Fractionation of highly siderophile and chalcogen elements in the lower oceanic crust: Insights from the troctolites of the Alpine-Apennine Jurassic ophiolites

The present study aims at investigating the role of reactive porous flow in the fractionation of highly siderophile (HSE: Os, Ir, Ru, Rh, Pt, Pd, Au and Re) and chalcogen (S, Se, Te) elements during construction of the lower oceanic crust in (ultra-)slow spreading ridges. At this purpose, we analyzed the whole-rock HSE and chalcogen elements, and Re-Os isotopes in olivine-rich troctolites embedded within large-scale gabbroic sequences from the Alpine- Apennine Jurassic ophiolites. Leucotroctolites and chromitites associated with the olivine-rich troctolites were also investigated. The olivine-rich troctolites have initial γOs ranging from +0.2 to +5.9. Their primitive mantle-normalized patterns are characterized by a slight enrichment of Os over Ir, and an increase from Ir to Ru, Rh, Pt, Pd and Au, nearly flat Au-Te-Se-S, and weak Re depletion with respect to S. This HSE and chalcogen element, and Os isotopic signature was acquired in response to sulfide segregation, which was most likely trig- gered by reaction between an olivine-rich matrix and migrating MORB-type melts. The chromitite layers occur- ring within the olivine-rich troctolites exhibit high concentrations of platinum group elements (PGE: Os, Ir, Ru, Rh, Pt and Pd). Formation of the chromitites might produce melts depleted in PGE that reactively migrated within the olivine-rich matrix, and ultimately locally led to olivine-rich troctolites characterized by a slight increase of the PGE/chalcogen element fractionation. The leucotroctolites differ from associated olivine-rich troctolites in the lower concentrations of HSE and chalcogen elements, with subparallel primitive mantle-normalized patterns but slightly higher Se/Te values. The crystallization of the olivine-rich troctolites might release HSE and chalcogen elements-depleted melts that reacted with an olivine + plagioclase crystal mush to form the leucotroctolites. Al- ternatively, formation of the leucotroctolites involved a process of reacting melt flow characterized by a low melt/ crystal matrix ratio, which led to a relatively low proportion of trapped melt and related sulfides. At (ultra-)slow spreading ridges, the crystallization of sulfides in high-Mg# lower crustal rocks may exert a significant control in shaping the HSE and chalcogen element signature of erupted basalts.