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Some inclusions Really don't incorporate many specifics of P-T conditions because the minerals are steady in excess of these a wide array of circumstances (for instance: quartz). Other mineral inclusions are quite handy for inferring P-T disorders and route segments, particularly when these here minerals now not exist from the matrix of your rock (that may be, outside the garnet).
At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or small) further response occurred as the rock cooled and decompressed en path to the Earth's area.
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