Deformaciones plio-cuaternarias en la region de Rabat

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dc.contributor.authorAkil, Mustafa
dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorTahayt, A.
dc.contributor.authorJabaloy, A.
dc.contributor.authorChabli, A.
dc.contributor.authorRuano, Patricia
dc.contributor.authorChalouan, Ahmed
dc.date.accessioned2015-01-28T13:50:43Z
dc.date.available2015-01-28T13:50:43Z
dc.date.issued2000
dc.description.abstractThe Rabat region, located in the northern border of the Moroccan Meseta, is generally considered as a present-day stable region. However, the fluvial and marine sedimentary rocks, with Pliocene and Quaternary ages, are deformed by joints, generally tensional, and by normal and strike-slip faults. The brittle structures indicate N-S compressional deformations, probably related to the present-day regional stresses in the crust, and extensional deformations related to the proximity to the Gharb basinen_US
dc.identifier.urihttp://hdl.handle.net/10272/9765
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMoroccan Mesetaen_US
dc.subject.otherRabaten_US
dc.subject.otherRecent tectonicsen_US
dc.subject.otherBrittle deformationsen_US
dc.titleDeformaciones plio-cuaternarias en la region de Rabaten_US
dc.titlePlio-Quaternary deformations in the Rabat regioneng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 29, (2000)