Pliegues limitados por fallas en el subbético medio (sector de torre cardela, Granada)

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dc.contributor.authorSanz de Galdeano, Carlos
dc.date.accessioned2014-10-29T11:07:04Z
dc.date.available2014-10-29T11:07:04Z
dc.date.issued2003
dc.description.abstractIn the area of Torre Cardela, situated to the NE of Granada, there are NE-SW to NNE-SSW folds comprised among ENE-WSW dextral strike-slip fauts. The formation of all these structures are interpreted as singenetic, within a compressional elipsoid which o1 varies from WNW-ESE to NW-SE direction. These structures form part of the zone of deformations produced by the Cadiz-Alicante strike-slip faultsen_US
dc.identifier.urihttp://hdl.handle.net/10272/9012
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.otherFaultsen_US
dc.subject.otherFoldsen_US
dc.subject.otherTranspressionen_US
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherSubbeticen_US
dc.titlePliegues limitados por fallas en el subbético medio (sector de torre cardela, Granada)en_US
dc.titleFolds comprised among faults in the Median Subbetic (Torre Cardela sector, Granada, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 35, (2003)