Control tectónico de las características sedimentológicas del sistema aluvial de Cobatillas (Provincia de Teruel)
The Cobatillas alluvia/ system consists of two short superposed fans. The upper one shows wet fan facies within a semiarid climatic context. This is due both to the sediment source size, which is situated at the back of the obligue ramp of the Muela de Montalbán thrust sheet, and to the basin southe...
| 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:10272/18041 |
| Acceso en línea: | http://hdl.handle.net/10272/18041 |
| Access Level: | acceso abierto |
| Palabra clave: | Alluvial fan Thrust sheet Tectonic-sedimentation relationship Tertiary Iberian Range |
| Sumario: | The Cobatillas alluvia/ system consists of two short superposed fans. The upper one shows wet fan facies within a semiarid climatic context. This is due both to the sediment source size, which is situated at the back of the obligue ramp of the Muela de Montalbán thrust sheet, and to the basin southern margin subsidence originated by the thrust in such margin |
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