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This paper discusses new geological and geochemical data on intrusion-related gold deposits found in historically tin-tungsten mineralized terranes, linking them to specific magmatic-hydrothermal processes. The findings suggest that exploration should focus on moderately reduced, metaluminous I-type granites rather than highly fractionated S-types, with a variety of deposit styles influenced by host rock and depth of emplacement. Additionally, new fluid inclusion data reveals significant geochemical variati

Author

Rene Bautista

Language

EN