Evolución geomorfológica del karst y paleoambientes cuaternarios en el macizo de Patones-Cerro de la Oliva (Madrid)
Geomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitati...
| Autores: | , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2001 |
| 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:10272/9487 |
| Acceso en línea: | http://hdl.handle.net/10272/9487 |
| Access Level: | acceso abierto |
| Palabra clave: | Karst Evolución paleoambiental Cuaternario Sistema Central |
| Sumario: | Geomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitation under favorable climatic conditions during isotopic stages 9-11?, 7, 5, 4-3 and 7, respectively |
|---|