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Iberian range Alpine dextral slip quantification from gravity data

dc.contributor.authorBergamín, J. F.
dc.contributor.authorVicente, Gerardo de
dc.contributor.authorTejero López, Rosa
dc.contributor.authorGómez, D.
dc.contributor.authorMuñoz Martín, Alfonso
dc.contributor.authorPerucha, M. A.
dc.date.accessioned2016-06-30T09:17:16Z
dc.date.available2016-06-30T09:17:16Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12447
dc.description.abstractIntraplate deformation in the eastern zone of the Iberian Peninsula is characterized by strike-slip faulting during Tertiary. Gradient pattern of Bouguer Anomaly Map of the Spanish Central SystemIberian Range linking zone are related to main crustal faults. Gradients pattern has been analysed by means of a raster type Geographic Information System. Two main gradien orientations associated with Spanish Central System structures (NE-SW) and with Iberian Range structures (NW-SE) have been established. Gradient map and artificial shading image have been used to quantify dextral slip along NOSE faults. Slip value reach a figure of 34 km. Assuming that the slip began in Oligocene times, movement rate between the Spanish Central System and the Iberian Range Castilian Branch is 0.93 mm/y. Considering a Middle Miocene start a 2.2 mm/y slip rate is computeden_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherIberian Rangeen_US
dc.subject.otherBouguer anomaly Mapen_US
dc.subject.otherDextral slipen_US
dc.titleCuantificación del desplazamiento dextroso Alpino en la cordillera Ibérica a partir de datos gravimétricosen_US
dc.titleIberian range Alpine dextral slip quantification from gravity dataeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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