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Fluid-deposited graphite: The mineralization from Huelma (Jaen)

dc.contributor.authorRodas, M.
dc.contributor.authorBarrenechea, J. F.
dc.contributor.authorLuque, F. J.
dc.date.accessioned2017-01-27T11:41:07Z
dc.date.available2017-01-27T11:41:07Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/13218
dc.description.abstractThe volcanic-hosted graphite mineralization of Huelma Qaén) has been studied in order to stablish the mineralogical characteristics and mechanisms of formation. The graphite is highly ordered (as revealed by XRD and Raman data) and rather pure chemically (C content >90% ). The isotopic signature (8 13C = -23 to -20.7%o) and other geological evidences indicate that C in these graphites is derived from the organic matter included in the metamorphic basementen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGraphiteen_US
dc.subject.otherFluid-depositionen_US
dc.subject.otherBetic Cordillerasen_US
dc.titleFormación de grafito a partir de fluidos: La mineralización de Huelma (Jaén)en_US
dc.titleFluid-deposited graphite: The mineralization from Huelma (Jaen)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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