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

<div>Subsidence plot for the Upper Jurassic carbonate rocks, divided into the western (gray) and eastern (black) Molasse Basin. The eastern Molasse Basin was down-lifted further than the western Molasse Basin, and both parts have reached the maximum depth today. The sediment thickness was used from the borehole data at Traunreut (eastern Molasse Basin) and Mauerstetten (western Molasse Basin) and was not corrected for compaction. Due to varying geothermal gradients, the relative depths were assumed.</div>

Geofluids

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Figure 14

Figure 14: Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 

Figure 14 | Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 