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A couple of common procedures for inferring P-T path segments are: Mineral inclusions Some minerals comprise inclusions
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Some inclusions Really don't have lots of specifics of P-T problems because the minerals are stable around these kinds of an array of disorders (by way of example: quartz). Other mineral inclusions are incredibly helpful for inferring P-T disorders and path segments, especially if these minerals no more exist inside the matrix of the rock (that is definitely, outdoors the garnet).
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