Relación estructural entre los cuerpos peridotíticos situados al Norte y al Sur del Estrecho de Gibraltar

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dc.contributor.authorSánchez Gómez, Mario
dc.contributor.authorGarcía Dueñas, V.
dc.contributor.authorMuñoz, Mercedes
dc.contributor.authorBalanyá, Juan Carlos
dc.date.accessioned2017-07-11T10:27:52Z
dc.date.available2017-07-11T10:27:52Z
dc.date.issued1994
dc.description.abstractThe peridotite bodies of the Bedes and Rif, on either side of the Strait of Gibraltar, are intercaled among the highest units of the Alpujarride complex. Before Miocene times, they must have constituted an uitramaficsiab (several kilometers thick). This former slab was fragmented by large extensionai structures developed during the formation of the Gibraltar Arc and the Alboran Basines_ES
dc.identifier.urihttp://hdl.handle.net/10272/13922
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherRonda peridotitees_ES
dc.subject.otherCrustal thinninges_ES
dc.subject.otherGibraltar Arces_ES
dc.titleRelación estructural entre los cuerpos peridotíticos situados al Norte y al Sur del Estrecho de Gibraltares_ES
dc.titleStructural relationships between the peridotíte bodies located northw ard and southw ard the Strait of Gibraltareng
dc.typeconference outputes_ES
dspace.entity.typePublication

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Geogaceta -- Nº 17, (1994)