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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Active faulting induced by slip partitioning in Montserrat and link with volcanic activity: New insights from the 2009 GWADASEIS marine cruise data</title>
<creator>Feuillet, Nathalie</creator>
<creator>Leclerc, Frédérique</creator>
<creator>Tapponnier, Paul</creator>
<creator>Beauducel, François</creator>
<creator>Boudon, Georges</creator>
<creator>Le Friant, Anne</creator>
<creator>Deplus, Christine</creator>
<creator>Lebrun, Jean-Frédéric</creator>
<creator>Nercessian, Alexandre</creator>
<creator>Saurel, Jean-Marie</creator>
<creator>Clément, Valentin</creator>
<contributor>Institut de Physique du Globe de Paris (IPGP) ; 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>Laboratoire de Recherche en Géosciences et Énergies (LaRGE) ; Université des Antilles et de la Guyane (UAG)</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>insu-01586768</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01586768</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01586768/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01586768/file/Feuillet_et_al-2010-Geophysical_Research_Letters.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01586768</source>
<source>Geophysical Research Letters, American Geophysical Union, 2010, 37 (19), pp.L00E15. 〈10.1029/2010GL042556〉</source>
<identifier>DOI : 10.1029/2010GL042556</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2010GL042556</relation>
<language>en</language>
<subject>[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanology</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>New high-resolution marine data acquired aboard R/V Le Suroît was used to map active normal faults offshore Montserrat in greater detail. The main faults of the Montserrat-Havers fault zone have cumulative scarps up to 200 m high, and offset sedimentary layers by hundreds of meters. They are arranged in a right-stepping, en echelon, trans-tensional array, which confirms that they accommodate the left-lateral component of motion resulting from slip partitioning of oblique convergence along the volcanic arc. They cut across Montserrat's recent volcanic complex. Faulting and fissuring exerted control on the position of andesitic domes, which are aligned along the N110°E average fault trend. The ≈10 km-long fault segments that cross the island could produce damaging, M ≈ 6 events comparable to the shallow, 16 March 1985, Mw∼6.3 earthquake that ruptured a submarine, N140°E striking, left-lateral fault near Redonda.</description>
<date>2010</date>
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