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Paralleling this alteration was the formation of abrupt pyrite-pyrrhotite transitions, and a zonation from sphalerite to galena to chalcopyrite.
The characteristic folded and breccia ores were not the result of ductile or fluid-assisted deformation of preexisting sulphide-siltstone interlayers, but instead formed by shear-controlled carbonate alteration that was ultimately replaced by sulphides.
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A completely different ore genesis paradigm may result and exploration concepts may need to be substantially modified.
Progressively further inwards, it changes to mica and albite-bearing ‘buff alteration’, commonly into siderite, magnetite and stilpnomelane, through a chloritic zone, to ultimately massive ‘silica-dolomite’ alteration.This is the same event as that which formed the copper ore (Perkins, 1984; Swager, 1985a) and indicates copper-lead-zinc to be a zoned late-stage epigenetic system.A succession of stratigraphically-constrained samples traced into the orebody reveals the progressive development of an alteration system that formed from well-laminated carbonaceous siltstones and mudstones.Layer-parallel mineralisation commonly terminates abruptly on or near extensional dolomite veins that formed progressively through the last major deformation event in the mine.