Condicionantes estructurales de la unidad hidrogeológica del Campo de Montiel (Provincias de Ciudad Real y Albacete)

Abstract

The type of crustal deformation in the Campo de Montiel can assistin the understanding of the internal features of the main aquifer developed in the Jurassic carbonate platform . The direction of subsurface flow, the transmisivity and internal subdivision of the aquifer are interpreted in terms of cover and whole crust flexures as well as N140E directed transverse fault and fracture zones