Tectónica de cabalgamientos en la Faja Pirítica Ibérica (Zona Sur Portuguesa): el Antiforme de la Puebla de Guzmán, y la lámina de cabalgamiento de Sanlúcar de Guadiana

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dc.contributor.authorSoriano Clemente, C.
dc.date.accessioned2016-09-21T12:26:29Z
dc.date.available2016-09-21T12:26:29Z
dc.date.issued1996
dc.description.abstractThe Sanlucar de Guadiana thrust sheet and the Puebla de Guzmán Antiform in the central Iberian Pyrite Belt are interpreted as alloctonous units displaced to the south, forming part of an imbricated thrust system dipping to the north . Shortening calculations account for the part of bulk shortening involved in macroscopic fault related folds and in fault displacementsen_US
dc.identifier.urihttp://hdl.handle.net/10272/12672
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.otherBalanced cross-sectionen_US
dc.subject.otherDecollementen_US
dc.subject.otherFault related foldingen_US
dc.subject.otherImbricated fanen_US
dc.subject.otherShorteningen_US
dc.titleTectónica de cabalgamientos en la Faja Pirítica Ibérica (Zona Sur Portuguesa): el Antiforme de la Puebla de Guzmán, y la lámina de cabalgamiento de Sanlúcar de Guadianaen_US
dc.titleThrust tectonics in the Iberian Pyrite Belt (South Portuguese Zone): the Puebla de Guzmán Antiform and the Sanlúcar de Guadiana thrust sheeteng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)