is the result of dynamic metamorphism of granite
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granite, by metamorphism during rock flowage, may become a mica schist or mica gneiss. Mica is increased at the expense of the feldspar and some of the ferromagnesian minerals.
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Granite, by metamorphism during rock flowage, may become a mica schist or mica gneiss. Mica is increased at the expense of the feldspar and some of the ferromagnesian minerals.
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