@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.},
}