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
The 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 i...
| Autor: | |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/12672 |
| Acceso en línea: | http://hdl.handle.net/10272/12672 |
| Access Level: | acceso abierto |
| Palabra clave: | Balanced cross-section Decollement Fault related folding Imbricated fan Shortening |
| Sumario: | The 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 displacements |
|---|