Estructuras bioturbadas de las facies Muschelkalk de la Zona Subbética
In Majanillos Formation (middle -upper Ladinian age) of the Subbetic Zone, the bioturbate textures are related with deep ramp facies. F/ieTlialassinoides trace fossil is placed in the middle levels of the formation corresponding to lagoon facies (low energy). And the Diplocaaterion, Rhizocorallium a...
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1992 |
| 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:10272/16338 |
| Acceso en línea: | http://hdl.handle.net/10272/16338 |
| Access Level: | acceso abierto |
| Palabra clave: | Triassic Muschelkalk Subbetic Trace fossil |
| Sumario: | In Majanillos Formation (middle -upper Ladinian age) of the Subbetic Zone, the bioturbate textures are related with deep ramp facies. F/ieTlialassinoides trace fossil is placed in the middle levels of the formation corresponding to lagoon facies (low energy). And the Diplocaaterion, Rhizocorallium and Chondrites trace fossils are related with the shallower facies of a restricted stone |
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