“…Dissolution of carbonates ( e.g. , calcite and dolomite) in shales due to the injection of acid, most commonly HCl, has been shown to increase porosity and open pore throats in the shale matrix. ,,− This is particularly crucial for carbonate-rich systems. − Lu et al observed a limited increase in the permeability of Eagle Ford shale (52 wt % calcite) pre- and post-exposure to NaCl brine; however, Marcellus shale (6 wt % calcite, 3 wt % dolomite) exposed to the same brine showed a 5 times increase in permeability, which was assumed to be due to differences in mineral dissolution that either limited or enhanced further penetration of the fluid for the Eagle Ford and Marcellus shales, respectively. Li et al compared the chemically altered zone of a carbonate-poor Marcellus shale (1 wt % calcite, 6 wt % dolomite) and a carbonate-rich Eagle Ford shale (52 wt % calcite) exposed to HFF and quantified that carbonate dissolution extended deeper into the carbonate-poor matrix compared to the carbonate-rich matrix (100–200 vs 30–40 μm, respectively).…”