{"@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/1361137045857455360.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2002jb002373"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2002JB002373"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2002JB002373"}}],"dc:title":[{"@value":"GPS measurements of crustal deformation in the Baikal‐Mongolia area (1994–2002): Implications for current kinematics of Asia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We present new geodetic results of crustal velocities over a large part of northern Asia based on GPS measurements in the Baikal rift zone and Mongolia spanning the 1994–2002 period. We combine our results with the GPS velocity field for China of <jats:ext-link xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"#jgrb13739-bib-0066\"><jats:italic>Wang et al.</jats:italic> [2001]</jats:ext-link> and derive a consistent velocity field for most of Asia. We find contrasted kinematic and strain regimes in Mongolia, with northward velocities and N‐S shortening in westernmost Mongolia but eastward to southeastward motion and left‐lateral shear for central and eastern Mongolia. This eastward to southeastward motion of central and eastern Mongolia is accommodated by left‐lateral slip on the E‐W trending Tunka, Bolnay, and Gobi Altay faults (2 ± 1.2 mm yr<jats:sup>−1</jats:sup>, 2.6 ± 1.0 mm yr<jats:sup>−1</jats:sup>, and 1.2 mm yr<jats:sup>−1</jats:sup>, respectively) and by about 4 mm yr<jats:sup>−1</jats:sup> of extension across the Baikal rift zone. Consequently, ∼15% of the India‐Eurasia convergence is accommodated north of the Tien Shan, by N‐S shortening combined with dextral shear in the Mongolian Altay and by eastward displacements along major left‐lateral strike‐slip faults in central and eastern Mongolia. We find a counterclockwise rotation of north and south China as a quasi‐rigid block around a pole north of the Stanovoy belt, which rules out the existence of an Amurian plate as previously defined and implies <2 mm yr<jats:sup>−1</jats:sup> of left‐lateral slip on the Qinling Shan fault zone.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045857455490","@type":"Researcher","foaf:name":[{"@value":"Eric Calais"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Atmospheric Sciences Purdue University  West Lafayette Indiana USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455488","@type":"Researcher","foaf:name":[{"@value":"Mathilde Vergnolle"}],"jpcoar:affiliationName":[{"@value":"UMR CNRS 6526 University of Nice  Valbonne France"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455363","@type":"Researcher","foaf:name":[{"@value":"Vladimir San'kov"}],"jpcoar:affiliationName":[{"@value":"Institute of the Earth's Crust Siberian Branch of the Russian Academy of Sciences  Irkutsk Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455361","@type":"Researcher","foaf:name":[{"@value":"Andrei Lukhnev"}],"jpcoar:affiliationName":[{"@value":"Institute of the Earth's Crust Siberian Branch of the Russian Academy of Sciences  Irkutsk Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455489","@type":"Researcher","foaf:name":[{"@value":"Andrei Miroshnitchenko"}],"jpcoar:affiliationName":[{"@value":"Institute of the Earth's Crust Siberian Branch of the Russian Academy of Sciences  Irkutsk Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455362","@type":"Researcher","foaf:name":[{"@value":"Sharavyn Amarjargal"}],"jpcoar:affiliationName":[{"@value":"Research Center for Astronomy and Geophysics  Ulan Baatar Mongolia"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045857455360","@type":"Researcher","foaf:name":[{"@value":"Jacques Déverchère"}],"jpcoar:affiliationName":[{"@value":"UMR CNRS 6538 University Bretagne Occidentale  Plouzané France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2003-10","prism:volume":"108","prism:number":"B10","prism:startingPage":"2501"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2002JB002373"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2002JB002373"}],"createdAt":"2003-10-25","modifiedAt":"2023-10-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017287039993088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Determining In-Situ Stress State by Anelastic Strain Recovery Method Beneath Xiamen: Implications for the Coastal Region of Southeastern China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185522934528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Present tectonics of the southeast of Russia as seen from GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855574156800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper mantle structure beneath the Mongolian region from multimode surface waves: Implications for the western margin of Amurian plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205510603136","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Influences of Long-Term Tectonic and Geo-Climatic Effects on Geotechnical Problems of Soft Ground - Ulaanbaatar, Mongolia"},{"@language":"en","@value":"Influences of Long-Term Tectonic and Geo-Climatic Effects on Geotechnical Problems of Soft Ground - Ulaanbaatar, Mongolia"}]},{"@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":"10.1029/2002jb002373"},{"@type":"CROSSREF","@value":"10.5047/eps.2013.09.010_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"},{"@type":"CROSSREF","@value":"10.1186/bf03352642_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2010.04871.x_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"},{"@type":"CROSSREF","@value":"10.1007/s00603-022-02915-7_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230506_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"},{"@type":"CROSSREF","@value":"10.14247/lti.18.1_51_references_DOI_XG4zVBUL1Z3ELDHUHqnk2NNTLy7"}]}