Litoestratigrafía del Jurásico de Gipuzkoa y NW de Navarra
Lithostratigraphic correlation of numerous sequences leads to the reconstruction of the mesoscale depositional geometries of the Jurassic succession of the eastern part of the Basque-Cantabrian Basin (Gipuzkoa and Navarra provinces). In all studied sections, the Lias shows similar thickness and limi...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1991 |
| 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:10272/18072 |
| Acesso em linha: | http://hdl.handle.net/10272/18072 |
| Access Level: | acceso abierto |
| Palavra-chave: | Diferential subsidence Tectonic control Swells and troughs Jurassic Gipuzkoa and Navarra |
| Resumo: | Lithostratigraphic correlation of numerous sequences leads to the reconstruction of the mesoscale depositional geometries of the Jurassic succession of the eastern part of the Basque-Cantabrian Basin (Gipuzkoa and Navarra provinces). In all studied sections, the Lias shows similar thickness and limited facies changes; the Dogger-Malm succession reveals the initial development of swells and troughs triggered by differential subsidence, and a significant facies changes; both of these features are even more marked on the latest Jurassic-Neocomian succession. lt is concluded, therefore, that the Jurassic evolution of the area was controlled by tectonics of increasing intensity, in addition to eustatism |
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