“…Deep magma in the continent's edge fiercely uplifted, resulting in massive volcanic eruptions, forming volcanoes of large‐scale and multistage composite superimposition (D. Li, He, Tang, Fan, & Kong, ; W. Z. Zhao, Zou, et al, ). This is also similar to environments of volcanoes in the Upper Carboniferous in Santanghu, Kelameili, and Wucaiwan (Z. Chen et al, ; Luo et al, ; J. Wu et al, ) which are in the nearby Mulei Depression.…”