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The Gordexola Formation sandstones (Albian, south limb of the Bilbao anticlinorium, Vizcaya). II: Cementation and diagenesis

dc.contributor.authorZuluaga, María Cruz
dc.contributor.authorGarcía Garmilla, Francisco
dc.contributor.authorArostegui García, Javier
dc.date.accessioned2015-05-12T11:50:52Z
dc.date.available2015-05-12T11:50:52Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10582
dc.description.abstractThe sandstones of the Gordexola Formation were studied using petrography, cathodoluminescence, electronic microprobe, SEM, and C and O isotopic relations. A diagenetic sequence was inferred from medium to late stages. The processes that affected sandstones occurred from syntaxial siliceous cements to different carbonates that precipitated and replaced previous felsdpar grains. Temperatures of late diagenesis could oscillate from 40° to 45° C. The very late diagenesis consisted on deformation of both grains and crystals under burial conditionsen_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.otherLower-to-middle Albianen_US
dc.subject.otherSandstone medium-to-late diagenesisen_US
dc.subject.otherSiliceous and carbonate cementsen_US
dc.subject.otherBurial compactionen_US
dc.titleLas areniscas de la Formación de Gordexola (Albiense, flanco sur del Anticlinorio de Bilbao, Vizcaya) II: Cementación y diagénesisen_US
dc.titleThe Gordexola Formation sandstones (Albian, south limb of the Bilbao anticlinorium, Vizcaya). II: Cementation and diagenesiseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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