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<title lang=en>Palaeozoic collision between the North and South China Blocks, Triassic intracontinental tectonics, and the problem of the ultrahigh-pressure metamorphism</title>
<creator>Faure, Michel</creator>
<creator>Lin, Wei</creator>
<creator>Monié, Patrick</creator>
<creator>Meffre, Sébastien</creator>
<contributor>Institut des Sciences de la Terre d'Orléans (ISTO) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Institute of Geology and Geophysics, LTE (LTE) ; Institute of Geology and Geophysics</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>
<contributor>School of Earth Sciences [Hobart] ; University of Tasmania </contributor>
<contributor>This work has been funded by the national key basis Research program of China (Grant no. 2005CB422101).</contributor>
<description>International audience</description>
<source>ISSN: 1631-0713</source>
<source>Comptes Rendus Géoscience</source>
<publisher>Elsevier Masson</publisher>
<identifier>insu-00191534</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00191534</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00191534/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00191534/file/Faure-ComptesRendusGeoscience.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00191534</source>
<source>Comptes Rendus Géoscience, Elsevier Masson, 2008, 340, pp.139-150. 〈10.1016/j.crte.2007.10.007〉</source>
<identifier>DOI : 10.1016/j.crte.2007.10.007</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2007.10.007</relation>
<language>en</language>
<subject lang=en>Qinling–Dabie Belt</subject>
<subject lang=en>Palaeozoic collision</subject>
<subject lang=en>Triassic tectonics</subject>
<subject lang=en>Continental subduction</subject>
<subject lang=en>Ultrahigh-pressure metamorphism</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<subject>[SDE.MCG.CG] Environmental Sciences/Global Changes/domain_sde.mcg.cg</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Qinling–Dabie Belt represents the boundary between the North and South China Blocks (NCB, SCB, respectively), where ultrahigh-pressure (UHP) rocks are widespread. A structural study in eastern Qinling and zircon LA ICPMS dating of the migmatite that form the core of the Central Qinling Unit allows us to argue that continental collision occurred in Silurian, before 400 Ma. In the Late Palaeozoic, from Devonian to Permian, the northern margin of SCB experienced a continental rifting. From Late Permian to Middle Triassic, northward continental subduction of SCB is responsible for the development of a high-pressure metamorphism. The age of the UHP metamorphism remains unsettled yet. A two-time genesis, Early Palaeozoic and Early Triassic, is often preferred, but a single Palaeozoic age followed by a Triassic resetting cannot be ruled out.</description>
<date>2008</date>
<rights>info:eu-repo/semantics/OpenAccess</rights>
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