{"@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/1361418520307542272.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005jb004062"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JB004062"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JB004062"}}],"dc:title":[{"@value":"Seismicity and one‐dimensional velocity structure of the Himalayan collision zone: Earthquakes in the crust and upper mantle"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Earthquakes beneath the Himalayan collision zone occur at depths between near surface and around 100 km below sea level. After relocating earthquakes with two one‐dimensional (1‐D) velocity models, we found a clear bimodal depth distribution for earthquakes in the Himalayas of eastern Nepal and the southern Tibetan Plateau and evidence that some earthquakes originate at upper mantle depths. Seismicity in Nepal shows an accumulation of earthquakes along the front of the Himalayan arc, with a seismic gap between longitudes 87.3°E and 87.7°E. Although upper crustal seismicity along the topographic front of the High Himalaya is consistent with a region of high strain accumulation associated with convergence on the Main Himalayan thrust fault, microearthquakes do not necessarily occur on this fault. Instead, they concentrate in the hanging wall. Seismic activity in the sub‐Himalaya and the Terai Plains is almost exclusively limited to the vicinity of the location of the magnitude 6.5 20 August 1988 Udayapur earthquake, with most of the earthquakes in the lower crust and the upper mantle. Clusters of earthquakes in the Lesser and High Himalayas and south Tibet (Tethyan Himalayas) mark very well defined zones of seismicity at depths between 50 and 100 km, confirming the presence of earthquakes in the upper mantle in the region of continental collision. The occurrence of earthquakes at sub‐Moho depths favors the idea that the continental upper mantle deforms by brittle processes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236852745608","@type":"Researcher","foaf:name":[{"@value":"G. Monsalve"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences and CIRES University of Colorado  Boulder Colorado USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520307542274","@type":"Researcher","foaf:name":[{"@value":"A. Sheehan"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences and CIRES University of Colorado  Boulder Colorado USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016868421759104","@type":"Researcher","foaf:name":[{"@value":"V. Schulte‐Pelkum"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences and CIRES University of Colorado  Boulder Colorado USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520307542275","@type":"Researcher","foaf:name":[{"@value":"S. Rajaure"}],"jpcoar:affiliationName":[{"@value":"Department of Mines and Geology National Seismological Centre  Kathmandu Nepal"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520307542273","@type":"Researcher","foaf:name":[{"@value":"M. R. Pandey"}],"jpcoar:affiliationName":[{"@value":"Department of Mines and Geology National Seismological Centre  Kathmandu Nepal"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520307542276","@type":"Researcher","foaf:name":[{"@value":"F. Wu"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences and Environmental Studies State University of New York at Binghamton  Binghamton New York USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2006-10","prism:volume":"111","prism:number":"B10","prism:startingPage":"B10301"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JB004062"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JB004062"}],"createdAt":"2006-10-02","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050306506454177152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of 1-D velocity models beneath strong-motion observation sites in the Kathmandu Valley using strong-motion records from moderate-sized earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506455246592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aftershock activity of the 2015 Gorkha, Nepal, earthquake determined using the Kathmandu strong motion seismographic array"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942213120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tomographic imaging of the underthrusting Indian slab and mantle upwelling beneath central Tibet"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216113788160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tomography of the source zone of the 2015 M 7.8 Nepal earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390566775132635392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Indo–Eurasia convergent margin and earthquakes in and around Tibetan Plateau"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005jb004062"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0685-4_references_DOI_QZzd0gX0qhx9kAwXt0fsrcxnLSk"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0402-8_references_DOI_XkoIKJaj72RWaKq8h7l0sFF38cY"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2014.02.012_references_DOI_XkoIKJaj72RWaKq8h7l0sFF38cY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2016.01.008_references_DOI_XkoIKJaj72RWaKq8h7l0sFF38cY"},{"@type":"CROSSREF","@value":"10.2465/jmps.190927_references_DOI_XkoIKJaj72RWaKq8h7l0sFF38cY"}]}