“…Geochemical analysis of fillings is the common method used to distinguish karst stages, such as the analysis of trace elements in sand-mud filling , isotopic analysis of cave macrocrystalline calcite (Liu et al, 2008), strontium isotope (Zhang et al, 2005;Liu et al, 2006;Liu et al, 2007;Zhang and Cai, 2007), carbon and oxygen isotopes (Winter and Knauth, 1992;Chen, 1994;Wang and Al-Aasm, 2002;Xia and Tang, 2004;Xia et al, 2006;Qian et al, 2008;Ainsaar et al, 2010;Wu et al, 2010;Li et al, 2011;Meng et al, 2011;Xia et al, 2011;Haeri-Ardakani et al, 2013), aqueous inclusion homogenization temperature (Xia and Tang, 2004;Xia et al, 2006;Wu et al, 2010;Xia et al, 2011;Li et al, 2012;Li et al, 2013), and autogenous illite K-Ar dating (Xu et al, 2012). Combined with the analysis of regional tectonic evolution and associated quantitative parameters (Xu et al, 2012;Zhang, 2020), a comprehensive application of a variety of geochemical methods (Zhang et al, 2012;Wang et al, 2017;Lyu et al, 2020) was also used to distinguish collapse-filling stages. However, there is still a lack of suitable methods to classify karst stages in detail by integrating core, isotope, and other means.…”