hydrothermal metamorphism
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
- hydrothermal mineral deposit
- metamorphism
- metamorphic rock - Hydrothermal metamorphism
- metamorphic rock - Reactions of other mineral systems
- metamorphic rock - Classification into four chemical systems
- igneous rock - Pegmatites and late-stage mineralization
- rock - Thermal expansion
- metamorphic rock - Temperature
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