConceptScore W234830331C97355855 @default.
• W234830331 hasLocation W2348303311 @default.
• W234830331 hasOpenAccess W234830331 @default.
• W234830331 hasPrimaryLocation W2348303311 @default.
• W234830331 hasRelatedWork W1939344824 @default.
• W234830331 hasRelatedWork W1969816273 @default.
• W234830331 hasRelatedWork W2002327323 @default.
• W234830331 hasRelatedWork W2026187630 @default.
• W234830331 hasRelatedWork W2028095547 @default.
• W234830331 hasRelatedWork W2048735209 @default.
• W234830331 hasRelatedWork W2080278598 @default.
• W234830331 hasRelatedWork W2084804351 @default.
• W234830331 hasRelatedWork W2351770240 @default.
• W234830331 hasRelatedWork W2574256538 @default.
• W234830331 hasRelatedWork W2774393737 @default.
• W234830331 hasRelatedWork W2895498186 @default.
• W234830331 hasRelatedWork W2982166882 @default.
• W234830331 hasRelatedWork W2992896272 @default.
• W234830331 hasRelatedWork W3095686084 @default.
• W234830331 hasRelatedWork W3101075761 @default.
• W234830331 hasRelatedWork W3103890699 @default.
• W234830331 hasRelatedWork W3109198537 @default.
• W234830331 hasRelatedWork W3127665758 @default.
• W234830331 hasRelatedWork W3981355 @default.
• W234830331 isParatext "false" @default.
• W234830331 isRetracted "false" @default.
• W234830331 magId "234830331" @default.
• W234830331 workType "article" @default.