Implicaciones geológicas de la presencia de mármoles con escapolita en el Sinclinorio de Vizcaya
We report by the first time the finding of scapolite-bearing marbles in the Southern limb of the Biscay Synclinorium (Basque-Cantabrian basin). Marbles are found as layers or fragments in Triassic evaporites. I. Evaporitic rocks an antiform cut acrossby crop out in transversal faults. The presence o...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1997 |
| 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:10272/10562 |
| Acceso en línea: | http://hdl.handle.net/10272/10562 |
| Access Level: | acceso abierto |
| Palabra clave: | Marbles Biscay Synclinorium North Pyrenean Fault |
| Sumario: | We report by the first time the finding of scapolite-bearing marbles in the Southern limb of the Biscay Synclinorium (Basque-Cantabrian basin). Marbles are found as layers or fragments in Triassic evaporites. I. Evaporitic rocks an antiform cut acrossby crop out in transversal faults. The presence of such marbles lead us to propose a new location for the prolongation of the North Pyrenean Fault in western sectors of the Basque-Cantabrian bassin |
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