Resumen de El drenaje subterráneo de la Sierra de Cameros en la Cuenca del Ebro y su implicación en la génesis de depósitos marginales evaporíticos miocenos
Pablo Coloma López, Francisco Javier Martínez Gil, José Ángel Sánchez Navarro
In the northern margin of the Cameros Basin miocene evaporitics units are found related with sha/low saline lakes. The lakes were fed principaly by groundwater loaded with dissolved salts (calcicsulphate waters) from the Lias and Keuper evaporite formations. Ourin 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.
