Research Article
Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution
Figure 8
Boxplots of homogenization temperature versus true vertical depth of the calcite and dolomite 2-phase fluid inclusions from the wells in the Molasse Basin. In gray, the sampled wells are named using the same abbreviation as Figure 1.