Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution

<div>Overview of the study area in the Molasse Basin, southern Germany and eastern Switzerland. In addition, the measured temperature and salinity values measured in the fluid inclusion assemblage (FIA) of the cement phase of the late vein calcites and in the present reservoir fluid are given.</div>

Geofluids

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Figure 15

Figure 15: Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 

Figure 15 | Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 