La Caliza de Peña Redonda (Westfaliense A-B): Evolución tecto-sedimentaria (Cuenca Carbonífera Central asturiana)
The occurrence of destructive carbonatic facies at the top of a tectonically controlled megasequence and his probable widespread distribution may be an indicator of an extensive emersion during Westfalian A-B boundary, and could hide important changes in the local fossil distribution
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1990 |
| 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:10272/18117 |
| Acceso en línea: | http://hdl.handle.net/10272/18117 |
| Access Level: | acceso abierto |
| Palabra clave: | Carbonatic facies Westfalian Asturian Central Basin |
| Sumario: | The occurrence of destructive carbonatic facies at the top of a tectonically controlled megasequence and his probable widespread distribution may be an indicator of an extensive emersion during Westfalian A-B boundary, and could hide important changes in the local fossil distribution |
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