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

Figure 7

The relationships between K⁺ and Mg²⁺, Rb⁺ and Br^-, and Sr²⁺ and Ca²⁺ in halite fluid inclusions from 1476 m in borehole DZK01.