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<title lang=en>Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China</title>
<creator>Faure, Michel</creator>
<creator>Shu, Liangshu S.</creator>
<creator>Wang, Bo</creator>
<creator>Charvet, Jacques</creator>
<creator>Choulet, Flavien</creator>
<creator>Monié, Patrick</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>Department of Earth Sciences, Nanjing University ; Université du Québec</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>This research has been supported by National Natural Science Foundation of China (No. 40634022)</contributor>
<description>International audience</description>
<source>ISSN: 0954-4879</source>
<source>EISSN: 1365-3121</source>
<source>Terra Nova</source>
<publisher>Wiley-Blackwell</publisher>
<identifier>hal-00420901</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00420901</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00420901/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00420901/file/Faureetal-TerraNova-2009.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00420901</source>
<source>Terra Nova, Wiley-Blackwell, 2009, 21, pp.360-368. 〈10.1111/j.1365-3121.2009.00888.x〉</source>
<identifier>DOI : 10.1111/j.1365-3121.2009.00888.x</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3121.2009.00888.x</relation>
<language>en</language>
<subject lang=en>SOUTH CHINA</subject>
<subject lang=en>U-PB</subject>
<subject lang=en>SOUTHEASTERN CHINA</subject>
<subject lang=en>JIANGXI PROVINCE</subject>
<subject lang=en>CATHAYSIA BLOCK</subject>
<subject lang=en>TECTONIC EVOLUTION</subject>
<subject lang=en>TIEN-SHAN</subject>
<subject lang=en>SM-ND</subject>
<subject lang=en>AGE</subject>
<subject lang=en>COLLISION</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Early Palaeozoic Orogen of SE China consists of three litho-tectonic elements, from top to bottom: a sedimentary Upper Unit, a metamorphic Lower Unit and a gneissic basement. The boundaries between these units are flat lying, south directed, ductile decollements. The lower one is coeval with an amphibolite facies metamorphism (M1). The belt is reworked by migmatite-granite domes, high-temperature metamorphism (M2) and granitic plutons related to post-orogenic crustal melting. We date here the syn-M1 ductile shearing at 453 +/- 7 Ma by U-Th/Pb method on monazite. Previous ages and our new</description>
<date>2009</date>
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