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Working with zoning information and facts to reconstruct the A part of the P-T path expert via the zoned mineral is not straightforward, but some typical aspects of the relationship of zoning to P-T path may possibly quickly be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims record development zoning that represents the transform within the lower-T situations 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-formed garnet, depleting the neighborhood setting with the escalating garnet in Mn. (b) Minerals that show significant component progress zoning in all probability didn't working experience very high metamorphic temperatures. At higher temperature (> 700 C) and adequate length, zoning could possibly be homogenized as intracrystalline diffusion will become more practical at doing away with compositional variation.
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