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

<div>Relative variation of porosity and permeability within the fault F2 after 8000 years. Negative value means the decrease of porosity and permeability due to mineral precipitation.</div>

Geofluids

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Figure 8

Figure 8: Numerical Modeling of Reactive Transport and Self-Sealing Processes in the Fault-Controlled Geothermal System of the Guide Basin, China 