Estudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricos

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dc.contributor.authorPerucha Atienza, María Ángeles
dc.contributor.authorMuñoz Martín, Alfonso
dc.contributor.authorTejero López, Rosa
dc.contributor.authorBergamín, J. F.
dc.date.accessioned2017-03-21T13:26:55Z
dc.date.available2017-03-21T13:26:55Z
dc.date.issued1995
dc.description.abstractAn integrated geophysical and geological study has been carried out along a trasverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background model for the gravity modeling. Mesozoic cover structure is characterized by thrusts, E dipping, associated with a decollement located in triassic beds. Gravity modeling shows that high-angle faults bound basement blocks. The faults control triassic sediments thicknessen_US
dc.identifier.urihttp://hdl.handle.net/10272/13489
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.otherMadrid basinen_US
dc.subject.otherAltomira Rangeen_US
dc.subject.otherLoranca basinen_US
dc.subject.otherStructureen_US
dc.subject.otherSeismicen_US
dc.subject.otherGravityen_US
dc.subject.otherForward modelingen_US
dc.titleEstudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricosen_US
dc.titleIntegrated structural, seismic and gravity data study along a trasverse from the Madrid basin to the Iberian Rangeeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)