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The increasing garnets surrounded these relict minerals as the garnets grew, and the relict minerals are preserved as mineralogical proof of an earlier phase in the metamorphic heritage on the rock.

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Working with zoning data to reconstruct the A part of the P-T route knowledgeable by the zoned mineral will not be easy, but some basic 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 change through the reduce-T disorders at which the garnet core grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and strain). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-shaped garnet, depleting the nearby natural environment from the escalating garnet in Mn. (b) Minerals that present important component growth zoning possibly didn't expertise very substantial metamorphic temperatures. At superior temperature (> seven hundred C) and enough duration, zoning can be homogenized as intracrystalline diffusion becomes website simpler at eliminating compositional variation.

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