Paleoesfuerzos alpinos en el borde suroccidental de la cuenca de Madrid (Montes de Toledo)

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dc.contributor.authorMartín, S.
dc.contributor.authorVicente, Gerardo de
dc.date.accessioned2017-04-04T11:48:47Z
dc.date.available2017-04-04T11:48:47Z
dc.date.issued1995
dc.description.abstractThe paleostress analysis are used here to outline the Alpine deformation of the contact between the Toledo Mountains and the Madrid Basin. This limit results from a system of E-W-trending reverse faults, NW-SE-trending dextral normal strike-slip faults and NNE-SSW-trending sinistral normal strike-slip faultsen_US
dc.identifier.urihttp://hdl.handle.net/10272/13549
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.otherFaults population analysis,en_US
dc.subject.otherPaleostress analysisen_US
dc.subject.otherCuenca de Madrid.en_US
dc.titlePaleoesfuerzos alpinos en el borde suroccidental de la cuenca de Madrid (Montes de Toledo)en_US
dc.titleAlpine paleostress in the South-Western margin of the Madrid basin (Toledo Mountains)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)