Hydrothermal Dissolution of Deeply Buried Cambrian Dolomite Rocks and Porosity Generation: Integrated with Geological Studies and Reactive Transport Modeling in the Tarim Basin, China

Figure 13

The fluid velocity for Scenario I with fault permeability of 1 × 10⁻¹³ m²: (a)  : , (b)  : , and (c)  :  and fault permeability of 1 × 10⁻¹⁵ m²: (d)  : , (e)  : , and (f)  : .

(a)

(b)

(c)

(d)

(e)

(f)