La Formación Marín: redepósito de material jurásico durante el Mioceno (zona Subbética)
An important volume about resedimented materials during the Burdigalian has been confused with the oolite Dogger even today. This article determines the Marin Formation, litostratigraphic unit that includes these rocks. It will be caracterized by the prevalence of the conglomeratic beds (A facies),...
| Autores: | , , |
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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:10272/18188 |
| Acceso en línea: | http://hdl.handle.net/10272/18188 |
| Access Level: | acceso abierto |
| Palabra clave: | Resedimented materials Burdigalian Subbetic zone |
| Sumario: | An important volume about resedimented materials during the Burdigalian has been confused with the oolite Dogger even today. This article determines the Marin Formation, litostratigraphic unit that includes these rocks. It will be caracterized by the prevalence of the conglomeratic beds (A facies), with planktonic foraminifera in the matrix |
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