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 9

Initial values of horizontal permeability used in simulations for Scenario I (a), Scenario II (b), and Scenario III (c). Note that the permeability was assigned to different stratigraphic and lithologic units based on Figure 3. The lithologic units which are not displayed in Figure 3 are assigned based on the stratigraphic description in Figure 2.

(a)

(b)

(c)