Las facies terrígenas del Muschelkalk basal en el extremo noroccidental de la Cordillera Ibérica

Abstract

Clastic Materials of basal Muschelkafk in the northestern edge of lberian Ranges represent subtidaf environments and even high energy events in the inner platform (presence of H.C.S.). Such events disturb the ínter and supratidal sedimentation development of both under and overlaying units.