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Calatayud Gypsum: application of the study of sulphates facies and geochemistry to the knowledge of an evaporitic system

dc.contributor.authorOrtí, Federico
dc.contributor.authorRosell, L.
dc.contributor.authorFallick, A. E.
dc.contributor.authorUtrilla, R.
dc.date.accessioned2017-08-07T10:59:33Z
dc.date.available2017-08-07T10:59:33Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/14016
dc.description.abstractThe study of depositional and diagenetic calcium-sulphate evaporites in the Calatayud Gypsum (Zaragoza prov., Spain), reveals the existence of a NW to SE elongated and relatively asymmetrical arrangement in this Miocene lacustrine system. In this particular arrangement a marginal belt exists of bioturbated gypsum, surrounding a central body formed by nodular laminated-facies. This marginal belt is narro win the N W zone and wider in the SE zone. The isotopic compositions (8'30 , 8 34S) of all the studied samples suggest that a concentration gradient occurred in the basin towards the NW area of the central body, where the more saline waters and the depocentre were probably located.es_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.otherGypsumes_ES
dc.subject.otherEvaporiteses_ES
dc.subject.otherGeochemistryes_ES
dc.subject.otherMiocenees_ES
dc.subject.otherCalatayudes_ES
dc.subject.otherSpaines_ES
dc.titleYesos de Calatayud: aplicación del estudio de facies y geoquímica de sulfatos al conocimiento de un sistema evaporíticoes_ES
dc.titleCalatayud Gypsum: application of the study of sulphates facies and geochemistry to the knowledge of an evaporitic systemeng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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