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<title lang=en>Paleo-Tethyan Evolution of Tibet as Recorded in the East Cimmerides and West Cathaysides</title>
<creator>Xu, Zhiqin</creator>
<creator>Dilek, Yildirim</creator>
<creator>Cao, Hui</creator>
<creator>Yang, Jingsui</creator>
<creator>Robinson, Paul</creator>
<creator>Ma, Changqian</creator>
<creator>Li, Huaqi</creator>
<creator>Jolivet, Marc</creator>
<creator>Roger, Françoise</creator>
<creator>Chen, Xijie</creator>
<contributor>state key laboratory of continental tectonics and dynamics ; Institute of Geology, Chinese Academy of Geological Sciences, Beijing ; Université du Québec - Université du Québec</contributor>
<contributor>Beijing Institute of Technology (BIT)</contributor>
<contributor>Department of Earth Sciences and Environmental Science, Dalhousie University, Halifax, B3H 4R2, Canada</contributor>
<contributor>Géosciences Rennes (GR) ; Université de Rennes 1 (UR1) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire des Sciences de l'Univers de Rennes (OSUR) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0743-9547</source>
<source>Journal of Southeast Asian earth sciences</source>
<publisher>Elsevier</publisher>
<identifier>insu-01119604</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01119604</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01119604/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01119604/file/Xu-JAES-2015.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01119604</source>
<source>Journal of Southeast Asian earth sciences, Elsevier, 2015, 105, pp.320-337. 〈10.1016/j.jseaes.2015.01.021〉</source>
<identifier>DOI : 10.1016/j.jseaes.2015.01.021</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jseaes.2015.01.021</relation>
<language>en</language>
<subject lang=en>Orogenic collage</subject>
<subject lang=en>Paleo-Tethyan Tibet</subject>
<subject lang=en>Cathaysides</subject>
<subject lang=en>Cimmerides</subject>
<subject lang=en>Décollement-type orogen</subject>
<subject lang=en>Ophiolites and suture zones</subject>
<subject lang=en>Paleo-Tethys</subject>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Paleozoic-early Mesozoic geology of Tibet was controlled by the rift-drift, seafloor spreading and subduction zone tectonics of a Paleo-Tethyan realm, which evolved between the West Cathaysides (WC) and the East Cimmerides (EC). Different suture zones with ophiolites and ophiolitic mélanges, high-pressure metamorphic belts, magmatic arcs and accretionary prism complexes separating different terranes mark multiple subduction-accretion systems within this Paleo-Tethyan domain, reminiscent of the modern Western Pacific Ocean. Discrete basins separated by different continental blocks and magmatic arcs constituted a complex paleogeography of Paleo-Tethys, and these oceanic strands were closed as a result of subduction with different polarities during the late Paleozoic-Triassic. The Longmu Tso Shuanghu-Changning Menglian Suture zone (LS-CMS) in Tibet represents the main tectonic boundary between the WC and EC that developed in the Devonian. The East Kunlun-A’nyemaqen oceanic slab was subducted northward beneath the East Kunlun terrane in northern Tibet, whereas the Sumdo oceanic slab was subducted northward beneath the South Qiangtang-North Lhasa terrane in southern Tibet. The Longmu Tso Shuanghu-Changning Menglian and Jinshajiang-Ailaoshan-Song Ma ophiolites were developed and emplaced in subduction-accretion systems with opposite polarities (westward and eastward) beneath the North Qiangtang-Qamdo-Simao-Indochina terrane in central Tibet. The Jinshajiang-Ailaoshan-Song Ma oceanic slab was subducted westward beneath the North Qiangtang-Simao-Indochina terrane along the Jinshajiang and Ailaoshan-Song Ma trenches in a trench-ridge-trench triple junction plate configuration. The Emeishan mantle plume produced a large Permian basaltic terrane, developed on the western passive margin of the South China block. The final closure of the Paleo-Tethyan oceanic branches resulted in continental collisions and development of a vast Indosinian orogenic collage in the latest Triassic-Jurassic.</description>
<date>2015</date>
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