Aspectos paleogeográficos del «Keuper» en el borde SW. de la Rama Castellana de la Cordillera Ibérica.

Abstract

The Keuper materials in this region show some facial anomalies. Its study helps to establish some paleogeographical elements during the Upper Triassic; it was placed in the internal border of a «lagoon» where most of the sediments were deposited.