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<identifier>oai:HAL:hal-01397683v1</identifier>
<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Origin and time evolution of subduction polarity reversal from plate kinematics of Southeast Asia</title>
<creator>Von hagke, Christoph</creator>
<creator>PHILIPPON, Melody</creator>
<creator>Avouac, Jean-Philippe</creator>
<creator>Gurnis, M.</creator>
<contributor>Institute of Structural Geology, Tectonics, and Geomechanics, RWTH Aachen,</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>Division of Geological and Planetary Sciences [Pasadena] ; California Institute of Technology (CALTECH)</contributor>
<contributor>Seismological Laboratory, California Institute of Technology,</contributor>
<description>International audience</description>
<source>ISSN: 0091-7613</source>
<source>EISSN: 0091-7613</source>
<source>Geology</source>
<publisher>Geological Society of America</publisher>
<identifier>hal-01397683</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01397683</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01397683</source>
<source>Geology, Geological Society of America, 2016, 44 (8), pp.659-662. 〈10.1130/G37821.1〉</source>
<identifier>DOI : 10.1130/G37821.1</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1130/G37821.1</relation>
<language>en</language>
<subject lang=en>Southeast Asia</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>We present a regional model of plate geometry and kinematics of Southeast Asia since the Late Cretaceous, embedded in a global plate model. The model involves subduction polarity reversals and sheds new light on the origin of the subduction polarity reversal currently observed in Taiwan. We show that this subduction zone reversal is inherited from subduction of the proto–South China Sea plate and owes its current location to triple junction migration and slab rollback. This analysis sheds new light on the plate tectonic context of the Taiwan orogeny and questions the hypothesis that northern Taiwan can be considered an older, more mature equivalent of southern Taiwan.</description>
<date>2016-08</date>
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