Tectónica distensiva y halocinesis en el margen SO de la cuenca Vasco- Cantábrica
Extensional tectonics and associated halokinetics processes controlled the sedimentation in the southwestern margin of the Basco-Cantabrian basin during Upper Jurassic and Lower Cretaceous times. The development of Mesozoic growth faults, compressive features at present, controlled the geometry and...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1994 |
| 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:10272/14013 |
| Acceso en línea: | http://hdl.handle.net/10272/14013 |
| Access Level: | acceso abierto |
| Palabra clave: | Extensional tectonics Halokinetics Growth faults Basco-Cantabrian basin |
| Sumario: | Extensional tectonics and associated halokinetics processes controlled the sedimentation in the southwestern margin of the Basco-Cantabrian basin during Upper Jurassic and Lower Cretaceous times. The development of Mesozoic growth faults, compressive features at present, controlled the geometry and limits of the sedimentary bodies deposited at those times |
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