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Applying zoning data to reconstruct the A part of the P-T route knowledgeable by the zoned mineral will not be easy, but a handful of standard elements of the connection of zoning to P-T path may perhaps effortlessly be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims record expansion zoning that represents the transform in the lessen-T situations at which the garnet Main grew to the higher-T disorders at which the garnet rim grew (i.e., prograde metamorphism involving escalating temperature and pressure). Mn is preferentially partitioned into garnet relative to most other widespread minerals, so Mn is sequestered in early-formed garnet, depleting the community atmosphere with the escalating garnet in Mn. (b) Minerals that clearly show major factor growth zoning probably didn't practical experience quite higher metamorphic temperatures. At superior temperature (> 700 C) and ample period, zoning can be homogenized as intracrystalline diffusion will become more effective at eliminating å°ä¸ç¡¬ç¢Ÿæ•‘æ´ compositional variation.
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