Fracture, Dissolution, and Cementation Events in Ordovician Carbonate Reservoirs, Tarim Basin, NW China
Figure 1
Simplified tectonic map of the Tarim Basin showing paleouplifts and depressions (after Zhao et al. [25]), the distribution of platform margins of Ordovician carbonates (after Lin et al. [59]), and occurrence of basalts of the Tarim Large Igneous Province (after Xu et al. [47]).
