Resultados preliminares en la caracterización geométrica 3D de un litosoma arenoso de progradación deltaica mediante Georadar (GPR) (Fm. Arenisca de Roda, Eoceno, Cuenca de Graus-Tremp).

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RECERCAT Home > Universitat de Barcelona > Dinàmica de la Terra i l'Oceà > Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) > View document

To access the full text documents, please follow this link: http://hdl.handle.net/2445/42029

dc.contributor	Universitat de Barcelona
dc.contributor.author	Coll, M.
dc.contributor.author	López Blanco, Miguel
dc.contributor.author	Marcuello Pascual, Alejandro
dc.date	2007
dc.identifier.citation	0213-683X
dc.identifier.uri	http://hdl.handle.net/2445/42029
dc.format	4 p.
dc.format	application/pdf
dc.language.iso	spa
dc.publisher	Sociedad Geológica de España
dc.relation	Geogaceta, 2007, vol. 41, p. 51-54
dc.rights	(c) Sociedad Geológica de España, 2007
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Prospecció geofísica
dc.subject	Geomagnetisme
dc.subject	Eocè
dc.subject	Geophysical exploration
dc.subject	Geomagnetism
dc.subject	Eocene Epoch
dc.title	Resultados preliminares en la caracterización geométrica 3D de un litosoma arenoso de progradación deltaica mediante Georadar (GPR) (Fm. Arenisca de Roda, Eoceno, Cuenca de Graus-Tremp).
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/publishedVersion
dc.description.abstract	A set of GPR profiles have been recorded in order to determine the 3D geometry of a prograding delta-front sandbody (Roda sandstone formation, Eocene, Graus-Tremp basin). Common Mid Points (CMP) also have been recorded to obtain the velocity of the electromagnetic wave in ground. In order to build the topsurface of a 3D prism a set of topographic points have been acquired. Most of the GPR profiles are oriented parallel to the progradation direction (NNE-SSW) and show the expected geometries. The 3D prism has been built from the individual profiles, which shows the three dimensional geometry of the sandy lithosome.

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