2024-03-29T00:26:40Zhttp://buleria.unileon.es/oai/requestoai:buleria.unileon.es:10612/96852020-12-10T09:10:48Zcom_10612_17col_10612_21
Facultad de Ciencias Biologicas y Ambientales
Rodríguez, Sergio
Fernández Martínez, Esperanza
Cózar, Pedro
Valenzuela Ríos, José Ignacio
Liao, Jau Chyn
Pardo Alonso, Miguel V.
May, Andreas
Paleontologia
2007
2019-03-11T21:57:07Z
2019-03-11T21:57:07Z
2019-03-11
X Internacional Congress on Fossil Cnidaria and Porifera, 12-16 de agosto, 2007, San Petersburgo (Rusia)
http://hdl.handle.net/10612/9685
The Devonian succession between the Guadiana and Guadalquivir Valleys in the Obejo-Valsequillo Domain comprises more than 600 m of shale and sandstone with some interbedded limestone and marl. The most complete sequences are located in the Guadámez-2, Arroyo del Lobo, Zújar, Peñón Cortado and Arroyo del Pozo del Rincón sections. Pragian reefal facies occur at most of these localities but Emsian reefs are well developed only in the Guadámez-2 section.
eng
Paleontología
Arrecifes
Guadalquivir (España, Cuenca)
Guadiana (Cuenca)
Devónico
Devonian
Obejo
Valsequillo
Estratigrafía
Sedimentos (Geología)
Guadámez-2
Arroyo del Lobo
Zújar
Peñón Cortado
Arroyo del Pozo del Rincón
Emsian
Emsian reefal development in Ossa-Morena Zone (SW Spain): Stratigraphic succession, microfacies, fauna and depositional environment
info:eu-repo/semantics/conferenceObject
info:eu-repo/semantics/lecture