El origen del azufre en mineralizaciones filonianas en el centra de la Península Ibérica

dc.contributor.authorLillo Bevia, J.
dc.contributor.authorOyarzun, Roberto
dc.contributor.authorOrtega, Lorena
dc.date.accessioned2017-02-24T12:42:09Z
dc.date.available2017-02-24T12:42:09Z
dc.date.issued1995
dc.description.abstractSulphur isotope data from several base metals-Ba-(F)-(Ag) and Ag-base metals vein-type deposits in the Central Iberian Zone o f the Hesperian Massif suggest a magmatic and /or metasedimentary origin o f this ore-forming component. Deposits exclusively hosted in metasediments (p.e. Alcudia Valley, type IV) display a magmatic signature. Even those lodes and stratabound deposits hosted by Permian-Triassic terrigenous and andesites (Las Torrecillas-Linares y Atienza) are formed by "igneous" sulphuren_US
dc.identifier.urihttp://hdl.handle.net/10272/13389
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPb-Znen_US
dc.subject.otherAgen_US
dc.subject.otherVein-type mineralizationsen_US
dc.subject.otherSpanish Central Systemen_US
dc.subject.otherLinares-La Carolinaen_US
dc.subject.otherAlcudia Valleyen_US
dc.subject.otherCentral Iberian Zoneen_US
dc.titleEl origen del azufre en mineralizaciones filonianas en el centra de la Península Ibéricaen_US
dc.titleOrigin of sulphur in vein-type deposits in central Iberian Peninsulaeng
dc.typejournal articleen_US
dspace.entity.typePublication

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