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dc.contributor.authorEguiluz, Luis
dc.contributor.authorÁbalos, Benito
dc.contributor.authorGil Ibarguchi, José Ignacio
dc.date.accessioned2020-06-09T16:20:33Z
dc.date.available2020-06-09T16:20:33Z
dc.date.issued1989
dc.identifier.urihttp://hdl.handle.net/10272/18239
dc.description.abstractC-type eclogites occur within garnet-amphibo/ites of the Azuaga gneisses a/lochthon in the Badajoz-Córdoba shear belt (SW Spain). The eclogites were formed under conditions of ca. 600 0 C, > 73 Kbar, and record a complex evolution related to various espisodes of recrystallization and deformation. The Badajoz-Córdoba shear belt may be interpreted in terms of a polyphase geodynamic evolution involving initial Upper-Proterozoic to EarlyCambrian subduction, followed by continental collision, Middle Paleozoic crustal extension and intense Upper Paleozoic (Hercynian) intracontinental ductile wrenchinges_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.otherEclogiteses_ES
dc.subject.otherBadajozes_ES
dc.subject.otherCórdobaes_ES
dc.subject.otherHigh-pressurees_ES
dc.subject.otherHercynianes_ES
dc.subject.otherSpaines_ES
dc.titleEclogitas de la banda de Cizalla Badajoz-Córdoba (Suroeste de España). Datos petrográficos y significado geodinámicoes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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