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dc.contributor.authorGarcía Dueñas, V.
dc.contributor.authorMartínez Martínez, J. M.
dc.contributor.authorOrozco, Miguel
dc.contributor.authorMartín Ramos, D.
dc.date.accessioned2020-07-03T13:58:43Z
dc.date.available2020-07-03T13:58:43Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18421
dc.description.abstractThe Veleta Unit and the Mulhacen nappe Group (Calar Alto and Bédar-Macael Nap pes) make up the Nevado-Filábride Complex. The westward movement of the both nappes occurred along NW to WSW trajectories. [n the Sierra Nevada, the nappe pile is strongly thinnedes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMylonitic fabricses_ES
dc.subject.otherShear zoneses_ES
dc.subject.otherNappeses_ES
dc.subject.otherBetic Cordillerases_ES
dc.titleEl sentido de desplazamiento de los Mantos Nevado-Filábrideses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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