{"@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/1363670318911676544.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/96jb03831"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03831"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03831"}}],"dc:title":[{"@value":"Tertiary diachronic extrusion and deformation of western Indochina: Structural and <sup>40</sup>Ar/<sup>39</sup>Ar evidence from NW Thailand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Wang Chao and Three Pagodas fault zones cut the western part of the Indochina block and run parallel to the Red River Fault. Evidence of intense ductile left‐lateral shear is found in the Lansang gneisses, which form a 5 km wide elongated core along the Wang Chao fault zone. Dating by <jats:sup>40</jats:sup>Ar/<jats:sup>39</jats:sup>Ar shows that such deformation probably terminated around 30.5 Ma. The Wang Chao and Three Pagodas faults offset the north striking lower Mesozoic metamorphic and magmatic belt of northern Thailand. <jats:sup>40</jats:sup>Ar/<jats:sup>39</jats:sup>Ar results suggest that this belt suffered rapid cooling in the Tertiary, probably around 23 Ma. These results imply that the extrusion of the southwestern part of Indochina occurred in the upper Eocene‐lower Oligocene. It probably induced rifting in some basins of the Gulf of Thailand and in the Malay and Mekong basins. In the Oligo‐Miocene, the continuing penetration of India into Asia culminated with the extrusion of all of Indochina along the Ailao Shan‐Red River fault. This occurred concurrently with the onset of E‐W extension more to the south. Plotting in a geographical reference frame the diachronic time spans of movement on left‐lateral faults east and southeast of Tibet implies that the northward movement of the Indian indenter successively initiated new strike‐slip faults located farther and farther north along its path.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318911676674","@type":"Researcher","foaf:name":[{"@value":"Robin Lacassin"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676545","@type":"Researcher","foaf:name":[{"@value":"Henri Maluski"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676673","@type":"Researcher","foaf:name":[{"@value":"P. Hervé Leloup"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676544","@type":"Researcher","foaf:name":[{"@value":"Paul Tapponnier"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676547","@type":"Researcher","foaf:name":[{"@value":"Chaiyan Hinthong"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676672","@type":"Researcher","foaf:name":[{"@value":"Kanchit Siribhakdi"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676548","@type":"Researcher","foaf:name":[{"@value":"Saengathit Chuaviroj"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318911676546","@type":"Researcher","foaf:name":[{"@value":"Adul Charoenravat"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1997-05-10","prism:volume":"102","prism:number":"B5","prism:startingPage":"10013","prism:endingPage":"10037"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03831"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03831"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285711150862976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoearthquake Investigations of the Mae Hong Son Fault, Mae Hong Son Region, Northern Thailand"}]},{"@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/1390282680170959744","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleaogeography and Climatic Change recorded on Viviparidae Carbon and Oxygen Isotope in Mae Moh Coal Mine, Northern Thailand"},{"@language":"ja","@value":"タイ北部マエモー炭鉱産タニシ類化石の炭素・酸素同位体に記録された古生物地理と古気候の変化"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489365760","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"GPS measurements of horizontal deformation across the Lai Chau-Dien Bien (Dien Bien Phu) fault, in Northwest of Vietnam, 2002-2004"},{"@value":"GPS measurements of horizontal deformation across the Lai Chau—Dien Bien (Dien Bien Phu) fault, in Northwest of Vietnam, 2002-2004"}]},{"@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":"10.1029/96jb03831"},{"@type":"CROSSREF","@value":"10.1142/s1793431114500079_references_DOI_SjYVYffUfdvoSyLvhCwiy1pCVft"},{"@type":"CROSSREF","@value":"10.5047/eps.2013.09.010_references_DOI_SjYVYffUfdvoSyLvhCwiy1pCVft"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.11.045_references_DOI_SjYVYffUfdvoSyLvhCwiy1pCVft"},{"@type":"CROSSREF","@value":"10.1186/bf03351949_references_DOI_SjYVYffUfdvoSyLvhCwiy1pCVft"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.59.327_references_DOI_SjYVYffUfdvoSyLvhCwiy1pCVft"}]}