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dc.rights.licenseopenen_US
dc.contributor.authorFOURNIER, Marc
dc.contributor.authorCHAMOT-ROOKE, Nicolas
dc.contributor.authorRODRÍGUEZ, Mathieu
dc.contributor.authorHUCHON, Philippe
dc.contributor.authorPETIT, Carole
dc.contributor.authorBESLIER, Marie-Odile
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.date.accessioned2024-10-25T08:05:36Z
dc.date.available2024-10-25T08:05:36Z
dc.date.issued2011-02-01
dc.identifier.issn0012-821Xen_US
dc.identifier.urihttp://hal.archives-ouvertes.fr/hal-00577753/en/
dc.identifier.urihttps://hal.archives-ouvertes.fr/hal-00577753
dc.identifier.uriorcid:0000-0002-9256-0034:10.1016/j.epsl.2010.12.027
dc.identifier.urioai:crossref.org:10.1016/j.epsl.2010.12.027
dc.identifier.urioadoi:https://hal.archives-ouvertes.fr/hal-00577753/file/ms_revised_fig.pdf
dc.identifier.uriftccsdartic:oai:hal.archives-ouvertes.fr:hal-00577753
dc.identifier.uriftunivnice:oai:HAL:hal-00577753v1
dc.identifier.urioai:researchgate.net:50403558
dc.identifier.uriorcid:0000-0001-9924-749X:10.1016/j.epsl.2010.12.027
dc.identifier.urioadoi:https://hal.archives-ouvertes.fr/hal-00577753/document
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202796
dc.description.abstractEnWe surveyed the Owen Fracture Zone at the boundary between the Arabia and India plates in the NW Indian Ocean using a high-resolution multibeam echo-sounder (Owen cruise, 2009) for search of active faults. Bathymetric data reveal a previously unrecognized submarine fault scarp system running for over 800 km between the Sheba Ridge in the Gulf of Aden and the Makran subduction zone. The primary plate boundary structure is not the bathymetrically high Owen Ridge, but is instead a series of clearly delineated strike-slip fault segments separated by several releasing and restraining bends. Despite an abundant sedimentary supply by the Indus River flowing from the Himalaya, fault scarps are not obscured by recent deposits and can be followed over hundreds of kilometres, pointing to very active tectonics. The total strike-slip displacement of the fault system is 10-12 km, indicating that it has been active for the past ~3 to 6 Ma if its current rate of motion of 3±1 mm yr−1 has remained stable. We describe the geometry of this recent fault system, including a major pull-apart basin at the latitude 20°N, and we show that it closely follows an arc of small circle centred on the Arabia-India pole of rotation, as expected for a transform plate boundary.
dc.language.isoENen_US
dc.sourceorcid
dc.sourcecrossref
dc.sourceoadoi_repo
dc.sourcebase
dc.sourceresearchgate
dc.title.enOwen Fracture Zone: The Arabia–India plate boundary unveiled
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.epsl.2010.12.027en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalEarth and Planetary Science Lettersen_US
bordeaux.page247-252en_US
bordeaux.volume302en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1-2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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