Datos sobre los materiales del Cretáceo Terminal-Eoceno del sector del Alto Segura (Zona prebética occidental)
This paper account for result of a first general view of the materials from the final Cretaceus to the Nummulitic, in the sud-east area of the high Course of the Segura river. The Senonian presents southwards a more open-sea facies character. The Paleocene shows pararecifal facies. The passage from...
| Autores: | , |
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| Tipo de documento: | artigo |
| Data de publicação: | 1971 |
| País: | España |
| Recursos: | Universidad Complutense de Madrid (UCM) |
| Repositório: | Docta Complutense |
| Idioma: | espanhol |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/64562 |
| Acesso em linha: | https://hdl.handle.net/20.500.14352/64562 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Geología estratigráfica 2506.19 Estratigrafía |
| Resumo: | This paper account for result of a first general view of the materials from the final Cretaceus to the Nummulitic, in the sud-east area of the high Course of the Segura river. The Senonian presents southwards a more open-sea facies character. The Paleocene shows pararecifal facies. The passage from Cretaceous to Paleocene is represented by a lithological change or, at least, a change in the deposition conditions, without evidences for the presence of an unconformity. The Eocene has very homogeneous facies belonging to a shallow-water environment. The thickness seems to increase southerly. |
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