RT Journal Article
T1 El drenaje subterráneo de la Sierra de Cameros en la Cuenca del Ebro y su implicación en la génesis de depósitos marginales evaporíticos miocenos
T1 The Regional Groundwater Discharge from the Cameros Chain into the Ebro Tertiary Basin and its implications in the formation of miocene marginal evaporitic units
A1 Coloma, Pablo
A1 Martínez Gil, F. J.
A1 Sánchez Navarro, José Ángel
AB 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
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12873
UL http://hdl.handle.net/10272/12873
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026