An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has either seasoned significant temperature disorders or was never zoned (owing to a simple reaction historical past at constrained P-T or to expansion solely at higher-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other te
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An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has both seasoned superior temperature disorders or was by no means zoned (owing to a simple reaction historical past at minimal P-T or to expansion solely at superior-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or other textur
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