Tectónica distensiva y halocinesis en el margen SO de la cuenca Vasco- Cantábrica

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dc.contributor.authorSerrano, A.
dc.contributor.authorHernaiz Huerta, Pedro P.
dc.contributor.authorMalagón, J.
dc.contributor.authorRodríguez Cañas, C.
dc.date.accessioned2017-08-01T10:37:11Z
dc.date.available2017-08-01T10:37:11Z
dc.date.issued1994
dc.description.abstractExtensional tectonics and associated halokinetics processes controlled the sedimentation in the southwestern margin of the Basco-Cantabrian basin during Upper Jurassic and Lower Cretaceous times. The development of Mesozoic growth faults, compressive features at present, controlled the geometry and limits of the sedimentary bodies deposited at those timeses_ES
dc.identifier.urihttp://hdl.handle.net/10272/14013
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherExtensional tectonicses_ES
dc.subject.otherHalokineticses_ES
dc.subject.otherGrowth faultses_ES
dc.subject.otherBasco-Cantabrian basines_ES
dc.titleTectónica distensiva y halocinesis en el margen SO de la cuenca Vasco- Cantábricaes_ES
dc.titleExtensíonal tectonics and halokinetics in the SW margin of the Basco-Cantabrian basineng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)