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<title lang=en>Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a ~2.1 Ga thermal and tectonic event in the Fuping Massif</title>
<creator>Trap, Pierre</creator>
<creator>Faure, Michel</creator>
<creator>Lin, Wei</creator>
<creator>Bruguier, Olivier</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>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>The field work for this research was financially supported by a National Science Foundation of China grant no. 40472116</contributor>
<description>International audience</description>
<source>ISSN: 0191-8141</source>
<source>Journal of Structural Geology</source>
<publisher>Elsevier</publisher>
<identifier>insu-00309553</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00309553</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00309553/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00309553/file/Trap-JStructuralGeology-2008.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00309553</source>
<source>Journal of Structural Geology, Elsevier, 2008, 30 (9), pp.1109-1125. 〈10.1016/j.jsg.2008.05.001〉</source>
<identifier>DOI : 10.1016/j.jsg.2008.05.001</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsg.2008.05.001</relation>
<language>en</language>
<subject lang=en>Trans-North China Belt</subject>
<subject lang=en>Paleoproterozoic geodynamics</subject>
<subject lang=en>Dome-and-basin structure</subject>
<subject lang=en>Ductile shearing</subject>
<subject lang=en>Syntectonic plutonism</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>Structural analysis along with 40Ar–39Ar and U–Pb datings in the Fuping massif provide new insight into the evolution of the eastern part of the Trans-North China Belt (North China Craton), from 2.7 Ga to 1.8 Ga. D1 is responsible for the development of a dome-and-basin structure coeval with crustal melting giving rise to migmatite and Nanying gneissic granites at 2.1 Ga. This dome-and-basin architecture resulted from the interference between a N–S compression of a weak ductile crust and gravity-driven vertical flow, in a high thermal regime. The next events involved flat lying ductile thrusting (D2) and normal faulting (D3) dated at around 1880 Ma and 1830 Ma, respectively. The D2 and D3 events belong to the Trans-North China Orogeny that results in the final amalgamation of the North China Craton. The D1 deformation is considered as evidence for an earlier orogen developed around 2.1 Ga prior to the Trans-North China Orogeny. The change in the deformation style between the 2.1 Ga and 1.8 Ga could be viewed as a consequence of the cooling of the continental crust in the North China Craton.</description>
<date>2008</date>
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