I guess another point worth making is that a lot of mines (including in Australia) only contain very minor quartz veining within the ore.
Often if an ore body gets metamorphosed the original ore changes to new minerals and quartz veins disappear by chemical reaction. Hemlo in Canada is a multi-million ounce example - this is ore.
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Big Bell near Cue is another example (2.6 million oz) - I don't remember any distinct quartz vein there. President Herbert Hoover used to be the mine manager and a member of Cue municipal council (as he was also at Sons of Gwalior mine at Leonora, 5.5 million oz production so far, where his old house is perched on the edge of the open cut). The ore body there is a mica schist with just quartz stringers. Also Challenger in a quartz-feldspar-kyanite-garnet pegmatite (i.e. granite vein) in South Australia (750,000 oz). Others of this type are being found in the Wheat Belt of WA.
Also a small garnet rock gold body without quartz near Bathurst.
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And of course Olympic Dam copper ore body has produced millions of ounces of gold from ore with no quartz veins - a breccia ore body of just iron oxide and copper and iron sulphides. Sulphide ore bodies weather to iron oxide (gossan) at surface.
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Australia's largest gold mine, Boddington (at least 10 million oz so far, another 10 m oz still unmined) original mined gold from a bauxite laterite at surface (with coarse gold). It also produces copper.
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Here is another type of sulphide-rich gold ore with no defined quartz veins (in granite from Canada but similar to Cadia and others in NSW).
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Because gold can form nuggets in laterite soil above any of these types of ore body with negligible or no quartz, it is important to be aware of them.