Rosa Blanca Babín Vich, Juan Francisco Bergamín de la Viña, Carlos Fernández Rodríguez, José Manuel González Casado, José Luis Hernández Enrile, Antonio Rivas Ponce, Rosa María Tejero López, Gerardo de Vicente Muñoz
A gravity research was carried out in the SE of the Spanish Centra/ System. The upper crust has been modelled in 2 1/2 D along three profiles. The gravity models suggest that the faults affecting both the Mesozoic-Cenozoic cover and the Hercynian basement are main/y high angle inverse fau/ts. Sorne of them bound permian bassins and they are basement faults, reactivated during the alpine deformations. Key words: Gravity models, Upper Crust, Spanish Central System
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