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The Shihu gold deposit, situated in the Taihang Mesozoic orogen of the North China Craton (NCC), is hosted by ductile‐brittle faults within Archean metamorphic core complex. The deposit is characterized by gold‐bearing quartz‐polymetallic sulfides veins. The Mapeng granitoids stock and intermediate‐basic dikes intruded the metamorphic basement rocks, and are spatially related to gold mineralization...
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