Geochemically heterogeneous Martian mantle inferred from the lead isotope systematics in the two depleted shergottites Yamato 980459 and Dar al Gani 476
(49th Lunar and Planetary Science Conference 2018)
Lead isotope systematics of acid residues from depleted olivine-phyric shergottites: Implications for heterogeneous depleted source mantle
(48th Lunar and Planetary Science Conference 2017)