Geofluids / 2019 / Article / Fig 7

Research Article

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-, SO42-, 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)

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