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Temporal evolution of clay mineralassemblages in the Upper Permlan - Triassic materíals oí Cuenca and Teruel (SE Iberian Range)

dc.contributor.authorAlonso Azcárate, Jacinto
dc.contributor.authorArche, A.
dc.contributor.authorBarrenechea, J. M.
dc.contributor.authorLópez Gómez, José
dc.contributor.authorLuque, F. J.
dc.contributor.authorRodas, M.
dc.date.accessioned2017-07-20T11:30:39Z
dc.date.available2017-07-20T11:30:39Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/13951
dc.description.abstractClay mineralogy of the continetal and shallow marine sediments of Permian and Triassic age of the SE Iberian Ranges is a neglected subject. The present study shows the temporal variations of clay mineral assemblages and point out to two main primary controls: nature of the source area and sedimentary environments. Later diagenetic processes have not altered substantially the original mineralogyes_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.otherMinerales de la arcillaes_ES
dc.subject.otherPérmicoes_ES
dc.subject.otherTriásicoes_ES
dc.subject.otherCordillera Ibérica SEes_ES
dc.subject.otherPaleogeografíaes_ES
dc.titleLa evolución temporal de los minerales de la arcilla en el Pérmico superior y Triásico de Cuenca y Teruel (Cordillera Ibérica SE)es_ES
dc.titleTemporal evolution of clay mineralassemblages in the Upper Permlan - Triassic materíals oí Cuenca and Teruel (SE Iberian Range)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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