Correlación de alta resolución del Campaniense-Maastrichtiense, Pirineos sud-centrales
A regressive succesion ot deltaic, shoreface, and continental strata characterized the deposition during the Campanian-Maatrichtian time in the foreland basin of the south-central Pyrenees. This work introduces a high-resolution stratigraphic framework among these strata along the different structur...
| Autores: | , , , |
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| Formato: | artículo |
| Fecha de publicación: | 2001 |
| País: | España |
| Recursos: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/56762 |
| Acesso em linha: | https://hdl.handle.net/20.500.14352/56762 |
| Access Level: | acceso abierto |
| Palavra-chave: | 56:551.7 Bioestratigraphy Rudist Campanian Maastrichtian Pyrenees Geología estratigráfica 2506.19 Estratigrafía |
| Resumo: | A regressive succesion ot deltaic, shoreface, and continental strata characterized the deposition during the Campanian-Maatrichtian time in the foreland basin of the south-central Pyrenees. This work introduces a high-resolution stratigraphic framework among these strata along the different structural sectors of the eastern part of the basin. The framework is based on the reocgnition and section. These horizons, named after their most characterisitc species, have been correlated with planctonic foraminifera biozones following a shelf-to-basin stratigraphic cross-section. We conclude that these rudist horizons are valid as biostratigraphic markers. |
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