Research Article

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 14

The temperature patterns 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)