“…Cement textures, composition, crosscutting relationships, fracture intensity analysis around and away from fault cores, spatial arrangement, and geochronology can all be used to reconstruct the evolution of brittle deformation and associated poro-permeability (e.g. Hansman et al, 2018;Aubert et al, 2019Aubert et al, , 2020Aubert et al, , 2021Cochard et al, 2021;Hoareau et al, 2021;Muñoz-López et al, 2022). Importantly, recent advances in calcite U-Pb geochronology allow direct dating of the absolute timing of calcite precipitation (Rasbury and Cole, 2009;Roberts et al, 2020;Roberts and Walker, 2016;Goodfellow et al, 2017;, opening an opportunity for in-depth structural-diagenetic studies of the evolutionary history of carbonate-rich fault zones (e.g.…”