In geochemistry, 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. Examples include the production of talc under varied metamorphic conditions:
serpentine + carbon dioxide → talc + magnesite + water chlorite + quartz → kyanite + talc + water
Polymorphic transformations
Exsolution reactions
Devolatilization reactions
Continuous reactions
Ion exchange reactions
Oxidation/reduction reactions
Reactions involving dissolved species
Chemographics
Petrogenetic grids
Schreinemaker's method
Reaction mechanisms
See also Index mineral
Notes



