Quantitative Characterization and Determination of the Main Factors That Control Fracture Development in the Lower Paleozoic Shale in Southeastern Chongqing, China

<div>Distribution frequency diagram of shale fracture dip angle in the target layer, i.e., Longmaxi Formation (a) and Niutitang Formation (b), of southeastern Chongqing.</div>

Geofluids

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Figure 4

Figure 4: Quantitative Characterization and Determination of the Main Factors That Control Fracture Development in the Lower Paleozoic Shale in Southeastern Chongqing, China 

Figure 4 | Quantitative Characterization and Determination of the Main Factors That Control Fracture Development in the Lower Paleozoic Shale in Southeastern Chongqing, China 