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 15

The dolomite dissolution patterns simulated for an interval of 10 Ma for Scenario I: (a)  : , (b)  : , and (c)  : ; Scenario II: (d)  : , (e)  : , and (f)  : ; and Scenario III: (g)  : , (h)  : , and (i)  : . The plotting area is referred to the model domain below dashed lines in Figure 11 which is mainly composed of dolomite formation.

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)

(i)