The chemical composition of Zn-, Cu and Fe sulphides in base metal mineralizations of the Eastern Alps was investigated using laser ablation-ICP-MS methods, with a focus on the concentration of high-technology, critical metals. A total of more than 6300 in-situ analyses were carried out on 311 polished sections representing 27 individual mineralizations. These comprise carbonatehosted Pb-Zn deposits of the Bleiberg-type, stratiform deposits in Paleozoic metasediments and metavolcanic rocks (e. g. Arzberg, Walchen) and vein-type mineralization (e. g. Koprein, Metnitz). Two sphalerite types emerge: type (1) is poor in Fe (<1%), Mn, Co, Ga, In, Sn, Sb, but significantly enriched in Ge (up to >500 ppm), As, Tl and Pb; it is restricted to carbonate-hosted non-metamorphosed sediments. (2) Sphalerite elevated in Fe, Co, Ni, Cu, Ag, In and Sn in stratiform and vein-type ores hosted by Paleozoic low to medium grade metamorphic rocks. Large variations exist among both groups, and unusual compositions were also encountered, e. g. vein-type ores showing a Ge-Sb-Co association at Metnitz, Gurktal nappe. Chalcopyrite associated with type (2) sphalerite may have high Ag and In concentrations. Pyrite and pyrrhotine are carriers of Co, Ni and As. The highest potential for Ge is associated with carbonate-hosted ores in the Drauzug and Karawanken Mountains. For Co and In, low potentials are associated with some of the larger stratiform mineralizations.