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Location: 25 km NE from Barberton, South Africa
8 Streak StreetNelspruitSouth AfricaPO Box 820, Nel
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The Lily mine is a lode gold deposit along the faulted interface between the Figtree and Onverwacht groups of the Archaean Barberton greenstone belt. The Onverwacht metavolcanics are composed of talc and talc-carbonate schists derived from ultramafic precursors, while the Figtree metasediments comprise interbedded greywacke, shale and chert. The general trend is an east-west strike with asteep southerly dip. The shearing andmineralisation are parallel to the regional fabric. The gold mineralisation is structurally controlled and associated with fine grained pyrrhotite, minor arsenopyrite and chalcopyrite, and with quartz-carbonate veins.
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