
Location: |
Palabora (Phalaborwa) Complex, Transvaal, Republic of South Africa |
Major Minerals: |
Magnetite, chalcopyrite, bornite, locally cubanite |
Minor Minerals: |
Pyrrhotite, valleriite, chalcocite |
Trace Minerals: |
Include violarite, linnaeite, bravoite, millerite, pentlandite, siegenite, pyrite, marcasite, tetrahedrite, covelline, galena, sphalerite, baddeleyite, uranothorianite, ilmenite, ulvöspinel, hogbomite, pseudobrookite, native gold, electrum, mooihoekite |
Textures: |
Titaniferous magnetite is euhedral to subhedral and contains ilmenite, ulvöspinel, hogbomite and pseudobrookite inclusions. Ulvöspinel forms very fine exsolution lamellae along (100) planes of the host magnetite to give the characteristic 'cloth-weave' fabric. Chalcopyrite and bornite form lamellar intergrowths and either mineral can be the host. Coarse-grained intergrowths of chalcopyrite-cubanite-pyrrhotite are localized in occurrence. Bornite-chalcocite form symplectite intergrowths (graphic intergrowths). Chalcopyrite, bornite and chalcocite replace magnetite and silicates and are themselves replaced by valleriite |
References: |
Russell et al., 1954; Forster, 1958; Lombaard et al., 1964; Hanekom et al., 1965; Palabora Mining Staff, 1976; Verwoerd, 1986 |
