Intercalación de un sistema turbidítico siliciclástico entre carbonatos de plataforma: implicaciones tectónicas (Aptiense-Albiense, cabo Ogoño, Bizkaia)
A turbidite (channel-levee) siliciclastic system replaced vertically a mixed carbonate and terrigenous platform, and it in turn was replaced by litoral sandstones and bank carbonates (Aptian-Albian, Ogoño, Bizkaia). An E-W composite stratigraphical section shows that an inversion in subsidence tool&...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1991 |
| 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:10272/18068 |
| Acceso en línea: | http://hdl.handle.net/10272/18068 |
| Access Level: | acceso abierto |
| Palabra clave: | Siliciclastic turbidites Platform carbonates Paleo-fault |
| Sumario: | A turbidite (channel-levee) siliciclastic system replaced vertically a mixed carbonate and terrigenous platform, and it in turn was replaced by litoral sandstones and bank carbonates (Aptian-Albian, Ogoño, Bizkaia). An E-W composite stratigraphical section shows that an inversion in subsidence tool< place approximate/y around the Ibarrangelua N-S paleogeographic line during the process. Therefore, the action ofa deep-seated, probab/y wrench fau/t is invoked to account for the origin ofthe turbidite system in this unusual context |
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