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中科院地质地球所
(4)富Au中硫型矿床的成矿岩浆起源于俯冲交代地幔楔的部分熔融,形成于中性-挤压的火山弧中。有时在同一矿区除了发育富Au的NC型中硫型矿床外,还可以形成斑岩Cu ± Au和高硫型Au矿床( 图5A、图5B ...
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