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dc.contributor.authorLafosse, M.
dc.contributor.authord'Acremont, E.
dc.contributor.authorRabaute, A.
dc.contributor.authorVázquez, J.T. (Juan Tomás)
dc.contributor.authorEstrada, F.
dc.contributor.authorGalindo-Zaldívar, J.
dc.contributor.authorErcilla, G.
dc.contributor.authorAlonso, B.
dc.contributor.authorGorini, Ch.
dc.date.accessioned2017-09-21T14:57:09Z
dc.date.available2017-09-21T14:57:09Z
dc.date.issued2017-04-23
dc.identifier.urihttp://hdl.handle.net/10508/11273
dc.description.sponsorshipEUROPEAN GEOPHYSICAL UNIONes_ES
dc.language.isoenges_ES
dc.subjectALBORAN MARGINes_ES
dc.subjectTECTONICSes_ES
dc.titleOblique basin inversion and strain partitioning in back-arc context: example from the Moroccan Alboran Margin (Western Mediterranean)es_ES
dc.typeconferenceObjectes_ES
dc.identifier.bibliographicCitationEGU General Assembly 2017. (23/04/2017 - 28/04/2017. Viena (Austria)). 2017. . En: Geophysical Research Abstracts, 19, EGU2017-15654.*
dc.publisher.centreCentro Oceanográfico de Málagaes_ES
dc.relation.projectIDMONTERAes_ES
dc.rights.accessRightsopenAccesses_ES
dc.subject.asfaabstractses_ES
dc.subject.asfaseismic dataes_ES
dc.subject.asfasubsidencees_ES


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