RT Journal Article
T1 Hidrogeoquímica convencional e isotópica de las aguas carbónicas de Cataluña
T1 Conventional and isotopic hydrogeochemistry of CO2-rich waters of Catalonia
A1 Redondo, R.
A1 Yélamos, J. G.
AB Conventional and isotopic hydrogeochemical techniques have been applied to a study of CO2-rich waters in the northeast of Catalonia. Two hydrogeochemical facies, a calcium-bicarbonate and another sodium-bicarbonate are clearly distinguished. The second one seems to be the result of evolution from the calcium facies. The tritium-ages support the previous division in two hydrogeochemical facies. Measurements of ,sO and deuterium ratio indicate that the carbonic waters have a meteoric origin. The i3C/12C ratio varied from -5,0 to -0,64 6°/œ showing a deep origin of CO
PB Sociedad Geológica de España
YR 1999
FD 1999
LK http://hdl.handle.net/10272/9878
UL http://hdl.handle.net/10272/9878
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026