{"@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/1361699995673397888.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018tc005036"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018TC005036"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005036"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018TC005036"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005036"}}],"dc:title":[{"@value":"Mantle Flow and Deforming Continents: From India‐Asia Convergence to Pacific Subduction"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The formation of mountain belts or rift zones is commonly attributed to interactions between plates along their boundaries, but the widely distributed deformation of Asia from Himalaya to the Japan Sea and other back‐arc basins is difficult to reconcile with this notion. Through comparison of the tectonic and kinematic records of the last 50 Ma with seismic tomography and anisotropy models, we show that the closure of the former Tethys Ocean and the extensional deformation of East Asia can be best explained if the asthenospheric mantle transporting India northward, forming the Himalaya and the Tibetan Plateau, reaches East Asia where it overrides the westward flowing Pacific mantle and contributes to subduction dynamics, distributing extensional deformation over a 3,000‐km wide region. This deep asthenospheric flow partly controls the compressional stresses transmitted through the continent‐continent collision, driving crustal thickening below the Himalayas and Tibet and the propagation of strike‐slip faults across Asian lithosphere further north and east, as well as with the lithospheric and crustal flow powered by slab retreat east of the collision zone below East and SE Asia. The main shortening direction in the deforming continent between the collision zone and the Pacific subduction zones may in this case be a proxy for the direction of flow in the asthenosphere underneath, which may become a useful tool for studying mantle flow in the distant past. Our model of the India‐Asia collision emphasizes the role of asthenospheric flow underneath continents and may offer alternative ways of understanding tectonic processes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848661784429058","@type":"Researcher","foaf:name":[{"@value":"Laurent Jolivet"}],"jpcoar:affiliationName":[{"@value":"Sorbonne Université, CNRS‐INSU, Institut des Sciences de la Terre Paris, ISTeP UMR 7193  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995673397891","@type":"Researcher","foaf:name":[{"@value":"Claudio Faccenna"}],"jpcoar:affiliationName":[{"@value":"Dipartimento Scienze Università Roma Tre  Rome Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995673397888","@type":"Researcher","foaf:name":[{"@value":"Thorsten Becker"}],"jpcoar:affiliationName":[{"@value":"UTIG University of Texas at Austin  Austin TX USA"},{"@value":"DGS University of Texas at Austin  Austin TX USA"},{"@value":"JSG University of Texas at Austin  Austin TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995673397892","@type":"Researcher","foaf:name":[{"@value":"Magdala Tesauro"}],"jpcoar:affiliationName":[{"@value":"Dipartimento di Matematica e Geoscienze Universita degli studi di Trieste  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995673397890","@type":"Researcher","foaf:name":[{"@value":"Pietro Sternai"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Geneva  Geneva Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995673397889","@type":"Researcher","foaf:name":[{"@value":"Pierre Bouilhol"}],"jpcoar:affiliationName":[{"@value":"C.R.P.G. Université de Lorraine  Vandoeuvre‐les‐Nancy France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02787407"},{"@type":"EISSN","@value":"19449194"}],"prism:publicationName":[{"@value":"Tectonics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-09","prism:volume":"37","prism:number":"9","prism:startingPage":"2887","prism:endingPage":"2914"},"reviewed":"false","dc:rights":["http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018TC005036"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005036"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018TC005036"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005036"}],"createdAt":"2018-08-07","modifiedAt":"2023-09-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360286995504269312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of the early Cenozoic belt boundary thrust and Izanagi–Pacific ridge subduction in the western Pacific margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757167535232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Whole‐Mantle Tomography of Southeast Asia: New Insight Into Plumes and Slabs"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942140842496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of relocated hypocenters of the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three-dimensional seismic velocity structure"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266972609792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2018tc005036"},{"@type":"CROSSREF","@value":"10.1111/iar.12320_references_DOI_TwDAa45EqeZhUComOZNgwDl1mYH"},{"@type":"CROSSREF","@value":"10.1029/2022jb024298_references_DOI_TwDAa45EqeZhUComOZNgwDl1mYH"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0234-1_references_DOI_TwDAa45EqeZhUComOZNgwDl1mYH"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1100-0_references_DOI_TwDAa45EqeZhUComOZNgwDl1mYH"}]}