Un sistema de paleoalto carbonatado-surco siliciclástico (Gorbea-Artzentales, Albiense medio, Bizkaia)
During the middle Albian, fault block synsedimentary activity induced the formation of a paleohigh (Corbea) and an adjacent sedimentary trough, While (he high was exposed in the subaerial meteoric environment realm, the trough was filled by athick wedge up to 2 km of deeper water siliciclastics
| Autores: | , , , |
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| Formato: | artículo |
| Fecha de publicación: | 1994 |
| 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:10272/13970 |
| Acesso em linha: | http://hdl.handle.net/10272/13970 |
| Access Level: | acceso abierto |
| Palavra-chave: | Albian Carbonate platform Paleokarst Sillciclastic trough Sinsedimentary faults |
| Resumo: | During the middle Albian, fault block synsedimentary activity induced the formation of a paleohigh (Corbea) and an adjacent sedimentary trough, While (he high was exposed in the subaerial meteoric environment realm, the trough was filled by athick wedge up to 2 km of deeper water siliciclastics |
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