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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Evidence for a wide and gently dipping Main Himalayan Thrust in western Bhutan</title>
<creator>LE ROUX-MALLOUF, Romain</creator>
<creator>Godard, Vincent</creator>
<creator>CATTIN, Rodolphe</creator>
<creator>FERRY, Matthieu</creator>
<creator>Gyeltshen, Jampel</creator>
<creator>RITZ, Jean-francois</creator>
<creator>Drupka, Dowchu</creator>
<creator>Guillou, Valery</creator>
<creator>Arnold, M.</creator>
<creator>Aumaitre, G.</creator>
<creator>Bourles, D. L.</creator>
<creator>Keddadouche, K.</creator>
<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>Risques ; 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) - 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>Department of Geology and Mines, Thimphu</contributor>
<description>International audience</description>
<source>ISSN: 0094-8276</source>
<source>EISSN: 1944-8007</source>
<source>Geophysical Research Letters</source>
<publisher>American Geophysical Union</publisher>
<identifier>hal-01174088</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01174088</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01174088v2/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01174088/file/lerouxmalloufGRL2015.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01174088</source>
<source>Geophysical Research Letters, American Geophysical Union, 2015, 42 (9), pp.3257-3265. 〈10.1002/2015GL063767〉</source>
<identifier>DOI : 10.1002/2015GL063767</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1002/2015GL063767</relation>
<language>en</language>
<subject lang=en>lateral variation</subject>
<subject lang=en>Main Himalayan Thrust</subject>
<subject lang=en>Himalaya</subject>
<subject lang=en>denudation</subject>
<subject lang=en>cosmonuclide</subject>
<subject lang=en>Bhutan</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>The Main Himalayan Thrust (MHT) is the source of great earthquakes that have been documented along the range. Its geometry is a key parameter that influences accommodation of tectonic loading and earthquake magnitudes along the Himalayan Arc. Although seismic images are available for both the western and the central part of the range, this geometry remains poorly constrained for the Bhutanese Himalayas. Here we address this issue using a 10Be cosmogenic nuclides denudation transect across western Bhutan. We observe a wide low denudation rate domain between 50 km and 110 km from the front followed by a strong northward increase. Using a joint inversion of denudation rates, GPS data, and Holocene uplift rates, we interpret this pattern as a consequence of a flat-ramp transition along the MHT. Compared to central Nepal and Sikkim, this location of the ramp suggests a wider décollement, with implications for greater seismogenic potential of the MHT in western Bhutan.</description>
<date>2015-05-16</date>
<rights>info:eu-repo/semantics/OpenAccess</rights>
</dc>
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