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The length of the path from start off (onset of metamorphism) to finish (exposure in the rock within the Earth's surface area) will differ from rock to rock with regards to the tectonic record

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Employing zoning information to reconstruct the Element of the P-T path experienced with the zoned mineral isn't very simple, but a number of general areas of the relationship of zoning to P-T route could conveniently be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims record expansion zoning that represents the transform from your lessen-T situations at which the garnet core grew to the upper-T conditions at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and stress). Mn is preferentially partitioned into garnet relative to most other prevalent minerals, so Mn is sequestered in early-formed garnet, depleting the community ecosystem on the growing garnet in Mn. (b) Minerals that display major element growth zoning possibly didn't encounter extremely superior metamorphic temperatures. At superior temperature (> 700 C) and enough duration, here zoning can be homogenized as intracrystalline diffusion becomes simpler at doing away with compositional variation.

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