The 982 Ma Re-Os age of copper-nickel sulfide ores in the Baotan area, Guangxi and its geological si

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Re-Os dating on copper-nickel sulfide ores from the Baotan area, Guangxi, yielded an ore-forming age of 982±21 Ma(2σ), which demonstrates that copper-nickel sulfide deposits and their related mafic-ultramafic rocks occurred in the same period of time
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