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Structure of the Campo de Dalías from gravimetric and seismic data

dc.contributor.authorMarín Lechado, Carlos
dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorRodríguez Fernández, L. R.
dc.contributor.authorPedrera Parias, Antonio
dc.date.accessioned2014-09-17T12:28:37Z
dc.date.available2014-09-17T12:28:37Z
dc.date.issued2004
dc.identifier.urihttp://hdl.handle.net/10272/8804
dc.description.abstractThe analysis of new gravity data and multichannel seismic profiles of the Campo de Dalías give new insight about the main features of the deep structure. The progressive development since the Tortonian of folds determine the location of a large ENE-WSW elongated depocentre in a synform located at the central area, bordered by two antiforms situated respectively southwards, near the coast line, and northwards, in the Sierra de Gádor. Folding increase at depth and minor folds are also recognised in the limbs of the major folds. The faults in the region have relatively short slips and most of them have not clear expression in the geophysical dataen_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.otherCampo de Dalíasen_US
dc.subject.otherBetic Cordillerasen_US
dc.subject.otherGravimetryen_US
dc.subject.otherSeismic reflection onshore profilesen_US
dc.subject.otherGrowth foldsen_US
dc.titleEstructura del Campo de Dalías a partir de datos gravimétricos y sísmicosen_US
dc.titleStructure of the Campo de Dalías from gravimetric and seismic dataeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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