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Neoformation of barite in The Villamayor sdndslone (Salamanca). Preliminary study

dc.contributor.authorAlonso Gavilán, G.
dc.contributor.authorMoro Benito, M. C.
dc.contributor.authorCembranos Pérez, M. L.
dc.contributor.authorAreas, A.
dc.date.accessioned2015-05-08T09:22:34Z
dc.date.available2015-05-08T09:22:34Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10524
dc.description.abstractThe barite studied in the Villamayor sandstone is located in old rhizoliths related to subvertical fractures which affect these subarcosic deposits. These zones are actually in great circulation within underground waters and full of clay materials. The mineral's form together with ist mineralogical, chemical and isotopic characteristics suggests that its formation is related with the postneogene alteration processes (caolinitization) of sandstones which liberate Ba of the feldspars and with the infiltration and circulation of metheoric waters that contain dissolved sulphatesen_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.otherBariteen_US
dc.subject.otherNeoformationen_US
dc.subject.otherVillamayor Sandstonesen_US
dc.subject.otherSalamancaen_US
dc.titleBarita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminaren_US
dc.titleNeoformation of barite in The Villamayor sdndslone (Salamanca). Preliminary studyeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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