All abstracts by Marco L. Fiorentini at Goldschmidt2006
| (2006) Multiple S isotope study indicates footwall hydrothermal exhalative massive sulfides were the major sulfur source for Archean komatiite-hosted magmatic nickel-sulfides from Western Australia and Canada
Fiorentini M, Bekker A, Rumble D, Barley M & Beresford S |
| (2006) The role of water in Precambrian ultramafic magmatism: Insights from an in-situ microbeam and nanobeam assessment of hydromagmatic amphibole
Fiorentini M, Beresford S, Deloule E, Stone B, Hanski E & Pearson N |