Depósitos mareales y de tormenta en la Formación Cuevas Labradas (Jurásico Inferior) al SO de Berlanga de Duero (Soria)
Thee levels have been stablished in the sediments of the Cuevas Labradas Formation (SW of Soria province). These correspond to the tectosedimentary units III, IV and V proposed by Yébenes et al. (1988). Two environments have been recognized: a) A predominant subtidal one, more or less protected, rec...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1989 |
| 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:10272/18236 |
| Acceso en línea: | http://hdl.handle.net/10272/18236 |
| Access Level: | acceso abierto |
| Palabra clave: | Sequences Tidal deposits Storm deposits Lower Jurassic Western Iberian Chain |
| Sumario: | Thee levels have been stablished in the sediments of the Cuevas Labradas Formation (SW of Soria province). These correspond to the tectosedimentary units III, IV and V proposed by Yébenes et al. (1988). Two environments have been recognized: a) A predominant subtidal one, more or less protected, receiving frequent storm deposits. b) Another one affected by important tidal dynamics resulting in oolitic bars with sigmoida/ stratification and herring bone |
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