Metamorphic reaction
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]
Schematic representation of a metamorphic reaction. Abbreviations of minerals: act = actinolite; chl = chlorite; ep = epidote; gt = garnet; hbl = hornblende; plag = plagioclase. Two minerals represented in the figure do not participate in the reaction, they can be quartz and K-feldspar. This reaction takes place in nature when a mafic rock goes from amphibolite facies to greenschist facies.
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
Schreinemakers Method
Reaction Mechanisms
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gollark: There are some HTTP *1.0* requests too.
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gollark: ```<86.186.223.37> 104.199.36.222 [11/Jun/2020:08:37:45 +0000] "GET / HTTP/1.1" 404 153 "-" "python-requests/2.23.0" secure<86.186.223.37> 192.35.168.215 [11/Jun/2020:07:11:47 +0000] "GET / HTTP/1.1" 404 153 "-" "Mozilla/5.0 zgrab/0.x" secure```Interesting user agents here.
See also
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