Implicaciones geológicas de la presencia de mármoles con escapolita en el Sinclinorio de Vizcaya

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dc.contributor.authorCuevas, Julia
dc.contributor.authorAranguren, A.
dc.contributor.authorBadillo, J. M.
dc.contributor.authorTubía, José María
dc.date.accessioned2015-05-11T12:29:39Z
dc.date.available2015-05-11T12:29:39Z
dc.date.issued1997
dc.description.abstractWe report by the first time the finding of scapolite-bearing marbles in the Southern limb of the Biscay Synclinorium (Basque-Cantabrian basin). Marbles are found as layers or fragments in Triassic evaporites. I. Evaporitic rocks an antiform cut acrossby crop out in transversal faults. The presence of such marbles lead us to propose a new location for the prolongation of the North Pyrenean Fault in western sectors of the Basque-Cantabrian bassinen_US
dc.identifier.urihttp://hdl.handle.net/10272/10562
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.otherMarblesen_US
dc.subject.otherBiscay Synclinoriumen_US
dc.subject.otherNorth Pyrenean Faulten_US
dc.titleImplicaciones geológicas de la presencia de mármoles con escapolita en el Sinclinorio de Vizcayaen_US
dc.titleGeological implications of scapolite-bearing marbles in the Biscay Synclinoriumeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 22, (1997)