Hydrothermal Alteration
The interaction between the circulating thermal fluids and rocks results in water-rock reactions that produce assemblages of secondary (hydrothermal) minerals that are often used as a guide to present or past subsurface temperatures and fluid type. Permeability and porosity of the host rock strongly influence the water-to-rock volumetric ratio and the degree to which the original minerals are altered. The suit of secondary minerals is less controlled by rock type than by temperature and composition of the fluids (Browne, 1978). Read more…

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