@article{10272/12260, year = {1996}, url = {http://hdl.handle.net/10272/12260}, abstract = {The Cameros Basin ( N W o f the Iberian Range) is m a in ly composed o f very homogeneous silicic d e tr ita l m aterials in Weald facies. The occurrence o f c h lo rito id , cookeite, p y rite an d muscovite/p aragonite is related to a cretacic very low grade metamorphism. The geochemical analysis of this materials displays differences linked to lithologic features; comparison between metamorphic and no metamorphic materials shows no main differences in the chemical contents, but in the relationships between elements}, publisher = {Sociedad Geológica de España}, keywords = {Cameros Basin}, keywords = {Weald facies}, keywords = {Geochemistry}, keywords = {Very Low grade - Metamorphism}, title = {Diferenciación geoquímica de los materiales en facies «Weald» de la Cuenca NE de Cameros (Soria - La Rioja)}, title = {Geochemical differentiation of «Weald» materials of Cameros Basin (Soria - La Rioja)}, author = {Mata Campo, M. P. and Osácar, María Cinta and López Aguayo, F.}, }