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 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.