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Proposal of a structural setting for the giant volcanogenic massive sulphide deposit of Río Tinto, Iberian Pyrite Belt

dc.contributor.authorGonzález Clavijo, Emilio J.
dc.contributor.authorDíez Montes, Alejandro
dc.date.accessioned2014-03-18T10:27:28Z
dc.date.available2014-03-18T10:27:28Z
dc.date.issued2010
dc.identifier.urihttp://hdl.handle.net/10272/7906
dc.description.abstractNew field reconnaissance around the Río Tinto Mine led to a better structural knowledge on the area. The improved map support a different geological evolution on this sector determined by an earlier extensional event, which probably conditioned the mineralization processes. Later compressive poly-cyclic Variscan events developed thin-skinned tectonicsen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherStructureen_US
dc.subject.otherDetachmenten_US
dc.subject.otherThin-skinneden_US
dc.subject.otherVariscanen_US
dc.subject.otherRío Tintoen_US
dc.titlePropuesta de estructura geológica para el depósito gigante de sulfuros masivos volcanogénicos de Río Tinto, Faja Pirítica Ibéricaen_US
dc.titleProposal of a structural setting for the giant volcanogenic massive sulphide deposit of Río Tinto, Iberian Pyrite Belteng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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