Las facies Keuper al SW de la provincia de Soria

E. Aracil; S. Hernando

doi:10.3989/egeol.88443-4539

Las facies Keuper al SW de la provincia de Soria

Authors

E. Aracil Instituto de Geología Económica. C.S.I.C. Departamento de Estratigrafía. Facultad de Ciencias Geológicas. Universidad Complutense de Madrid
S. Hernando Departamento de Estratigrafía. Facultad de Ciencias Geológicas. Universidad Complutense de Madrid

DOI:

https://doi.org/10.3989/egeol.88443-4539

Keywords:

Triassic, Keuper, Soria, Alluvial fan, sabkha

Abstract

This paper deals with the sedimentological analysis of the materials that correspond to the Keuper facies in the area situated between the Iberian Ranges and the Central System. Acording to the obtained data, two main aspects are emphasized: - During the Upper Triassic, a c1ear retreat of the roast line towards the East took place, since this area constituted the litoral zone during the sedimentation of the Rot and Muschelkalk. - Facies change lateraly from West to East as proximal alluvial Can sediments pass into facies interpreted as distal alluvial fans and continental sabkha environment.

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Published

1988-08-30

How to Cite

Aracil, E., & Hernando, S. (1988). Las facies Keuper al SW de la provincia de Soria. Estudios Geológicos, 44(3-4), 211–217. https://doi.org/10.3989/egeol.88443-4539

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Issue

Vol. 44 No. 3-4 (1988)

Section

Articles

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