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<title lang=en>Initial movement of the Karakorum Fault in western Tibet: constraints from SHRIMP U-Pb dating of zircons</title>
<creator>Li, H. B.</creator>
<creator>Valli, F.</creator>
<creator>Liu, D. Y.</creator>
<creator>Xu, Z. Q.</creator>
<creator>Yang, J. S.</creator>
<creator>Arnaud, Nicolas</creator>
<creator>Tapponnier, P.</creator>
<creator>Lacassin, R.</creator>
<creator>Chen, S. Y.</creator>
<creator>Qi, X. X.</creator>
<contributor>Institute of Geology, Chinese Academy of Geological Sciences, Beijing ; Université du Québec</contributor>
<contributor>Department of Earth Sciences [Hong kong] ; The University of Hong Kong (HKU)</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 de Physique du Globe de Paris (IPGP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<source>ISSN: 1001-6538</source>
<source>EISSN: 1861-9541</source>
<source>Chinese Science Bulletin</source>
<publisher>SpringerOpen</publisher>
<identifier>hal-00406402</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00406402</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00406402</source>
<source>Chinese Science Bulletin, SpringerOpen, 2007, 52 (8), pp.1089-1100. 〈10.1007/s11434-007-0164-6〉</source>
<identifier>DOI : 10.1007/s11434-007-0164-6</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s11434-007-0164-6</relation>
<language>en</language>
<subject lang=en>ductile shear zone</subject>
<subject lang=en>zircon SHRIMP U-Pb dating</subject>
<subject lang=en>Karakorum Fault</subject>
<subject lang=en>Tibetan Plateau</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Karakorum Fault zone (KFZ) plays an important role in understanding the formation, evolvement and deformation of the Tibetan Plateau. The high-T dextral shearing metamorphic rocks, e.g., mylonites or mylonitized gneisses-granites, locally crop out along the southeastern part of the KFZ in the Ayila Ri'gyü Range area. The SHRIMP U-Pb dating of the syn-kinematic crystallized zircons indicates that the initial age of the KFZ is ∼27 Ma, ∼10 Ma older than previous results. The extensive high-T dextral shearing along the KFZ started at least at 27–20 Ma, accompanied by the syn-kinematic emplacement of leuco-granites. Deformation and concomitant fluid circulation during shearing most likely occurred as early as at 25–13 Ma. The KFZ probably grew from southeast to northwest along the fault as a result of continuous convergence between the India plate and Eurasia plate.</description>
<date>2007</date>
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