Nuevos datos y modelo genético sobre brechas jurásicas generadas en relación con fallas transcurrentes (Subbético Externo. Provincia de Córdoba)
In the External Subbetic, Upper Jurassic coarse breccias organized in lenticular sedimentary bodies prograding to the west, are genetically relationed to N-S transcurrent faults affecting to the basin to the end of the Middle Jurassic. The breccias were probably deposited over a sunken block displac...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1989 |
| 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:10272/18256 |
| Acesso em linha: | http://hdl.handle.net/10272/18256 |
| Access Level: | acceso abierto |
| Palavra-chave: | Breccias Listric faults Transcurrent faults Upper Jurassic External Subbetic |
| Resumo: | In the External Subbetic, Upper Jurassic coarse breccias organized in lenticular sedimentary bodies prograding to the west, are genetically relationed to N-S transcurrent faults affecting to the basin to the end of the Middle Jurassic. The breccias were probably deposited over a sunken block displaced to the north in respect of the northern palaeogeographic units, which stratigraphic series made up a main source area. The sunken block was probably emerged during the Late Liassic and Middle Jurassic, so that the breccias are underlied by the Lower Liassic Gavilan Fm |
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