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 10

Crossplots of porosity and permeability for different types of dolomite rocks. Note the three lines which show the three classes of porosity-permeability relationship according to Lucia (1995). The permeability of the detection limit is 4 × 10⁻¹⁷m².