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 11

The fluid velocity for Scenario I: (a)  : , (b)  : , and (c)  : , Scenario II: (d)  : , (e)  : , and (f)  : , and Scenario III: (g)  : , (h)  : , and (i)  : . The arrow lines indicate the general pathways of fluids. 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)