@article{10272/13196,
year = {1996},
url = {http://hdl.handle.net/10272/13196},
abstract = {The Cameros basin (Iberian Chain) developed under a very subsident extensional regime during the latest Jurassic-early Cretaceous. Its fill constitutes a magasequence o f more than 5000 m of vertical thickness. That would produce a gravity low. Nevertheless, the gravity map of this area draws a gravity high in the eastern part of the basin. We propose an explanation to this contradiction},
publisher = {Sociedad Geológica de España},
title = {Estructura profunda de la cuenca de Cameros (Cordillera Ibérica) a partir de datos gravimétricos},
title = {Deep structure of thè Cameros basin (Iberian Chain) from gravity data},
author = {Rivero, Luis and Guimerà, J. and Casas Sainz, Antonio},
}