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| | Regional Metamorphism |
 | | It is nearly pure albite in the chlorite and biotite zones, and becomes somewhat more calcic (oligoclase) in higher grade zones. |
 | | Chlorite, sericite, quartz, albite, magnetite, ±garnet (highest grade greenschist facies). |
 | | In 1961, Miyashiro noted that in the cicumpacific region, belts of high pressure, low temperature metamorphism on the oceanic side were associated with belts of high pressure, high temperature metamorphism on the continent side. |
| www.tulane.edu /~sanelson/geol212/regionalmetamorph.htm (2430 words) |
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