“…Due to the differences in geological characteristics between the lacustrine shale in China and the marine shale in North America, such as complex structure, deep burial, and strong heterogeneity, it is hard to copy the successful experience and models of North America (Cui et al, 2015;Zhou et al, 2015;Jin et al, 2016). At present, the research of lacustrine shale has already made certain understanding and essential progress in mineral composition and genesis (Aplin and Macquaker, 2011;Slatt and Rodriguez, 2012;Chermak and Schreiber, 2014;Liu et al, 2020a), shale sedimentary environment (Wang et al, 2019;Liu et al, 2020b;Ji et al, 2020;Liu et al, 2021;Wang et al, 2021), and pore types and characteristics (Loucks et al, 2012;Milliken et al, 2013;Ji et al, 2019). The lithofacies of shale contain information including mineral components, rock types, sedimentary structures, and organic matter abundance (Loucks and Ruppel, 2007;Ross and Bustin, 2009;Xu et al, 2018;Xu et al, 2019;Xu et al, 2020), which makes the division and distribution of lithofacies become a fundamental geology issue (Newport et al, 2016;Tang et al, 2016;Wang et al, 2018).…”