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Making use of zoning information and facts to reconstruct the part of the P-T path knowledgeable via the zoned mineral will not be basic, but a few standard aspects of the relationship of zoning to P-T route may perhaps effortlessly be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims document development zoning that signifies the improve within the decreased-T circumstances at which the garnet Main grew to the higher-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and tension). Mn is preferentially partitioned into garnet relative to most other typical minerals, so Mn is sequestered in early-fashioned garnet, depleting the nearby ecosystem in the escalating garnet in Mn. (b) Minerals that present important component advancement zoning probably did not practical experience extremely significant metamorphic temperatures. At higher temperature (> seven hundred C) and sufficient length, zoning may very well be homogenized as intracrystalline diffusion turns into more practical at removing compositional variation.
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