Análisis secuencial y correlación de los abanicos aluviales de Peña Oroel y la Sierra de Cancias. (Eoceno superior. Cuenca Surpirenaica Central)

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dc.contributor.authorMontes Santiago, M. J.
dc.contributor.authorColombo Piñol, Ferrán
dc.date.accessioned2015-10-16T11:24:51Z
dc.date.available2015-10-16T11:24:51Z
dc.date.issued1996
dc.description.abstractIn the Cuarga Syndfne (jaca Basin), the Sierra de Cancias conglomerates, has been placed traditionally In a lower stratigraphic position than Peña Oroel conglomerates. However; a detai/led geological mapi, based in the systematic line-drawing of the photogeological layer beds, show a similar depositional architecture and a good correlationship between both outcropsen_US
dc.identifier.urihttp://hdl.handle.net/10272/11219
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.otherRegional geologyen_US
dc.subject.otherSequential analysisen_US
dc.subject.otherUpper Eoceneen_US
dc.subject.otherJaca Basinen_US
dc.subject.otherPyreneesen_US
dc.titleAnálisis secuencial y correlación de los abanicos aluviales de Peña Oroel y la Sierra de Cancias. (Eoceno superior. Cuenca Surpirenaica Central)en_US
dc.titleSequential analysis and stratigraphic relationship of Peña Oroel and Sierra de Cancias aluvial fans. (Upper Eocene. South-Pyrenean Central Basin)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-1, (1996)