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 1

(a) Map of the Tarim Basin showing the main tectonic units (modified from He et al., [23]). Dashed rectangle denotes the location of study area and TS1. (b) Palaeogeographic setting of the northern Tarim Basin (study area) during the Cambrian period (modified from [17–21]). Dashed line indicates the location of seismic profile shown in Figure 3.

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