Estructura profunda de la cuenca de Cameros (Cordillera Ibérica) a partir de datos gravimétricos

dc.contributor.author	Rivero, Luis
dc.contributor.author	Guimerà, J.
dc.contributor.author	Casas Sainz, Antonio
dc.date.accessioned	2017-01-26T09:58:35Z
dc.date.available	2017-01-26T09:58:35Z
dc.date.issued	1996
dc.description.abstract	The Cameros basin (Iberian Chain) developed under a very subsident extensional regime during the latest Jurassic-early Cretaceous. Its fill constitutes a magasequence o f more than 5000 m of vertical thickness. That would produce a gravity low. Nevertheless, the gravity map of this area draws a gravity high in the eastern part of the basin. We propose an explanation to this contradiction	en_US
dc.identifier.uri	http://hdl.handle.net/10272/13196
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.accessRights	open access	en_US
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Gravity data	en_US
dc.subject.other	Iberian range	en_US
dc.subject.other	Cameros basin	en_US
dc.title	Estructura profunda de la cuenca de Cameros (Cordillera Ibérica) a partir de datos gravimétricos	en_US
dc.title	Deep structure of thè Cameros basin (Iberian Chain) from gravity data	eng
dc.type	journal article	en_US
dspace.entity.type	Publication

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