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 12

The temperature patterns of Scenario I: (a)  : , (b)  : , and (c)  : ; Scenario II: (d)  : , (e)  : , and (f)  : ; and Scenario III: (g)  : , (h)  : , and (i)  : . Note the model domains below the dashed lines which were arranged for plotting dissolved porosity in Figure 15.

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)

(i)