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Multi-stage fluid boiling and formation of the giant Fujiawu porphyry Cu-Mo deposit in South China
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文摘
Multi-stage fluid boiling corresponds to the Cu and Mo mineralization at Fujiawu. High-salinity inclusions were not produced by fluid boiling. The Fujiawu deposit was generated in a localized extensional setting. Subduction-modified lithospheric mantle is an important metal source.

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