A fluid inclusion study of the Hetai goldfield in the Qinzhou Bay-Hangzhou Bay metallogenic belt, South China
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文摘

The Hetai goldfield in South China is a structural controlled lode system.

The deposit was formed by metamorphic-devolatilized CO2-rich fluids.

Immiscibility and CO2 effervescence of fluids are the key to gold precipitation.

The Hetai goldfield resembles typical orogenic gold deposits in the world.

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