@article{10272/12873,
year = {1996},
url = {http://hdl.handle.net/10272/12873},
abstract = {In the northern margin of the Cameros Basin miocene evaporitics units are found related with shallow saline lakes. The lakes were fed principal)/ by groundwater loaded with dissolved salts (calcicsulphate waters) from the Lias and Keuper evaporite formations. Durin Miocene, Ebro Basin was a endorheic depression, so the dissolved salts that were carried by groundwater had to precipitate inside the basin; groundwater discharge not be concentrated in a few big springs but it should be distributed in humid areas with evaporitic precipitation},
publisher = {Sociedad Geológica de España},
title = {El drenaje subterráneo de la Sierra de Cameros en la Cuenca del Ebro y su implicación en la génesis de depósitos marginales evaporíticos miocenos},
title = {The Regional Groundwater Discharge from the Cameros Chain into the Ebro Tertiary Basin and its implications in the formation of miocene marginal evaporitic units},
author = {Coloma, Pablo and Martínez Gil, F. J. and Sánchez Navarro, José Ángel},
}