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Silver-lead-zinc vein districts are commonly associated with major fault zones in clastic metasedimentary terranes; individual veins occur in a variety of lithologies ranging in age from Proterozoic to Cenozoic. Silver-lead-zinc veins are a late feature in the tectonic evolution of orogens. Classical examples are the Kokanee Range (British Columbia), Keno Hill (Yukon Territory), Coeur d’Alene (U.S.A.), Pribram (Czechoslovakia), and the Harz Mountains and Freiberg (Germany) (Fig. 16-1).

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