Numerical Modeling of Reactive Transport and Self-Sealing Processes in the Fault-Controlled Geothermal System of the Guide Basin, China

Figure 7

(a) Calculated temperatures along fast upflow paths at the position of ZR1, (b) the variation of mineral saturation indices, (c) Na⁺, K⁺, Ca²⁺, Mg²⁺, Al³⁺, HCO₃^-, Cl^-, SO₄^2-, and SiO₂ concentrations, and (d) mineral abundance. The mineral abundance of kaolinite, chlorite, smectite-Ca, and dolomite maintains unchanged which is not shown in (d).

(a)

(b)

(c)

(d)