2026-06-28T20:09:29Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/645622024-07-18T14:14:11Zcom_20.500.14352_14col_20.500.14352_15

Datos sobre los materiales del Cretáceo Terminal-Eoceno del sector del Alto Segura (Zona prebética occidental) Martínez Gallego, J. Dabrio González, Cristino José 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. 2023-06-21T02:00:41Z 2023-06-21T02:00:41Z 2023-06-21T02:00:41Z 1971 journal article https://hdl.handle.net/20.500.14352/64562 0366-600X spa open access Granada: Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias