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

Figure 11

Oxygen and carbon isotopes of Upper Jurassic carbonates from deep wells of the southern Molasse Basin. Dashed window—Upper Jurassic dolomitization window according to Reinhold [17]; the new interpreted Upper Jurassic dolomitization window, LT: low-temperature dolomites; HT: high-temperature dolomites; TZ: transition zone according to Allan and Wiggins [54]. Arrow lines with a trend of increasing meteoric influence according to Liedmann [18].