The Sensitivity of Temperature to Tachyhydrite Formation: Evidence from Evaporation Experiments of Simulated Brines Based on Compositions of Fluid Inclusions in Halite

<div>A simulated evaporation-crystallization path on the Jänecke phase diagram at 50°C. (a) Khorat Plateau; (b) Sergipe basin; (c) Congo basin. The evaporite mineral succession. (d) Khorat Plateau; (e) Sergipe basin; (f) Congo basin.</div>

Geofluids

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Figure 4

Figure 4: The Sensitivity of Temperature to Tachyhydrite Formation: Evidence from Evaporation Experiments of Simulated Brines Based on Compositions of Fluid Inclusions in Halite 

Figure 4 | The Sensitivity of Temperature to Tachyhydrite Formation: Evidence from Evaporation Experiments of Simulated Brines Based on Compositions of Fluid Inclusions in Halite 