Presencia de la discontinuidad sárdica en la Zona Cantábrica
The «sardic unconformity» (near the Cambrian-Ordovician boundary), ocurring in the middle part of the Armorican Quartzite-Barrios Fm., is for the first time reported in the Cantabrian Zone. A close comparison with the Cambro-Ordovician successions in other regions is then possible, having important...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1988 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18383 |
| Acesso em linha: | http://hdl.handle.net/10272/18383 |
| Access Level: | acceso abierto |
| Palavra-chave: | Cambrian Ordovician Sardic unconformity Armorican Quartzite Cantabrian Zone |
| Resumo: | The «sardic unconformity» (near the Cambrian-Ordovician boundary), ocurring in the middle part of the Armorican Quartzite-Barrios Fm., is for the first time reported in the Cantabrian Zone. A close comparison with the Cambro-Ordovician successions in other regions is then possible, having important tecto-sedimentary conclusions |
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