Aluminium mohility in hydrothermally altered granités

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dc.contributor.authorLillo Bevia, J.
dc.contributor.authorLópez Sopeña, F.
dc.date.accessioned2017-03-20T11:20:50Z
dc.date.available2017-03-20T11:20:50Z
dc.date.issued1995
dc.description.abstractImmobile elements are used to evaluate metasomatism caused by hydrothermal alteration in Linares granite related to Ba-(base metals) veins. Mass transfers of Aluminium (which Is commonly considered as the best monitor) are been detected by correlating the monitor elements, being Zr used as more reliable monitoren_US
dc.description.abstractEl metasomatismo de la adamellita de Linares, causado por la alteración hidrotermal asociada a filones de Ba-(Pb-Zn), es evaluado utilizando elementos inmóviles como monitores. Por correlación, se comprueba que existe transferencia de Al, utilizándose Zr como elemento de referenciaen_US
dc.identifier.urihttp://hdl.handle.net/10272/13460
dc.language.isoengen_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.otherHydrothermal alterationen_US
dc.subject.otherGranite metasomatismen_US
dc.subject.otherAluminiumen_US
dc.subject.otherBa-(Pb-Zn) oreen_US
dc.subject.otherLinaresen_US
dc.titleAluminium mohility in hydrothermally altered granitésen_US
dc.titleMobilidad del aluminio en granitos hidrotermalmente alteradosspa
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)