Interacción entre la tectónica local y los eventos oceánicos en el Cenomaniense-Turoniense de la Cuenca de Sopeira (Pirineos)

dc.contributor.authorCaus, E.
dc.contributor.authorTeixell, Antonio
dc.contributor.authorBernaus, J. M.
dc.date.accessioned2016-05-30T09:27:53Z
dc.date.available2016-05-30T09:27:53Z
dc.date.issued1996
dc.description.abstractThe Sopeira Basin is a small extensional basin with a conlinuous record of deposition from the upper Albian to the upper Turonian. In its early stages (upper Albian-middle Cenomanian) the sedimentation was controlled by local factors (extensional tectonics) with an influence of eustatic sea- level change. Later, during the upper Cenomanian-middle Turonian, the main sedimentary features are controlled mainly by global oceanic changesen_US
dc.identifier.urihttp://hdl.handle.net/10272/12190
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherTectonicsen_US
dc.subject.otherEustasyen_US
dc.subject.otherEutrophycationen_US
dc.subject.otherCenomanian-Turonianen_US
dc.subject.otherPyreneesen_US
dc.titleInteracción entre la tectónica local y los eventos oceánicos en el Cenomaniense-Turoniense de la Cuenca de Sopeira (Pirineos)en_US
dc.titleInteraction between local tectonics and oceanic events in the Cenomanian- Turonian of the Sopeira Basin (Pyrenees)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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