In December 2025, the joint ESA and JAXA BepiColombo mission will enter orbit around Mercury to begin a 1-year nominal plus 1-year extended science mission (Benkhoff et al., 2010). Among the 16 instruments shared across two spacecraft is the Mercury Imaging X-ray Spectrometer (MIXS) on board the Mercury Planetary Orbiter (MPO). The MIXS instrument represents the first time a true-imaging X-ray spectrometer has been sent to another planet and it is expected to offer unprecedented insights into the surface elemental composition of Mercury (Bunce et al., 2020;Fraser et al., 2010). This instrument will follow on from the successful MErcury Surface, Space ENvironment, Geochemistry and Ranging (MESSENGER) mission (Solomon & Anderson, 2018) which has posed a number of questions of great scientific importance for follow up by BepiColombo.As part of target prioritization for the MIXS instrument, we identified a need for a catalog of all the craters that retain a central peak (or peak-ring) structure resolvable by MIXS (Data Set S1; Tables S1 and S2; Figures S1-S8). Interestingly, upon completion of the MIXS crater catalog we identified a potential spatial correlation between an abnormally high spatial density of peak-ring basins (PRB) and the high-magnesium