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Applying zoning data to reconstruct the Component of the P-T path professional by the zoned mineral is just not straightforward, but some typical components of the connection of zoning to P-T path may possibly easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims document expansion zoning that represents the modify within the decrease-T conditions at which the garnet Main grew to the upper-T situations 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 popular minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood ecosystem in the escalating garnet in Mn. (b) Minerals that show key element progress zoning probably did not working experience really substantial metamorphic temperatures. At superior temperature (> seven hundred C) and ample duration, zoning can be homogenized as intracrystalline diffusion becomes simpler at getting rid of compositional variation.
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