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The Tanjianshan gold deposit, located at the tectonic boundary between the Oulongbuluk block (OB) and North Qaidam orogenic belt (NQO) on the northern margin of the Qaidam basin (NMQB), western China, underwent Early Palaeozoic and Late Palaeozoic to Early Mesozoic multiple accretions and collisional orogenies. It is a typical example of a deposit resulting from two gold mineralizing events related...
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