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Palaeostress reconstruction in the foreland basins of the northwestern part of gibraltar arc (upper miocene to the present)

dc.contributor.authorCamacho Cerro, Manuel Alejandro 
dc.contributor.authorGarcía Navarro, Encarnación 
dc.contributor.authorFernández Rodríguez, Carlos 
dc.contributor.authorAlonso Chaves, Francisco Manuel
dc.description.abstractGraphical and numerical methods of fault slip data inversion have been applied to obtain palaeostress reconstructions in Neogene and Quaternary basins, located in the northwestern part of Gibraltar Arc. The most important brittle structures affecting these sediments are high-angle faults with oblique-slip. Two sets of faults with NW-SE and NE-5W trends have been distinguished. The trend of the major axis of the palaeostress ellipse in the horizontal plane has rotated from E-W in the Upper Miocene to NW-SE in the Pliocene-Quaternaryen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherFaulting analysisen_US
dc.subject.otherAlpine Tectonicen_US
dc.subject.otherGibralltar Arcen_US
dc.titlePaleoesfuerzos en las cuencas de antepaís en la parte noroccidental del arco de gibraltar (mioceno superior-actualidad)en_US
dc.titlePalaeostress reconstruction in the foreland basins of the northwestern part of gibraltar arc (upper miocene to the present)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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