Crisis tectónicas cuaternarias en la cuenca de Madrid

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dc.contributor.authorGiner Robles, J. L.
dc.contributor.authorVicente, Gerardo de
dc.contributor.authorPérez González, Alfredo
dc.contributor.authorSánchez Cabañero, J. G.
dc.contributor.authorPinilla, L.
dc.date.accessioned2016-06-29T12:11:24Z
dc.date.available2016-06-29T12:11:24Z
dc.date.issued1996
dc.description.abstractQuaternary sediment deformation structures of Madrid Basin have been analyzed. We get a high symmetry degree in deduced stress tensor trends, concluding that there are a regional stress field with NW-SE Shmax trend. Local stress field (NE-SW) is also deduced. This deformational process has been active since Middle-Upper Miocene, and it is still active as can be seen from seismological data. Largest deformation structures occur in the centre of the basin, where gypsum outcrops appear. It seems that halokynetics processes potentiated this tectonic deformation. Analyzed areas and ages of deformed quaternary sediments, leads us to the conclusion that intense faulting occured in Lower-Middle Pleistocene. Related paleoseismic structures appearen_US
dc.identifier.urihttp://hdl.handle.net/10272/12439
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.otherNeotectonicsen_US
dc.subject.otherFault populational analysisen_US
dc.subject.otherPaleoseismicityen_US
dc.subject.otherQuaternaryen_US
dc.titleCrisis tectónicas cuaternarias en la cuenca de Madriden_US
dc.titleMadrid basin Quaternary tectonic crisiseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)