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abihsoT是個， T hcatiH是個碟硬的�?碟硬取讀法無也卻盒接外他其到裝顆單出取我 能可這述上有否是知不，定設過動沒�?述

Working with zoning facts to reconstruct the Component of the P-T route seasoned because of the zoned mineral will not be uncomplicated, but some normal areas of the connection of zoning to P-T path may possibly conveniently be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims file progress zoning that represents the alter from your decreased-T circumstances at which the garnet core grew to the higher-T conditions at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and force). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-fashioned garnet, depleting the community setting in the developing garnet in Mn. (b) Minerals that display important aspect growth zoning in all probability did not knowledge really large metamorphic temperatures. At superior temperature (> seven hundred C) and adequate period, zoning can be homogenized as intracrystalline diffusion turns into more effective at getting rid of compositional variation.

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