The variability of ruthenium in chromite from chassignite and olivine-phyric shergottite meteorites: New insights into the behavior of PGE and sulfur in Martian magmatic systems.
Baumgartner, R. J., Fiorentini, M. L., Baratoux, D., Ferrière, L., Locmelis, M., Tomkins, A. and Sener, K. A. Meteoritics & Planetary Science. doi: 10.1111/maps.12795 LINK “The Martian meteorites comprise mantle-derived mafic to ultramafic rocks that…