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dc.contributor.authorD'Acremont, E.-
dc.contributor.authorGorini, Christian-
dc.contributor.authorElabbassi, Mohammed-
dc.contributor.authorFarran, Marcel-lí-
dc.contributor.authorLeroy, Sylvie-
dc.contributor.authorMercier de Lépinay, Bernard-
dc.contributor.authorMigeon, S.-
dc.contributor.authorPoort, Jeffrey-
dc.contributor.authorAmmar, Abdellah-
dc.contributor.authorSmit, Jeroen-
dc.contributor.authorDo Couto, Damien-
dc.contributor.authorErcilla, Gemma-
dc.contributor.authorAlonso, Belén-
dc.date.issued2012-05-22-
dc.identifier.urihttp://hdl.handle.net/10261/49924-
dc.description.abstractSince the Tortonian, the thinned continental crust and the overlying sedimentary cover of the Alboran Sea are submitted to tectonic inversion due to the convergence between Eurasia and Africa. The past and present deformation is significant along the Moroccan margin where the MARLBORO-1 cruise in 2011, acquired 1100 km of mid-resolution seismic reflection along 20 profiles perpendicular and parallel to the margin, off Al Hoceima, to latitude 36°N. The study area located on the Xauen/Tofino banks and the South Alboran ridge off Morocco, shows signs of both past and present strong tectonic deformation, submarine landslides, and contouriteses_ES
dc.description.abstractEGU General Assembly 2012, Vienna, 22-27 Apriles_ES
dc.language.isoenges_ES
dc.rightsopenAccesses_ES
dc.subjectAlboranes_ES
dc.subjectSeismices_ES
dc.subjectSedimentaryes_ES
dc.subjectTectonices_ES
dc.subjectMessinianes_ES
dc.subjectPlio-Quaternaryes_ES
dc.subjectContouriteses_ES
dc.subjectXauen-Tofiñoes_ES
dc.titleA seismic survey in the South Alboran Sea: past and present active sedimentary systems and tectonicses_ES
dc.typecomunicación de congresoes_ES
dc.description.peerreviewedPeer reviewedes_ES
Appears in Collections:(ICM) Comunicaciones congresos
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