Dedolomitization Potential of Fluids from Gypsum-to-Anhydrite Conversion: Mass Balance Constraints from the Late Permian Zechstein-2-Carbonates in NW Germany

<div>Paleogeography of the Zechstein-2-Carbonate for the study area in northern Germany. The map displays the studied wells and the uppermost facies association of the Stassfurt Carbonate (Ca2) within this area (modified after Strohmenger and Strauss [<a href="/journals/geofluids/2018/1784821/#B41">35</a>]).</div>

Geofluids

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Figure 3

Figure 3: Dedolomitization Potential of Fluids from Gypsum-to-Anhydrite Conversion: Mass Balance Constraints from the Late Permian Zechstein-2-Carbonates in NW Germany 

Figure 3 | Dedolomitization Potential of Fluids from Gypsum-to-Anhydrite Conversion: Mass Balance Constraints from the Late Permian Zechstein-2-Carbonates in NW Germany 