Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution
Table 3
Fluid composition of the geothermal wells in the southern Molasse Basin.
Well
Salinity from FI data (g/L)
Salinity (g/L) reservoir in production
STG
33
18.0
A1
112
0.5-10.6
MOS
12
0.2-2.0
C1
9
5.0-10.0
SCH
18
5.0-10.0
FRH 1
19
4.1
GEN
27
1.6
UHA 1
18
0.6
TRN 1
42
0.5
Recent well data were provided by Florian Heine, Technical University of Munich (TUM), Chair of Hydrogeology. Wolfgramm et al. [60], Birner et al. [59], and Stober et al. [58].
