Whether the Middle Eocene Salt-Forming Brine in the Kuqa Basin Reached the Potash-Forming Stage: Quantitative Evidence from Halite Fluid Inclusions

<div>Characteristics of evaporite lithology and halite fluid inclusions from borehole DZK01 in the Kuqa Basin. (a) Gypsum rock with maroon boulder clay; (b) pure rock salt and rock salt with maroon boulder clay; (c, d) primary band-like fluid inclusions developed along growth faces of halite crystals and pits left on the surface of halite after laser ablation.</div>

Geofluids

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Figure 3: Whether the Middle Eocene Salt-Forming Brine in the Kuqa Basin Reached the Potash-Forming Stage: Quantitative Evidence from Halite Fluid Inclusions 

Figure 3 | Whether the Middle Eocene Salt-Forming Brine in the Kuqa Basin Reached the Potash-Forming Stage: Quantitative Evidence from Halite Fluid Inclusions 