Yacimiento de arcilla caolinífera de relleno Kárstico en Chavaler (Cordillera Ibérica, Soria)

dc.contributor.authorSanz Pérez, Eugenio
dc.date.accessioned2014-10-29T12:39:06Z
dc.date.available2014-10-29T12:39:06Z
dc.date.issued2003
dc.description.abstractThe Chavaler karstic deposit is a clay accumulation in a dolina of 90 m in diameter. Clay minerals are represented mainly by kaolinite (80% kaolinite, 20% quartz) and locally also kaolinite-gibbsite facies, and natroaluite. The feldespatic detrital material of the Weald Facies was deposited on a pre-existing prefinimiocene-Pleistocene karst. The karst depression has protected kaolinic deposits from further erosion. The favourable drainage contributed to the kaolinization and initial bauxitizationen_US
dc.identifier.urihttp://hdl.handle.net/10272/9021
dc.language.isospaen_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.otherKaolin depositsen_US
dc.subject.otherPaleokarsten_US
dc.subject.otherIberian Chainen_US
dc.titleYacimiento de arcilla caolinífera de relleno Kárstico en Chavaler (Cordillera Ibérica, Soria)en_US
dc.titleThe Chavaler Kaolin Karstic deposits (Iberian Chain, Soria)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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