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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:18:45Z</responseDate> <request identifier=oai:HAL:hal-01467822v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01467822v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Joint approach combining damage and paleoseismology observations constrains the 1714AD Bhutan earthquake at magnitude 8 +/- 0.5</title> <creator>Hetenyi, Gyorgy</creator> <creator>LE ROUX-MALLOUF, Romain</creator> <creator>Berthet, Theo</creator> <creator>CATTIN, Rodolphe</creator> <creator>Cauzzi, Carlo</creator> <creator>Phuntsho, Karma</creator> <creator>Grolimund, Remo</creator> <contributor>Université de Lausanne</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>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>Uppsala University</contributor> <contributor>ETH Zürich</contributor> <contributor>Shejun Agency for Bhutan's Cultural Documentation and Research, 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-01467822</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01467822</identifier> <source>https://hal.archives-ouvertes.fr/hal-01467822</source> <source>Geophysical Research Letters, American Geophysical Union, 2016, 43 (20), pp.10695-10702. 〈10.1002/2016GL071033〉</source> <identifier>DOI : 10.1002/2016GL071033</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1002/2016GL071033</relation> <language>en</language> <subject lang=en>Bhutan</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>The region of Bhutan is thought to be the only segment of the Himalayas not having experienced a major earthquake over the past half millennium. A proposed explanation for this apparent seismic gap is partial accommodation of the India-Asia convergence further south across the Shillong Plateau, yet the seismic behavior of the Himalayan megathrust in Bhutan is unknown. Here we present historical documents from the region reporting on an earthquake in 1714 A.D. and geological evidence of surface rupture to constrain the latest large event in this area. We compute various earthquake scenarios using empirical scaling relationships relating magnitude with intensity, source location and rupture geometry. Our results constrain the 1714 A.D. earthquake to have ruptured the megathrust in Bhutan, most likely during a M7.5–8.5 event. This finding reclassifies the apparent seismic gap to a former information gap and implies that the entire Himalayan arc has a high level of earthquake potential.</description> <date>2016-10-28</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>