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 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.