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Geochemical differentiation of «Weald» materials of Cameros Basin (Soria - La Rioja)

dc.contributor.authorMata Campo, M. P.
dc.contributor.authorOsácar, María Cinta
dc.contributor.authorLópez Aguayo, F.
dc.date.accessioned2016-06-08T08:22:37Z
dc.date.available2016-06-08T08:22:37Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12260
dc.description.abstractThe Cameros Basin ( N W o f the Iberian Range) is m a in ly composed o f very homogeneous silicic d e tr ita l m aterials in Weald facies. The occurrence o f c h lo rito id , cookeite, p y rite an d muscovite/p aragonite is related to a cretacic very low grade metamorphism. The geochemical analysis of this materials displays differences linked to lithologic features; comparison between metamorphic and no metamorphic materials shows no main differences in the chemical contents, but in the relationships between elementsen_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.otherCameros Basinen_US
dc.subject.otherWeald faciesen_US
dc.subject.otherGeochemistryen_US
dc.subject.otherVery Low grade - Metamorphismen_US
dc.titleDiferenciación geoquímica de los materiales en facies «Weald» de la Cuenca NE de Cameros (Soria - La Rioja)en_US
dc.titleGeochemical differentiation of «Weald» materials of Cameros Basin (Soria - La Rioja)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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