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Consequently, Even though subduction zone rocks can adhere to numerous paths throughout subduction and exhumation, identifying the specific path that a specific exhumed subduction zone rock followed is essential for comprehension subduction dynamics.
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Making use of zoning information and facts to reconstruct the Section of the P-T path knowledgeable because of the zoned mineral is not really very simple, but several general components of the connection of zoning to P-T route could easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims record expansion zoning that represents the transform in the decrease-T problems at which the garnet core grew to the upper-T problems at which the garnet rim grew (i.e., prograde metamorphism involving increasing 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 neighborhood atmosphere in the escalating garnet in Mn. (b) Minerals that present important factor advancement zoning almost certainly didn't experience incredibly higher metamorphic temperatures. At significant temperature (> 700 C) and enough period, zoning could be homogenized as intracrystalline diffusion turns into more practical at removing compositional variation.
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