Hydrothermal Dissolution of Deeply Buried Cambrian Dolomite Rocks and Porosity Generation: Integrated with Geological Studies and Reactive Transport Modeling in the Tarim Basin, China

<div>Spatial patterns of fault/fracture systems on some important stratal levels traced by seismic reflection surfaces in northern Tarim. (a) T9<sup>0</sup> (lower surface of Cambrian formation), (b) T8<sup>0</sup> (upper surface of Cambrian formation), and (c) T7<sup>8</sup> (upper surface of Lower Ordovician Penglaiba Formation) as indicated in Figure <a href="../fig3/">3</a>. Note the location of borehole TS1.</div>

Geofluids

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Figure 5

Figure 5: 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 5 | Hydrothermal Dissolution of Deeply Buried Cambrian Dolomite Rocks and Porosity Generation: Integrated with Geological Studies and Reactive Transport Modeling in the Tarim Basin, China 