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Making use of zoning information and facts to reconstruct the Element of the P-T path seasoned because of the zoned mineral is just not straightforward, but a handful of standard aspects of the connection of zoning to P-T path may well very easily be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims file growth zoning that signifies the transform in the lessen-T situations at which the garnet Main grew to the higher-T conditions at which the garnet rim grew (i.e., prograde metamorphism involving escalating temperature and tension). Mn is preferentially partitioned into garnet relative to most other widespread minerals, so Mn is sequestered in early-formed garnet, depleting the regional atmosphere with the expanding garnet in Mn. (b) Minerals that demonstrate significant aspect growth zoning in all probability did not working experience quite substantial metamorphic temperatures. At large temperature (> 700 C) and sufficient length, zoning may be homogenized as intracrystalline diffusion becomes more effective at reducing compositional variation.
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