Investigating rare metal potentials of the Alpine regions is of great importance to progress towards future supply independence. Sphalerite is an important carrier of Co, In, Ga, Ge, and Sb, and we know from the Eastern Alps, that vein deposits roughly host 66% of the Co, 18% of the Ga and 4% of the In resource. Here, we present data of sphalerite (and chalcopyrite) from two contrasting vein deposits in the Southern Alpine basement: the Pfunderer Berg (PF) Cu-Zn-Pb-Ag mine near Klausen and the Rabenstein (RS) F-Zn mine in the Sarn Valley. The PF mine is a Permian intrusion-hosted vein deposit with a chalcopyrite-sphalerite-galena-sulphosalt paragenesis. RS mine is a vein deposit with fluorite-sphalerite paragenesis, probably related to the Periadriatic fault.
The two ores show contrasting textures and chemistry of sphalerite, which are primarily related to formation temperature: at PB high-T ZnS is black and homogeneous and enriched in Fe-Mn-Cd-Cu-Se-Co-In-Sn, while at RS low-T ZnS is honey-coloured and zones and enriched in Pb-As-Ag-Sb-Hg-Tl-Ga-Ge. Rare metal medians at PB are 303, 124, and 187 µg/g for Co, In, and Sn. At RS medians for Ga, Sb, Ag, Ge, are 383, 203, 85, and 9.1 µg/g. Spot analyses can reach higher values, either related to mineral inclusions (PB) or to zoning (RS). Across zoned ZnS grains, co-variations with Fe-content (0.3 to 6 wt.%) or Cu (70 to 5000 µg/g) are related to evolving hydrothermal pulse. Results demonstrate significant rare metal variations across deposit types, but also complexities of fractionation within given deposits.