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The document discusses the origin of Au-rich carbonate-hosted replacement deposits in the Kassandra Mining District of Northern Greece, focusing on the geological and hydrothermal processes involved. It presents evidence for late Oligocene structurally controlled hydrothermal systems, detailing mineral associations, isotopic compositions, and metal distribution patterns across various deposits. The findings suggest a complex zoned hydrothermal system influenced by magmatic sources and fluid interactions, co

Author

junior.geologia

Language

EN