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What is Sulfidation States in Hydrothermal Systems about?
This document discusses the sulfidation state of fluids in active and extinct hydrothermal systems, from porphyry to epithermal environments. It finds that sulfidation states of magmas are very low to low, while reactive magmatic-hydrothermal fluids trend to higher oxidation and sulfidation states with declining temperature. Sulfide mineral assemblages in various deposit types describe a cooling path of increasing sulfidation state from RS = -1 at 600°C to RS = -3 at 300°C, followed by an increase to RS = 0
- Author
- Angel Sinche
- Language
- EN