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hydrothermal metamorphism

geology

Quick Summary

Hydrothermal metamorphism involves changes in rocks near the Earth's surface due to intense activity of hot water. This process is driven by circulating groundwaters heated by proximity to igneous materials, radioactive decay, or faulting.123

Key factors for hydrothermal metamorphism include:
* Hot water: Dissolves and transports minerals.2
* Interconnected openings: Allows solutions to move through rocks.2
* Sites for deposition: Locations where minerals can precipitate.2
* Chemical reactions: Triggered by boiling, temperature drops, mixing with cooler solutions, or reactions with the rock itself.2

Hydrothermal solutions can fill cavities or replace rocks, forming mineral deposits. This process is significant in areas like Yellowstone National Park and can lead to extreme migration of chemical elements and mineral concentration.21

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