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Applying zoning data to reconstruct the A part of the P-T route skilled via the zoned mineral just isn't very simple, but a number of general areas of the relationship of zoning to P-T route could conveniently be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims history progress zoning that represents the adjust in 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 frequent minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood ecosystem in the escalating garnet in Mn. (b) Minerals that present important ingredient development zoning in all probability did not experience pretty significant metamorphic temperatures. At substantial temperature (> seven-hundred C) and enough length, zoning may be homogenized as intracrystalline diffusion gets more effective at removing compositional variation.

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