Consideraciones sobre la edad del techo de las calizas oolíticas del Jurásico medio del Subbético Interno oriental (Cordilleras Béticas)

Abstract

Oolitic limestones crop extensively out in the External Zones of the Betic Cordilleras, currently being considered Dogger in age througt indirect criteria (mainly the age of the underlying and overlying units). In this paper the calcareous nannofossil assemblages from some outcrops north of Vêlez Blanco have been studied, and they restrict the age of the top of the oolitic limestones to the early to mid Bathonian interval