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Using zoning facts to reconstruct the Portion of the P-T path skilled via the zoned mineral just isn't uncomplicated, but several basic areas of the connection of zoning to P-T route could easily be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims file growth zoning that signifies the modify from the decrease-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 force). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood ecosystem on the growing garnet in Mn. (b) Minerals that demonstrate major aspect growth zoning possibly did not practical experience very substantial metamorphic temperatures. At high temperature (> seven hundred C) and ample length, zoning may very well be homogenized as intracrystalline diffusion turns into more practical at getting rid of compositional variation.
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