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Ore geology, fluid inclusion and 40Ar/39Ar geochronology constraints on the genesis of the Yingchengzi gold deposit, southern Heilongjiang Province, NE China
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This paper firstly reports an orogenic Au deposit in Zhangguangcai Range, NE China.

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The deposit was formed during Late Permian–Triassic continental collision.

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Ore-fluids were mesothermal, CO2-rich and low salinity.

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Fluid boiling and mixing have caused gold and sulfide precipitation.

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