Metamorphic reaction
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A metamorphic reaction is a chemical reaction that takes place during the geological process of metamorphism wherein one assemblage of minerals is transformed into a second assemblage which is stable under the new temperature/pressure conditions resulting in the final stable state of the observed metamorphic rock.[1]
Examples include the production of talc under varied metamorphic conditions:
- serpentine + carbon dioxide → talc + magnesite + water
- chlorite + quartz → kyanite + talc + water
Polymorphic transformations
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Exsolution reactions
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Devolatilization reactions
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Continuous reactions
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Ion exchange reactions
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Oxidation/reduction reactions
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Reactions involving dissolved species
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Chemographics
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Petrogenetic grids
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Schreinemaker's method
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Reaction mechanisms
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See also
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[edit ]- ^ "Types of Metamorphic Reactions". Tulane University. Retrieved 2007年06月22日.