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The study investigates the Prominent Hill iron oxide copper-gold deposit in South Australia, revealing that its high-grade mineralization is primarily sourced from magmatic fluids that underwent atmospheric oxidation. The research identifies four distinct fluid types involved in the mineralization process, with the main ore fluid being weakly saline and rich in copper and uranium. Key factors for exploration include active volcanism, fluid mixing interfaces, and the presence of reactive host rocks.

Author

jshcugb

Language

EN