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An unzoned mineral that is typically zoned at lower-medium metamorphic grades has possibly professional high temperature circumstances or was in no way zoned (owing to a straightforward response record at restricted P-T or to development totally at significant-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or

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An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has both seasoned substantial temperature situations or was never ever zoned (owing to a straightforward response record at limited P-T or to expansion fully at significant-T). Response textures Some metamorphic rocks comprise proof for incomplete reactions or other tex