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<title lang=en>Transpressional tectonics and stream terraces of the Gobi-Altay, Mongolia</title>
<creator>Vassallo, R.</creator>
<creator>RITZ, Jean-francois</creator>
<creator>Braucher, Regis</creator>
<creator>Jolivet, Marc</creator>
<creator>Carretier, S.</creator>
<creator>Larroque, C.</creator>
<creator>CHAUVET, Alain</creator>
<creator>Sue, Christian</creator>
<creator>Todbileg, M.</creator>
<creator>Bourlès, D.</creator>
<creator>Arzhannikova, A.</creator>
<creator>Arzhannikov, S.</creator>
<contributor>Laboratoire Dynamique de la Lithosphère (LDL) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Institut national des sciences de l'Univers (INSU - CNRS) - 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>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire des Mécanismes et Transfert en Géologie (LMTG) ; Université Paul Sabatier - Toulouse 3 (UPS) - Observatoire Midi-Pyrénées (OMP) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géoazur (GEOAZUR) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Institut de Géologie et d'Hydrogéologie ; Université de Neuchâtel</contributor>
<contributor>Mongolian University of Science and Technology ; Mongolian University of Science and Technology</contributor>
<contributor>Institute of the Earth's Crust (IEC) ; Siberian Branch of the Russian Academy of Sciences (SB RAS)</contributor>
<description>International audience</description>
<source>ISSN: 0278-7407</source>
<source>Tectonics</source>
<publisher>American Geophysical Union (AGU)</publisher>
<identifier>hal-00323558</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00323558</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00323558v2/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00323558/file/Vassallo2007.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00323558</source>
<source>Tectonics, American Geophysical Union (AGU), 2007, 26 (5), pp.TC5013. 〈10.1029/2006TC002081〉</source>
<identifier>DOI : 10.1029/2006TC002081</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2006TC002081</relation>
<language>en</language>
<subject lang=en>Mongolia</subject>
<subject lang=en>Gobi-Altay</subject>
<subject lang=en>tectonic</subject>
<subject lang=en>landscape evolution</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 studied the patterns, rates and evolution of fluvial terraces and fault system during the building process of an intracontinental transpressional mountain in the Gobi-Altay (Mongolia). By analyzing incisions and offsets of fluvial terraces and alluvial fans, we show that the massif has grown by outward migration of thrust faults through time. On the northern flank, the present bounding thrust fault began its activity ~600 ka ago, while a more internal sub-parallel fault was still active until ~200-100 ka. Vertical offset of an alluvial fan abandoned ~100 ka ago allows an estimate of 0.1 mm/yr Upper Pleistocene - Holocene uplift rate. The morphology of the catchment-piedmont system strongly suggests a periodical formation of the alluvial surfaces, controlled by the climatic pulses, at the beginning of the wet interglacial periods. The abandonment of the alluvial terraces lags by several thousand years the abandonment of the alluvial fans, showing a diachronous incision propagating upstream. The incision rate deduced from the different elevations of straths exceeds of one order of magnitude the rock uplift rate. This excess is mostly due to ongoing drainage network growth at the core of the massif, and incision due to alluvial apron entrenchment near the outlet. This implies that fluvial response is mainly controlled by drainage growth, interaction with piedmont and cyclic climatic variations, rather than by rock uplift.</description>
<date>2007-10</date>
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