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dc.rights.licenseopenen_US
dc.contributor.authorRODRIGUEZ, Mathieu
dc.contributor.authorCHAMOT-ROOKE, Nicolas
dc.contributor.authorROOKE, Nicolas Chamot
dc.contributor.authorHUCHON, Philippe
dc.contributor.authorFOURNIER, Marc
dc.contributor.authorLALLEMANT, Siegfried
dc.contributor.authorDELESCLUSE, Matthias
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.contributor.authorMOUCHOT, Nicolas
dc.date.accessioned2024-10-24T12:21:22Z
dc.date.available2024-10-24T12:21:22Z
dc.date.issued2014-12-01
dc.identifier.issn0040-1951en_US
dc.identifier.urihttps://hal.archives-ouvertes.fr/hal-01059557
dc.identifier.uriorcid:0000-0002-9256-0034:10.1016/j.tecto.2014.08.001
dc.identifier.urioai:crossref.org:10.1016/j.tecto.2014.08.001
dc.identifier.uriftecolephe:oai:HAL:hal-01059557v1
dc.identifier.urioai:researchgate.net:264752708
dc.identifier.uriorcid:0000-0001-9924-749X:10.1016/j.tecto.2014.08.001
dc.identifier.urioadoi:https://hal.archives-ouvertes.fr/hal-01059557/document
dc.identifier.urioadoi:https://hal.archives-ouvertes.fr/hal-01059557/file/rodriguez_tectonophy_2014.pdf
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202710
dc.description.abstractEnThe Dalrymple Trough is a 150-km-long, 30-km-wide basin located at the northern termination of the Owen Fracture Zone (OFZ), which is the present-day active India-Arabia plate boundary. The Dalrymple Trough is closely associated with the Murray Ridge, a complex of prominent bathymetric highs located on its eastern flank. Recent multibeam mapping of the connection between the Dalrymple Trough and the OFZ revealed a horsetail structure, which suggests a close relationship between geological histories of both structures. However, the 3-6 Ma age of initiation of the OFZ contrasts with the commonly accepted Early Miocene emplacement of the Dalrymple Trough. Recent seismic lines document a new tectonic history of the Dalrymple Trough, involving two major episodes of deformation along the India-Arabia plate boundary at ~ 8-10 Ma and ~ 1.9 ± 0.9 Ma. The 8-10 Ma episode is marked by a system of folds linked to the main uplift of the southern Murray Ridge and the first uplift of the northern Murray Ridge. This episode is related to a global plate reorganization event in the Late Miocene, well expressed by intraplate deformation in the Central Indian Ocean. The Dalrymple Trough opened at ~ 1.9 ± 0.9 Ma subsequently to the formation of a stepover at the India-Arabia plate boundary, coeval with the regional M-unconformity in the Oman abyssal plain, which marks a structural reorganization of the Makran accretionary wedge, and the last uplift of the northern Murray Ridge.
dc.language.isoENen_US
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dc.sourceresearchgate
dc.sourceoadoi_repo
dc.title.enTectonics of the Dalrymple Trough and uplift of the Murray Ridge (NW Indian Ocean)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.tecto.2014.08.001en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalTectonophysicsen_US
bordeaux.page1-17en_US
bordeaux.volume636en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_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
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dc.rights.ccPas de Licence CCen_US
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