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Stratigraphic arquitecture of a storm-dominated shallow marine platform (Valmaseda Fm., Up. Albian - Lw. Cenomanian, Basque Cantabrian Basin)

dc.contributor.authorPérez García, Adán
dc.contributor.authorRobles, Sergio
dc.contributor.authorVicente Bravo, J. C.
dc.date.accessioned2015-05-08T09:00:09Z
dc.date.available2015-05-08T09:00:09Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10521
dc.description.abstractThe Valmaseda Fm. comprises a thick siliciclastic shallow marine depositions! system, developed in the southern margin of the Basque Cantabrian basin. Its western sector, located ¡between the Tornos Pass (Cantabria-Burgos) and Llodio (Alava) displays a thickness ranging from 1000 to 3500 m. Detailed facies analysis have allowed to establish five facies assemblages which build up the basic facies tract. It consists on a prograding / shallowing upward sequence developed on a storm-dominated siliciclastic platform. The stacking pattern of these basic sequences yields composite higher rank sedimentary cycles which represent overall shallowing upward / prograding units of regional extent, capped by transgresive deposits. These sedimentary cycles can be further grouped into four regionally extensive stratigraphic units which outline four depositional stages controlled by sedimentary tectonics. These comprise: encroachment of shallow marine siliciclastic fades within a tectonicilly induced trough, spreading of shallow marine facies across the studied area, phase of strong differential subsidence, and sharp replacement of siliciclastic facies by outer shelf carbonate fadesen_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.otherStratigraphic arquitectureen_US
dc.subject.otherStorm-dominated siliclastic platformen_US
dc.subject.otherBasque Cantabrian basinen_US
dc.subject.otherAlbian - Lw. Cenomanianen_US
dc.titleArquitectura estrati gráfica del sistema de plataforma dominada por tormentas de la Fm. Valmaseda (Albiense sup.-Cenomaniense inf. de la cuenca Vascocantábrica)en_US
dc.titleStratigraphic arquitecture of a storm-dominated shallow marine platform (Valmaseda Fm., Up. Albian - Lw. Cenomanian, Basque Cantabrian Basin)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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Atribución-NoComercial-SinDerivadas 3.0 España
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