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1) Mineralization at Bulyanhulu consists of quartz veins and alteration haloes adjacent to shear zones containing gold-bearing sulphides. 2) Three forms of sulphide mineralization can be distinguished: barren pyrite related to exhalative activity in the host rocks; quartz-carbonate veins dominated by pyrite and chalcopyrite with gold; and minor porphyry-hosted vein-associated sulphidation. 3) Early syn-depositional pyrite (pyrite 0) shows no significant gold anomalies and lacks gold associations, suggestin
- Author
- Regina Efraim
- Language
- EN