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Evolution of clay mineral in the Lorca basin (Murcia)

dc.contributor.authorGuillén Mondéjar, F.
dc.contributor.authorMancheño, Miguel Ángel
dc.contributor.authorArana, R.
dc.contributor.authorLópez Aguayo, F.
dc.date.accessioned2017-03-07T11:34:14Z
dc.date.available2017-03-07T11:34:14Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13408
dc.description.abstractThe clay mineral association of the Lorca basin (Murcia) is built by muscovite, chlorite (clinochlore), montmorillonite, kaolinite and something of paragonite. The application of statistical methods, the factor analysis and the analysis mineralogical: space-temporal distribution, mineral associations, mufua/ relationships and crystalchemical parameters, have allowed to know the possible source areas, the processes of transport and sedimentation-and climatology in each TSUen_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.otherLorca basinen_US
dc.subject.otherClay mineralen_US
dc.subject.otherNeogeneen_US
dc.titleLa evolución de los minerales de la arcilla en la cuenca de Lorca (Murcia)en_US
dc.titleEvolution of clay mineral in the Lorca basin (Murcia)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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