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Two epochs of magmatism and metallogeny in the Cuihongshan Fe-polymetallic deposit, Heilongjiang Province, NE China: Constrains from U-Pb and Re-Os geochronology and Lu-Hf isotopes
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文摘

We propose a two-epoch metallogenetic model for the Cuihongshan deposit.

The Fe mineralization was related to the alkali-feldspar granite.

The Pb–Zn (Cu) and W–Mo mineralization were associated with the syenogranite.

The Fe mineralization took place at about 491.1 ± 2.4 Ma.

The Pb–Zn (Cu) and W–Mo mineralization occurred at about 198.0 – 202.1 Ma.

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