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Clay mineral distribution in the Cuestas Unit (Neogene of the Duero Basin)

dc.contributor.authorCorrochano, A.
dc.contributor.authorArmenteros, Ildefonso
dc.contributor.authorPérez Pérez, C.
dc.contributor.authorSánchez de Vega, A.
dc.contributor.authorSan Dimas, L. E.
dc.date.accessioned2020-05-22T10:13:55Z
dc.date.available2020-05-22T10:13:55Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/18052
dc.description.abstractThe spatial distribution of clay minerals in the Cuestas Unit is described in this work. Cartographic distribution of the different minerals points towards a tectonic control of the genetic environments, resulting in NE-SW elongated bands. Kaolinite+chlorite and illite are located towards marginal areas of the Unit Palygorskite is concentrated in distal areas of a//uvial fans, derived from source areas located both to the NW and from the Honrubia basement area. Sepiolite and smectite concentrations are associated with evaporitic lacustrine basins, mainly located close to the Honrubia Massifes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMiocenees_ES
dc.subject.otherDuero Basines_ES
dc.subject.otherKaolinitees_ES
dc.subject.otherIllitees_ES
dc.subject.otherPalygorskitees_ES
dc.subject.otherSepiolitees_ES
dc.subject.otherSmectitees_ES
dc.titleDistribución de arcillas en la Unidad de Cuestas (Neógeno de la Cuenca del Duero)es_ES
dc.titleClay mineral distribution in the Cuestas Unit (Neogene of the Duero Basin)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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