Caracterización bioestratigráfica de la Biozona Transversarium (Oxfordiense medio) en el sector oriental de la Cordillera Ibérica
In NE Iberian Chain (E. Spain), the Transversarium Zone is developed in sponge limestone facies. All the subzones af this biozone have been characterised by means of ammonites. The basal, Parandieri Subzone, is only represented in the northwestern part of the studied area (Ricia). The uppermost, Rot...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1990 |
| 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:10272/18142 |
| Acceso en línea: | http://hdl.handle.net/10272/18142 |
| Access Level: | acceso abierto |
| Palabra clave: | Biostratigraphy Middle Oxfordian Transversarium Zone Iberian Chain Ammonites |
| Sumario: | In NE Iberian Chain (E. Spain), the Transversarium Zone is developed in sponge limestone facies. All the subzones af this biozone have been characterised by means of ammonites. The basal, Parandieri Subzone, is only represented in the northwestern part of the studied area (Ricia). The uppermost, Rotoides Subzone, recently defined, has been recognised in all the localities |
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