“…CBM is gradually formed in the long-term complex geological evolution process (Wang and Du, 2020;Zhou et al, 2021), so its occurrence is affected by structural evolution, depositional environment, buried depth, roof and floor lithology, coal seam thickness, hydrogeology, and magmatic activity (Xie et al, 2018;Zou et al, 2018a;Zhang C. L. et al, 2020;Kong B. et al, 2021;Zhang C. L. et al, 2021). Tectonic evolution is the key factor controlling the generation, migration, and occurrence of CBM (Zou et al, 2018b;Zhang K. Z. et al, 2020;Zhou et al, 2022).…”