Interpretación de la estructura de la zona NE de la cuenca de Madrid mediante datos gravimétricos

dc.contributor.author	Bergamín, J. F.
dc.contributor.author	Tejero, R.
dc.date.accessioned	2010-01-22T13:22:19Z
dc.date.available	2010-01-22T13:22:19Z
dc.date.issued	1994
dc.identifier.citation	Cadernos do Laboratorio Xeolóxico de Laxe, 1994, 19: 215-227 ISSN: 0213-4497	es_ES
dc.identifier.issn	0213-4497
dc.identifier.uri	http://hdl.handle.net/2183/6168
dc.description.abstract	[Abstract] Modelling of five profiles in the NE area of Madrid Basin shows that low anomalies are related to both the thicker sediments infill of the Basin and the basement rocks like gneiss and granites. The highs are related to thick sequences ofalternating slates and quarzites, outcropping or underlaying a thin cover. The main gradients are related to the marginal faults of the Basin. The existence of a granitic body and a NE-SW striking fault, was also detected. Out of the data obtained in the models, an isobaths map has been depicted of Madrid Basin which shows a fault bounded structure.
dc.language.iso	spa	es_ES
dc.publisher	Universidade da Coruña	es_ES
dc.subject	Madrid Basin	es_ES
dc.subject	Gravity modelling	es_ES
dc.subject	Structure	es_ES
dc.title	Interpretación de la estructura de la zona NE de la cuenca de Madrid mediante datos gravimétricos	es_ES
dc.title.alternative	Structure of Madrid basin (NE zone) derived from gravity data
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.access	info:eu-repo/semantics/openAccess