{"@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/1363388845392009472.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004jb003421"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003421"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003421"}}],"dc:title":[{"@value":"Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We derive a detailed horizontal velocity field for the southeast borderland of the Tibetan Plateau using GPS data collected from the Crustal Motion Observation Network of China between 1998 and 2004. Our results reveal a complex deformation field that indicates that the crust is fragmented into tectonic blocks of various sizes, separated by strike‐slip and transtensional faults. Most notably, the regional deformation includes 10–11 mm/yr left slip across the Xianshuihe fault, ∼7 mm/yr left slip across the Anninghe‐Zemuhe‐Xiaojiang fault zone, ∼2 mm/yr right slip across a shear zone trending northwest near the southern segment of the Lancang River fault, and ∼3 mm/yr left slip across the Lijiang fault. Deformation along the southern segment of the Red River fault appears not significant at present time. The region south and west of the Xianshuihe‐Xiaojiang fault system, whose eastward motion is resisted by the stable south China block to the east, turns from eastward to southward motion with respect to south China, resulting in clockwise rotation of its internal subblocks. Active deformation is detected across two previously unknown deformation zones: one is located ∼150 km northwest of and in parallel with the Longmenshan fault with 4–6 mm/yr right‐slip and another is continued south‐southwestward from the Xiaojiang fault abutting the Red River fault with ∼7 mm/yr left slip. While both of these zones are seismically active, the exact locations of faults responsible for such deformation are yet to be mapped by field geology. Comparing our GPS results with predictions of various models proposed for Tibetan Plateau deformation, we find that the relatively small sizes of the inferred microblocks and their rotation pattern lend support to a model with a mechanically weak lower crust experiencing distributed deformation underlying a stronger, highly fragmented upper crust.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579817220720512","@type":"Researcher","foaf:name":[{"@value":"Zheng‐Kang Shen"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earthquake Dynamics, Institute of Geology China Earthquake Administration  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845392009474","@type":"Researcher","foaf:name":[{"@value":"Jiangning Lü"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics Peking University  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845392009472","@type":"Researcher","foaf:name":[{"@value":"Min Wang"}],"jpcoar:affiliationName":[{"@value":"Institute of Earthquake Science China Earthquake Administration  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845392009473","@type":"Researcher","foaf:name":[{"@value":"Roland Bürgmann"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science University of California  Berkeley California 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":"2005-11","prism:volume":"110","prism:number":"B11","prism:startingPage":"B11409"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003421"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003421"}],"createdAt":"2005-11-28","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004231546203136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coulomb Stress Evolution History as Implication on the Pattern of Strong Earthquakes along the Xianshuihe-Xiaojiang Fault System, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232306087296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Pleistocene-Holocene tectonic landforms developed along the strike-slip Xianshuihe Fault Zone, Tibetan Plateau, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285714961139328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Timing and Spouting Height of Sand Boils Caused by Liquefaction during the 2010 Mw 6.9 Yushu Earthquake, Tibetan Plateau, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165986259456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Systematic deflection and offset of the Yangtze River drainage system along the strike-slip Ganzi-Yushu-Xianshuihe Fault Zone, Tibetan Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755972352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic imaging of potential seismogenic asperities on the Xianshuihe‐Anninghe‐Zemuhe fault system, southwest China, with a new 3‐D viscoelastic interseismic coupling model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088871552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetism of Late Jurassic to Early Cretaceous red beds from the Cardamom Mountains, southwestern Cambodia: Tectonic deformation of the Indochina Peninsula"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185523059200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oroclinal origin of the Simao Arc in the Shan-Thai Block inferred from the Cretaceous palaeomagnetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118820316800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linking deeply-sourced volatile emissions to plateau growth dynamics in southeastern Tibetan Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705593961728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake Cycle Deformation Associated With the 2021 <i>M</i><sub><i>W</i></sub> 7.4 Maduo (Eastern Tibet) Earthquake: An Intrablock Rupture Event on a Slow‐Slipping Fault From Sentinel‐1 InSAR and Teleseismic Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513981312","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Present-day crustal motion in northeast China determined from GPS measurements"},{"@value":"Present-day crustal motion in northeast China determined from GPS measurement"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367115171968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contemporary horizontal crustal movement estimation for northwestern Vietnam inferred from repeated GPS measurements"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2004jb003421"},{"@type":"CROSSREF","@value":"10.1007/s12583-018-0840-2_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.5047/eps.2013.09.010_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.11.045_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.4236/ojer.2015.41002_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1186/bf03352642_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1002/2014jb011492_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2012.05467.x_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1038/s41467-021-24415-y_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1029/2022jb024268_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2015.03.002_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2018.05.005_references_DOI_YXAfN19bgtHExEl4iW9ybCORyW0"}]}