Inversión estructural en la cuenca mesozoica del off-shore asturiano. Revisión de un modelo exploratorio

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dc.contributor.authorRiaza Molina, C.
dc.date.accessioned2015-11-23T10:57:43Z
dc.date.available2015-11-23T10:57:43Z
dc.date.issued1996
dc.description.abstractIn the off-shore area of the Asturian and Cantabrian provinces a mesozoic-cenozoic basin develops with an important thickness of the Upper Jurassic and lower Cretaceous series. The partial closure of the Biscay Bay during the Eocene caused a shortening of the series and produced a structural inversion of the Jurassic-Lower Cretaceous depocenters. The majority of the unsuccessful oil wells were drilled on the inverted anticlines located in this areaen_US
dc.identifier.urihttp://hdl.handle.net/10272/11399
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.otherStructural inversionen_US
dc.subject.otherAsturian basinen_US
dc.subject.otherRegional geologyen_US
dc.subject.otherCantabrian basinen_US
dc.subject.otherOil explorationen_US
dc.subject.otherSantander arcen_US
dc.subject.otherBay of Biscayen_US
dc.titleInversión estructural en la cuenca mesozoica del off-shore asturiano. Revisión de un modelo exploratorioen_US
dc.titleStructural inversion in the off-shore mesozoic asturian basin. Revision of an exploratory modeleng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-1, (1996)