Asociaciones de facies en los f an deltas de las cuencas neógenas y cuaternarias de las Cordilleras Béticas Orientales

Abstract

Fan deltas occur in a wide range of tectonic and sedimentary settings which are like/y to generate a varied mosaic of facies associations. Fan delta deposits provide a good geodynamic record of basins as illustrated by examples in sorne Late Neogene basins of the Betic Cordillera (S.f. Spain) which are described in ascending arder of subsidence.