{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362262943317137280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gl025109"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL025109"}}],"dc:title":[{"@value":"InSAR constraints on the source parameters of the 2001 Bhuj earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We present InSAR results of the coseismic displacement field for the January 2001 Bhuj earthquake. Using InSAR data along multiple tracks, we determine the optimal source parameters of the earthquake. The deformation pattern is first modeled assuming uniform slip on an elastic dislocation. A grid search is used to constrain the source location and finiteness assuming a strike, rake, and dip consistent with seismic studies. An inversion for the distributed slip places oblique reverse slip at depth with strike‐slip motion resolved at shallower depths. The estimated size of the event is M<jats:sub><jats:italic>w</jats:italic></jats:sub> 7.6. Results also suggest that the postseismic response is minimal.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004054083349762","@type":"Researcher","foaf:name":[{"@value":"D. A. Schmidt"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences University of Oregon  Eugene Oregon USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943317137280","@type":"Researcher","foaf:name":[{"@value":"R. Bürgmann"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science University of California  Berkeley California USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2006-01","prism:volume":"33","prism:number":"2","prism:startingPage":"L02315"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL025109"}],"createdAt":"2006-01-27","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202707280384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640349255936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Postseismic relaxation due to Bhuj earthquake on January 26, 2001: possible mechanisms and processes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gl025109"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0580-4_references_DOI_H7jXipDVM2pHnRPczas3VS4G7dR"},{"@type":"CROSSREF","@value":"10.1007/s11069-012-0184-7_references_DOI_H7jXipDVM2pHnRPczas3VS4G7dR"}]}