ABSTRACT
Fluid inclusion in primary and detrital scheelite from the Kłodzko–Złoty Stok Variscan granitoid massif area in the Central Sudetes yielded pressure 0.9 – 1.3 kbar and crystallisation temperature 350 – 480°C for the in situ samples. Similar data were obtained for the detrital scheelite: pressure 0.8 – 1.2 kbar and crystallisation temperature 370 – 460°C; total salt concentrations in inclusion solution ranged from 2 to 14 wt %. Considerations on genetic relation of the two scheelite groups are presented.
