Stacking faults and twin boundaries in sphalerite crystals from the Trepca mines in Kosovo

The structure and chemistry of {111} twin boundaries and stacking faults in Fe-rich sphalerite crystals from the Trepca mines in Kosovo were studied using electron microscopy. The {111} twin boundaries were found to be deficient in S and enriched in O, Mn, Fe, and Cu. The deficiency in S is compensated with 0, which is responsible for stabilizing the hexagonal stacking of the fault structures and the formation of {111} twin boundaries in sphalerite. Comparing the intensities of Bijvoet-related reflections we show that there is no inversion of the polar axis across the twin boundaries. In addition to twin boundaries we found two types of stacking faults with R-SF1 = 1/3.[(1) over bar 12] and R-SF2 = 2/3.[(1) over bar 12]. The excretion of isostructural copper from the sphalerite crystals peaks at the twin boundaries until it precipitates in the form of small chalcopyrite grains, aligned along the {111} twin boundaries.