“…• Flow of acidic brine through fractures in mineralogically heterogeneous rocks selectively dissolves calcite and creates a porous layer • Calcite-depleted porous layer collapses under normal stresses, filling the fracture with fine particles, decreasing permeability • Layer of fine particles lowers fracture frictional strength because it prevents the formation of interlocking microasperities 2013; Fang et al, 2016;Majer et al, 2007;Moeck et al, 2009;Rinaldi et al, 2015;Segall & Fitzgerald, 1998;Talwani, 1997;Walsh & Zoback, 2016;Zoback & Gorelick, 2012). Concurrently, the injection of fluids into the subsurface can create reactive fluids, such as the injection of CO 2 which dissolves in water and forms carbonic acid (Benson & Cole, 2008;Bielicki et al, 2018;Borgia et al, 2012;Gaus, 2010;Pearce & Dawson, 2018;Wilkins et al, 2016). Such reactive brines can enter and alter flow pathways by dissolving reactive minerals and increasing fracture permeability (e.g., Hawkes et al, 2005).…”