“…At the same time, the exposed rocks around the Qinshui Basin, which include Taershan, Huyanshan, Zijinshan, Erfengshan, Gufengshan, etc, started to form (Yan et al, 1988;Shanxi, 1989;Wu et al, 1996Wu et al, , 2008Ying et al, 2011;Si, 2015;Huo, 2016;Yang, 2016;Chang et al, 2017;. It can be seen that there was a tectono-thermal event represented by intense magmatic activity in the Late Jurassic to Early Cretaceous, which is generally considered to be closely related to the secondary gas peak of coal seams in the basin at the same time (Figure 11) (Zeng et al, 1999;Xu et al, 2004;Jiang et al, 2005;Ren et al, 2005;Sun et al, 2005;Duan et al, 2011;Chen et al, 2019Chen et al, , 2019Yu et al, 2020a;Gao et al, 2021).…”