“…To achieve it, we used the 3D trace element data reduction scheme (DRS) available on iolite 4 software after calibrating the instrument using both NIST SRM 612 and the North Chile (aka Filomena). Instead of the conventional instrumental drift approach, we applied a normalization that considers the sum of Fe, Ni, and Co mass fractions as 100%, eliminating the need for an independent measurement of Fe or Ni by another technique, as also demonstrated for other matrices. , In this way, Fe and Ni mass fractions can also be determined, yielding a complete set of elements needed for the chemical characterization of iron meteorites. This new calculation scheme was also applied to generate elemental imaging maps from the LA-ICP-MS data, expanding the versatility of the method.…”