Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica
Detrital platform sedimentation during the Devonian times took place in the homogeneous basin of the Iberian Pyrite Belt. This shallow basin changed to a mosaic of horsts and grabens just in the Devonian-Carboniferous boundary. Thick mattrix supported conglomerates (mega-debris flow) appear related...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1994 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13792 |
| Acesso em linha: | http://hdl.handle.net/10272/13792 |
| Access Level: | acceso abierto |
| Palavra-chave: | Devonian Mega-debris flow Iberian Pyrite Belt |
| Resumo: | Detrital platform sedimentation during the Devonian times took place in the homogeneous basin of the Iberian Pyrite Belt. This shallow basin changed to a mosaic of horsts and grabens just in the Devonian-Carboniferous boundary. Thick mattrix supported conglomerates (mega-debris flow) appear related with this dynamic. They suggest convulsive seismic events related to the Breton phase of the Hercynian orogeny |
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