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The Maevatanana gold deposit in Madagascar is characterized by quartz-sulfide veins in Archean metamorphic rocks, with gold mineralization linked to magmatic processes and tectonic activity. Fluid inclusion studies indicate that the ore-forming fluids originated from granitic magma, with a mineralization age of approximately 535 Ma, coinciding with the Cambrian post-collisional A-type granitoids. The deposit
- Author
- Siraj Beyan
- Language
- EN