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Working with zoning information and facts to reconstruct the A part of the P-T path expert by the zoned mineral is not straightforward, but a number of typical aspects of the relationship of zoning to P-T path may well simply be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims record growth zoning that represents the adjust with the lower-T circumstances at which the garnet core grew to the upper-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and pressure). Mn is preferentially partitioned into garnet relative to most other typical minerals, so Mn is sequestered in early-shaped garnet, depleting the regional natural environment of your expanding garnet in Mn. (b) Minerals that present key aspect advancement zoning probably did not encounter really substantial metamorphic temperatures. At substantial temperature (> seven-hundred C) and adequate length, zoning might be homogenized as intracrystalline diffusion gets to be more practical at reducing compositional variation.
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