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A couple of frequent approaches for inferring P-T route segments are: Mineral inclusions Some minerals consist of inclusions
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Some inclusions Never have lots of details about P-T conditions as the minerals are steady more than these types of a wide array of situations (as an example: quartz). Other mineral inclusions are very handy for inferring P-T problems and path segments, particularly when these minerals now not exist during the matrix on the rock (which is, outside the garnet).
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