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El abanico imbricado de Valverde del Camino (parte meridional de la Zona Sudportuguesa, Huelva)
The imbricate fan of Valverde del Camino (southern part of the South Portuguese Zone, Huelva)
| dc.contributor.author | Mantero Cuajares, Macarena | |
| dc.contributor.author | Alonso Chaves, Francisco Manuel | |
| dc.contributor.author | Azor, A. | |
| dc.date.accessioned | 2014-10-30T12:12:41Z | |
| dc.date.available | 2014-10-30T12:12:41Z | |
| dc.date.issued | 2003 | |
| dc.identifier.uri | http://hdl.handle.net/10272/9039 | |
| dc.description.abstract | The South Portuguese Zone is a foreland affected by a thin-skinned tectonics characterized by SSW-vergent thrust-and-folds developed in Carboniferous times as a consequence of the Variscan collision. In the Valverde del Camino area, detailed mapping and structural analysis show the existence of a fault-propagation antiform related to an imbricate fan with SSW sense of movement. The thrusts of this imbricate fan merge at depth with a detachment located in the middle crust. The total displacement produced by the imbricate fan is very scarce, most of the shortening being probably accommodated by folding and cleavage development | en_US |
| dc.language.iso | spa | en_US |
| dc.publisher | Sociedad Geológica de España | en_US |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
| dc.subject.other | Thrust system | en_US |
| dc.subject.other | Imbricate fan | en_US |
| dc.subject.other | Inclined folds | en_US |
| dc.subject.other | South Portuguese Zone | en_US |
| dc.title | El abanico imbricado de Valverde del Camino (parte meridional de la Zona Sudportuguesa, Huelva) | en_US |
| dc.title | The imbricate fan of Valverde del Camino (southern part of the South Portuguese Zone, Huelva) | eng |
| dc.type | info:eu-repo/semantics/article | en_US |
| dc.rights.accessRights | info:eu-repo/semantics/openAccess | en_US |
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