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<title lang=en>Comment on "Displacement along the Karakoram fault, NW Himalaya, estimated from LA-ICP-MS U Pb dating of offset geologic markers" published by Shifeng Wang et al. in EPSL, 2012</title>
<creator>Leloup, P.H.</creator>
<creator>Boutonnet, E.</creator>
<creator>Weinberg, R.</creator>
<creator>Mukherjee, B., </creator>
<creator>Tapponnier, P.</creator>
<creator>Lacassin, R.</creator>
<creator>Chevalier, M.L.</creator>
<creator>Li, Hongbo</creator>
<creator>Valli, F.</creator>
<creator>Arnaud, Nicolas</creator>
<creator>Paquette, Jean-Louis</creator>
<contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Claude Bernard Lyon 1 (UCBL) - École normale supérieure - Lyon (ENS Lyon)</contributor>
<contributor>Institute of Geosciences ; Johannes Gutenberg Univ Mainz</contributor>
<contributor>Australian Crustal Research Centre, School of Geosciences, Monash University ; Monash University [Clayton]</contributor>
<contributor>Wadia Institute Himalayan Geol. ; Wadia Inst Himalayan Geol</contributor>
<contributor>Earth Observ Singapore, Tecton Grp ; Nanyang Technological University [Singapour]</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>
<contributor>Inst Geol ; Chinese Academy of Sciences [Changchun Branch] (CAS)</contributor>
<contributor>Institute of Applied Mathematics ; Academia Sinica</contributor>
<contributor>Newmont Min Corp ; Australian National University (ANU)</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>Laboratoire Magmas et Volcans (LMV) ; Université Blaise Pascal - Clermont-Ferrand 2 (UBP) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Jean Monnet [Saint-Étienne] (UJM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0012-821X</source>
<source>Earth and Planetary Science Letters</source>
<publisher>Elsevier</publisher>
<identifier>hal-00829469</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00829469</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00829469</source>
<source>Earth and Planetary Science Letters, Elsevier, 2013, 363, pp.242-245. 〈10.1016/j.epsl.2012.12.012〉</source>
<identifier>DOI : 10.1016/j.epsl.2012.12.012</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2012.12.012</relation>
<language>en</language>
<subject lang=da>Karakorum strike-slip fault</subject>
<subject lang=da>offset</subject>
<subject lang=da>dating deformation</subject>
<subject lang=da>rate</subject>
<subject lang=da>synkinematic melting</subject>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Field evidence for syn-deformation migmatization and crystallization along the Karakorum fault contradicts the study of Wang et al. (2012). The ages of such magmatic rocks provide minimum ages for the onset of deformation at similar to 23 Ma in North Ayilari and similar to 19 Ma in Tangtse. The onset of deformation at 12 Ma in the Ayilari range inferred by Wang et al. (2012) from a muscovite Ar/Ar age is a cooling age, thus only a minimum age. The similar to 60 Ma granodiorite bodies, the ophiolitic rocks and the south Kailash thrust that are correlated across the fault to provide a 52 +/- 2 km finite offset do not define reliable piercing points. Such observations as well as our previous work concur to show that the Karakorum fault initiated in the Oligo-Miocene, and has a long-term dextral slip-rate between 7.5 and 13 mm/yr, approximately twice that proposed by Wang et al. (2012).</description>
<date>2013-02-01</date>
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