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<title lang=en>Cooling paths during the Mesozoic Extensional Tectonics of NE China: example from the South Liaodong Peninsula Metamorphic Core Complex</title>
<creator>Lin, Wei</creator>
<creator>Monié, Patrick</creator>
<creator>Faure, Michel</creator>
<creator>Schärer, Urs</creator>
<creator>Shi, Yonghong</creator>
<creator>Le Breton, Nicole</creator>
<creator>Wang, Qingchen</creator>
<contributor>State Key Laboratory of Lithospheric Evolution ; Institute of Geology and Geophysics, Chinese Academy of Sciences</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>Institut des Sciences de la Terre d'Orléans (ISTO) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Université François Rabelais - Tours - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géoazur (GEOAZUR) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Department of Geology ; University of Technology</contributor>
<description>International audience</description>
<source>ISSN: 1367-9120</source>
<source>Journal of Asian Earth Sciences</source>
<publisher>Elsevier</publisher>
<identifier>insu-00528171</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00528171</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00528171/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00528171/file/Lin-JAsianEarthSciences-2010.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00528171</source>
<source>Journal of Asian Earth Sciences, Elsevier, 2011, 42 (5), pp.1048-1065. 〈10.1016/j.jseaes.2010.09.007〉</source>
<identifier>DOI : 10.1016/j.jseaes.2010.09.007</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jseaes.2010.09.007</relation>
<language>en</language>
<subject lang=en>Lithospheric removal</subject>
<subject lang=en>Crustal extension</subject>
<subject lang=en>Metamorphic Core Complex</subject>
<subject lang=en>Cooling paths</subject>
<subject lang=en>Radiometric ages</subject>
<subject lang=en>North China Craton</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 South Liaodong Peninsula massif is the easternmost Mesozoic Metamorphic Core Complex, recognized in Eastern China. It provides a good example of the combination of ductile shearing, synkinematic plutonism and polyphase exhumation. The Jurassic granodioritic plutons, located at the footwall of the detachment normal fault, and dated here at ca 160 Ma, recorded two different phases of cooling. A slow cooling regime of about 3-10°C/my prevailing before 122 Ma, was followed by a significant increase in cooling rate of about 40-55°C/my after that time. By contrast, a single fast cooling path was recorded by the Cretaceous monzogranite situated in the footwall of the detachment normal fault. This result indicates that the Jurassic and Cretaceous plutons recorded different exhumation processes: a Jurassic slow or negligible exhumation and a Cretaceous fast one assisted by normal faulting. These two cooling stages correspond to distinct geodynamic processes during the Jurassic and Cretaceous. Extensional tectonics seems not significant before Early Cretaceous. The second stage, dominated by an extensional regime which develops after ca 120 Ma, is tentatively correlated to the lithosphere removal of the North China Craton.</description>
<rights>http://creativecommons.org/licenses/by-nc-nd/</rights>
<date>2011</date>
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