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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Survival of eclogite xenolith in a Cretaceous granite intruding the Central Dabieshan migmatite gneiss dome (Eastern China) and its tectonic implications.</title>
<creator>Lin, Wei</creator>
<creator>Enami, M.</creator>
<creator>Faure, Michel</creator>
<creator>Schärer, Urs</creator>
<creator>Arnaud, Nicolas</creator>
<contributor>Department of Earth and Planetary Sciences [Kobe] ; Kobe University</contributor>
<contributor>Institute of Geology and Geophysics, LTE (LTE) ; Institute of Geology and Geophysics</contributor>
<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>Laboratoire de tectonique, mécanique de la lithosphère (LTML) ; IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - 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>
<contributor>National Key Basic Research Program (Grant No. 2005CB422101) and NSFC (40202021, 40472116). JSPS is acknowledged for providing a Grant of Postdoctoral Fellowship for Foreign Researchers (14–02060 to W.L.) and Grant-in-Aid for Scientific Research (14540448 and 18340172 to M.E.)</contributor>
<description>International audience</description>
<source>ISSN: 1437-3254</source>
<source>EISSN: 1437-3262</source>
<source>International Journal of Earth Sciences</source>
<publisher>Springer Verlag</publisher>
<identifier>hal-00104224</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/hal-00104224</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/hal-00104224/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/hal-00104224/file/Lin-IntJEarthSciences-2007.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/hal-00104224</source>
<source>International Journal of Earth Sciences, Springer Verlag, 2007, 96, pp.707-724. 〈10.1007/s00531-006-0129-z〉</source>
<identifier>DOI : 10.1007/s00531-006-0129-z</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-006-0129-z</relation>
<language>en</language>
<subject lang=en>Eclogite xenolith</subject>
<subject lang=en>Mesozoic granite</subject>
<subject lang=en>Radiometric ages</subject>
<subject lang=en>Exhumation model</subject>
<subject lang=en>Dabieshan</subject>
<subject lang=en>China</subject>
<subject>[SDE.MCG.CG] Environmental Sciences/Global Changes/domain_sde.mcg.cg</subject>
<subject>[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology</subject>
<subject>[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanology</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>Investigation of an eclogite xenolith, discovered in a Cretaceous granite from the Central Domain of the Dabieshan massif in eastern China, yields new petrological insights into the high to ultrahigh-pressure metamorphism, experienced by the Qinling-Dabie orogen. Prior to inclusion as a xenolith in the granite during the Early Cretaceous, this eclogite xenolith had recorded a complex metamorphic evolution that complies with subduction and exhumation processes experienced by the continental crust of the South China Block. Well-preserved mineral parageneses substantiate the prograde and retrograde stages revealed by inclusions in porphyroblastic garnet and zoned minerals such as garnet, comphacite and amphibole in the matrix. The relatively low P/T re-equilibration during a latemetamorphic stage was textually inferred by the presence of aluminous and calcic-subcalcic amphiboles such as katophorite, edenite, taramite and pargasite as main matrix phases. According to our U/Pb, Rb/Sr and new 40Ar/39Ar geochronological results, namely 109 ± 1 and 112 ± 2 Ma plateau ages for muscovite and amphiboles, respectively, two successive but distinct cooling stages account for the thermal history of the granite–migmatite gneiss dome that forms the Central Dabieshan Domain. We argue that prior to the Cretaceous doming, the Central Dabieshan Domain experienced a tectono-metamorphic evolution similar to that observed in the high-pressure to ultra high-pressure units developed in the Southern Dabieshan Domain and Hong'an massif.</description>
<date>2007</date>
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