“…The components of shales, such as minerals and OM have their own Young's modulus and Poisson's ratio, indicating that different mineral types and content influence shale fracability differently (Huo et al, 2018). As typical brittle minerals, quartz and pyrite have strong fracability (Chen et al, 2021b; Gholami et al, 2016; Jin et al, 2015; Simmons and Birch, 1963), whereas clay minerals and OM have poor fracability (Lawal et al, 2021; Mews et al, 2019; Walles, 2004; Yasin et al, 2017). Calcite, dolomite, and siderite have similar Young's moduli and Poisson's ratios, are non-brittle minerals, and contribute moderately to fracability (Mathia et al, 2016; Christensen, 1972).…”