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Comparison of provenace results between lutitic and sandstone sediments: An example from Permotriassic of Desert de les Palmes area (Castellón)

dc.contributor.authorMartín Martín, Juan Diego
dc.contributor.authorGómez Gras, David
dc.contributor.authorSanfeliu, T.
dc.date.accessioned2015-02-13T10:39:16Z
dc.date.available2015-02-13T10:39:16Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9915
dc.description.abstractThe present study stablishes the compositional relation between sandstone and lutitic levels of the Permian and Triassic succession from Desert de les Palmes area (Castellón). The evolution shows a general quartz and kaoHnite decrease up of the serie, and an increase of illite and metamorphic fragments. Different relation between quartz-kaolinite and illite-metamorphic fragments have been associated with the sediment provenance and the geological evolution of the source area. Lower Unit derived from the erosion of an important weathered layer rich in quartz, kaoHnite and iron oxides developed on the Hercyninan materials. The continuous erosion of the source area lowered the weathering cover influence on the sedimentation of Middle and Upper Unitsen_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.otherPermianen_US
dc.subject.otherTriassicen_US
dc.subject.otherLutitesen_US
dc.subject.otherSandstonesen_US
dc.subject.otherProvenanceen_US
dc.subject.otherWeatheringen_US
dc.titleAnálisis comparativo de procedencia de sedimentos lutíticos y arenosos interestratificados: El Permotrías del Desert de les Palmes (Castellón)en_US
dc.titleComparison of provenace results between lutitic and sandstone sediments: An example from Permotriassic of Desert de les Palmes area (Castellón)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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