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The Qiyugou Au deposit in central China features breccia pipe-hosted and porphyry Au mineralization, with significant gold reserves. An integrated study utilizing geochronology and sulfur isotope analysis reveals a close spatial-temporal relationship between the two mineralization styles, indicating a shared magmatic-hydrothermal source. The findings suggest that the mineralization resulted from multiple fluid exsolution events from a deep-seated magma chamber.

Author

jshcugb

Language

EN