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The Keketale Pb–Zn volcanogenic massive sulfide (VMS) deposit occurs in the early Devonian sequence of the Kangbutiebao Formation of the Southern Altai Metallogenic Belt (SAMB), northern Xinjiang, China. All the orebodies are stratabound and hosted by a suite of meta-sedimentary rocks intercalated with volcanic rocks. Major sulfide ores are pyrite, sphalerite, galena, with minor pyrrhotite and rare...
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