Estructuración y significado tectonoestratigráfico de la formación calizas de panda (moscoviense superior, zona cantábrica)
The Panda Limestone Formation (upper Podolsky to Podolsky-Myachkovsky boundary, Pisuerga-Carrión Province, Cantabrian Zone) forms part of the Pando Group, the syn-orogenic wedge related to the emplacement of the Esla Unit. The formation has been divided into three informal members. Fades analysis su...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2002 |
| 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:10272/9313 |
| Acceso en línea: | http://hdl.handle.net/10272/9313 |
| Access Level: | acceso abierto |
| Palabra clave: | Cantabrian Zone Pisuerga-Carrión Province Carboniferous Moscovian Foreland Basin Mud Mounds |
| Sumario: | The Panda Limestone Formation (upper Podolsky to Podolsky-Myachkovsky boundary, Pisuerga-Carrión Province, Cantabrian Zone) forms part of the Pando Group, the syn-orogenic wedge related to the emplacement of the Esla Unit. The formation has been divided into three informal members. Fades analysis suggests that the Panda limestones were deposited in a ramp-like platform, in which subtidal carbonate platform (lower or Cosoya member) and deep platform with mud mounds (upper or Valcarque member) settings can be recognised. Locally, a destructive slope (Casasuertes breccia member) developed. The Panda Formation and the upper part of the underlying Vega cerneja Formation form a depositional sequence recording a deepening upward trend. Also, the platform seems to have developed on an E-W trending arc, which is thought to be due to a blind thrust related to the Esla Unit emplacement |
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