CO 2 geologic storage is an essential part of climate change solutions. Not only can it allow our fossil-fuel dominated society to achieve carbon neutrality while transitioning toward more renewables, but when combined with biomass energy or direct air capture, CO 2 geologic storage is a key component of negative carbon pathways (IPCC, 2005(IPCC, , 2014Rogelj et al., 2018;Wilcox et al., 2021). One major target for CO 2 geologic storage is deep saline aquifers due to their large storage capacity and widespread availability (IPCC, 2005). However, in the sedimentary basins where these saline aquifers are located, the rock formations all have natural geologic fabrics (depositional textures at cm-to-m scales) that can be highly heterogeneous (Murphy et al., 1984;Rubin & Carter, 1987). Even small-scale heterogeneities (cm-scale) can significantly affect CO 2 migration and trapping (