Tectónica distensiva y halocinesis en el margen SO de la cuenca Vasco- Cantábrica

Abstract

Extensional tectonics and associated halokinetics processes controlled the sedimentation in the southwestern margin of the Basco-Cantabrian basin during Upper Jurassic and Lower Cretaceous times. The development of Mesozoic growth faults, compressive features at present, controlled the geometry and limits of the sedimentary bodies deposited at those times