Initial gold enrichment within a Neoarchean granite-greenstone belt: Evidence from ore-bearing and ore-barren samples in the Jiapigou deposits, NE China
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文摘
The basement gneisses were formed at 2512 ± 9 Ma. They are mainly derived from a juvenile mafic LCC. Zircon reverse discordance is presented. The mechanism of initial Au preenrichment is presented.

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