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

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dc.contributor.authorMuñoz Martín, Alfonso
dc.contributor.authorVicente Muñoz, Gerardo De
dc.contributor.authorGonzález Casado, José Manuel
dc.date.accessioned2023-06-20T17:25:11Z
dc.date.available2023-06-20T17:25:11Z
dc.date.issued1994
dc.description.abstractAn analysis of Neogene brittle deformation using fault population 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.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/7949
dc.identifier.doi7949
dc.identifier.issn0213-4497
dc.identifier.officialurlhttp://www.iux.es/index.php?page=5&serie=1
dc.identifier.urihttps://hdl.handle.net/20.500.14352/58219
dc.journal.titleCadernos do Laboratorio Xeolóxico de Laxe
dc.language.isospa
dc.page.final214
dc.page.initial203
dc.rights.accessRightsopen access
dc.subject.keywordAltomira Range
dc.subject.keywordNeogene
dc.subject.keywordBrittle deformation
dc.subject.keywordFault population analysis
dc.subject.keywordStress tensor
dc.subject.keywordPaleostress field
dc.subject.ucmGeodinámica
dc.subject.unesco2507 Geofísica
dc.titleAnálisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de Madrid
dc.typejournal article
dc.volume.number19
dspace.entity.typePublication
relation.isAuthorOfPublication70f369a3-b3cd-43cb-874e-a7888da25de1
relation.isAuthorOfPublication09af5f8f-e65c-4c2b-8583-c1c43e152589
relation.isAuthorOfPublication.latestForDiscovery70f369a3-b3cd-43cb-874e-a7888da25de1

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