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of the metamorphic rock is the list of all P-T disorders knowledgeable by a rock during its metamorphic heritage (Figure 1).

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Working with zoning information to reconstruct the A part of the P-T route expert via the zoned mineral is not uncomplicated, but a few common facets of the connection of zoning to P-T route may perhaps effortlessly be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims record growth zoning that represents the adjust with the lessen-T conditions at which the garnet Main grew to the upper-T disorders at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and stress). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-shaped garnet, depleting the community atmosphere in the increasing garnet in Mn. (b) Minerals that exhibit important element development zoning almost certainly didn't experience very large metamorphic temperatures. At large temperature (> seven hundred C) and enough length, zoning may be homogenized as intracrystalline diffusion gets to be more effective at removing compositional variation.

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