Procedencia y evolución diagenética de las areniscas Permo-triásicas de la Cordillera Ibérica (Sierra de Albarracín-Boniches-Talayuelas, provincias de Teruel y Cuenca)

descriptionPublicationkeyboard_double_arrow_right Article 01 Jan 1987 Spain Publisher:Universidad Complutense de Madrid. Departamento de Estratigrafía

Authors: Cruz, Berta de la; Marfil Pérez, Rafaela; Peña, José Andrés de la; Arribas Mocoroa, José;

handle: 20.500.14352/64593 , 10261/5814

Procedencia y evolución diagenética de las areniscas Permo-triásicas de la Cordillera Ibérica (Sierra de Albarracín-Boniches-Talayuelas, provincias de Teruel y Cuenca)

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Abstract

[ES] Las series detríticas rojas atribuidas al Permo-Triásico en esta zona de la Cordillera Ibérica comprenden una potente sedimentación terrígena depositada en ambiente fundamentalmente fluvial, controlada por la tectónica que, según ALVARO et al. (1982>, representa las primeras etapas de relleno de cuencas de tipo semigraben del aulacógeno celtibérico.

[EN] The Permo-Triassic detrital red beds located on this zone of the Iberian Range comprise a huge terrigenous sedimentation, deposited under a dominating fluvial environment. The deposits are tectonically controlled and, according to ALVARO et al. (1982), they represent the early filling stages of a semigraben basin within the celtiberian aulacogen.

Peer reviewed

Country

Spain

Related Organizations

Complutense University of Madrid
Spain

Keywords

Cordillera Ibérica, Permo-Triásico, Arenisca, Diagénesis, Petrología, Areniscas, 552.5(234.1), Triásico

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