Cinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)

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dc.contributor.authorRodríguez Pascua, M.A.
dc.contributor.authorVicente Muñoz, Gerardo de
dc.contributor.authorGonzález Casado, J.M.
dc.date.accessioned2023-06-20T20:13:28Z
dc.date.available2023-06-20T20:13:28Z
dc.date.issued1994
dc.description.abstractThe geological macrostructure of Alto Tajo is defined by several N1500E dextral strike-slip faults with related secundary structures. The former set of faults together with others N-S sinistral strike-slip faults delimited areas in transtension and transpession. Four tectonic phases have been detected by means of microstructural analysis: N600E compression; N1500E compression (the main deformation phase). N-S compression, without important structures asociated and a last episode of radial extension.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedFALSE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/35725
dc.identifier.issn0213-4497
dc.identifier.officialurlhttp://www.iux.es/?page=5&serie=1
dc.identifier.urihttps://hdl.handle.net/20.500.14352/59881
dc.journal.titleCuadernos do Laboratorio Xeolóxico de Laxe
dc.language.isospa
dc.page.final174
dc.page.initial163
dc.publisherSeminario de Estudos Galegos. Area de Xeoloxía e Minería ; Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
dc.rights.accessRightsopen access
dc.subject.cdu551.24(460.281)
dc.subject.cdu(460.281)551.24
dc.subject.keywordFallas (Geología)
dc.subject.keywordEspaña-Guadalajara
dc.subject.keywordStrike-slip
dc.subject.keywordFaults
dc.subject.keywordFlower structures
dc.subject.keywordFault population analysis
dc.subject.keywordCataclastic rocks
dc.subject.keywordTertiary basin of Zaorejas
dc.subject.ucmGeodinámica
dc.subject.unesco2507 Geofísica
dc.titleCinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)
dc.title.alternativeKinematic and dynamic array of the alpine deformations in alto Tajo are a (Guadalajara)
dc.typejournal article
dc.volume.number19
dspace.entity.typePublication
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