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dc.contributor.authorTesón, E.
dc.contributor.authorTeixell, Antonio
dc.date.accessioned2014-07-28T08:44:31Z
dc.date.available2014-07-28T08:44:31Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8630
dc.description.abstractThe Sub-Atlas thrust belt and Ouarzazate basin constitutes the best and almost the unique synorogenic record of the Atlas mountain building. During the Eocene and Oligocene the deformation was concentred in the distant High Atlas whereas the marginal thrust belt was scarcely deformed. In Late Oligocene to early Miocene, deformation migrated forelandwards when complex thrust sequences created the Sub- Atlas foreland fold and thrust belt. Thrusting took place up to Pliocene times entraining the synorogenic sedimentary rocks, locally-sourced terrigenous and lacustrine depositsen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Españaen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherThrust sequenceen_US
dc.subject.otherTectonics – sedimentationen_US
dc.subject.otherOuarzazate basinen_US
dc.subject.otherHigh Atlasen_US
dc.subject.otherMoroccoen_US
dc.titleSecuencia de cabalgamientos en la Zona Sub-Atlásica y cuenca de Ouarzazate; borde sur del Alto Atlas (Marruecos)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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Atribución-NoComercial-SinDerivadas 3.0 España
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