“…Magnesium is the sixth most abundant element in the sun, 1 and one of the most important rock-forming constituents of planets from the inner solar system. Magnesium has three naturally occurring isotopes - 24 Mg, 25 Mg and 26 Mg -with relative abundances of $79%, 10% and 11%, respectively. Variations in the isotopic composition of Mg can potentially occur in solar system materials through a number of processes including (1) stellar nucleosynthesis, (2) the former presence and decay of the 26 Al nuclide (half-life ¼ 0.73 myr) and (3) mass-dependent isotopic fractionation during high-temperature processes such as partial evaporation/condensation as well as from low-temperature fluid/ rock interactions (e.g.…”