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The trajectory and condition on the P-T path, the rates of metamorphic procedures, along with the length of metamorphism really are a functionality with the supply of warmth as well as mechanisms of burial and unroofing (if tension change is concerned).

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Some inclusions don't comprise a great deal of details about P-T conditions as the minerals are stable around these an array of conditions (one example is: quartz). Other mineral inclusions are incredibly useful for inferring P-T ailments and path segments, particularly when these minerals no more exist inside the matrix of your rock (that is certainly, outside the garnet).

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