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

<div>Oxygen and carbon isotopes of Upper Jurassic carbonate rocks from outcrops of the Franconian and Swabian Alb. Dashed window—Upper Jurassic dolomitization window according to Reinhold [<a href="/journals/geofluids/2019/8980794/#B17">17</a>]. LT: low-temperature dolomites; HT: high-temperature dolomites; TZ: transition zone according to Allan and Wiggins [<a href="/journals/geofluids/2019/8980794/#B54">54</a>]. The arrow lines with a trend of increasing meteoric influence according to Liedmann [<a href="/journals/geofluids/2019/8980794/#B18">18</a>].</div>

Geofluids

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Figure 10: Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 

Figure 10 | Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution 