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What is High-Sulphidation Epithermal Gold Systems about?
1) Epithermal gold deposits form near the surface due to hot fluids emanating from magmas underground. These fluids transport gold and other metals. 2) There are two main types of epithermal gold deposits - low-sulfidation and high-sulfidation. High-sulfidation deposits form from strongly acidic fluids and dissolve surrounding rock, leaving silica behind to precipitate gold. 3) Notable high-sulfidation deposits include Yanacocha in Peru, one of the largest gold deposits in the world, and Pierina, also in
- Author
- Mohammad Wildan Arifin
- Language
- EN