Análisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de Madrid

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dc.contributor.authorMuñoz Martín, A.
dc.contributor.authorVicente Muñoz, G. de
dc.contributor.authorGonzález Casado, J. M.
dc.date.accessioned2010-01-22T13:22:40Z
dc.date.available2010-01-22T13:22:40Z
dc.date.issued1994
dc.description.abstractAn analysis of Neogene brittle deformation using fault populatíon analysis methods has been carried out between the SW border of the Iberian Range and Altomira Range. Two main paleostress fields have been established: 1) N70E - N120E compression (Altomira paleostress field) ofLate Oligocene - Early Miocene age that induced the formation of the SW border of Iberian Range and Altomira - Pareja thrust belts with reverse and strike-slip faults. 2) N140-N160E compression (Guadarrama paleostress field) of Middle Aragonian - early Pleistocene age that reactivated previous faults with strikeslip movement along the Iberian Range. A superposition of two regional stress fields (Iberian and Guadarrama) is proposed to explain E-W compression that formed Altomira Range. Stress tensorial additions have been realized to check this hypothesis.
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1994, 19: 203-214 ISSN: 0213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6181
dc.language.isospaes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.rights.accessRightsopen access
dc.subjectAltomira Rangees_ES
dc.subjectNeogenees_ES
dc.subjectBrittle deformationes_ES
dc.subjectFault population analysises_ES
dc.subjectStress tensores_ES
dc.subjectPaleostress fieldes_ES
dc.titleAnálisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de Madrides_ES
dc.title.alternativeTensorial analisis of the superposed deformation in the easthern border of the Madrid basin
dc.typejournal articlees_ES
dspace.entity.typePublication

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REV - CLXL - Vol. 19 (1994)