“…However, the empirical relationship is highly lithology-and region-specific (Tamunobereton-Ari et al, 2010). In carbonate formation, which has a complex pore structure and strong heterogeneity, the variation of shear wave velocity in carbonate is the result of an interaction between lithofacies, diagenetic process, and porosity (Rafavich et al, 1984;Anselmetti and Eberli, 1993;Tamunobereton-Ari et al, 2010;Qabany et al, 2011;Wang et al, 2011;Kittridge, 2015;Garia et al, 2019). Thus, simple linear approximation is insufficient for accurately estimating the Vs The rock physics modeling technique for carbonate has being extensively studied by considering different mineral types, pore structures, and fluid conditions, and the studies have shown promising results (Xu and Payne, 2009;Sun et al, 2012;Zhang et al, 2013;Azadpour et al, 2020;Seifi et al, 2020).…”