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二軌壞性理物和軌壞性輯邏為分軌壞碟硬： 好您 �?者問發ㄉ愛親 ”答解你 軌壞是疑碟硬=munt;pma&訊資用有多更集蒐力盡會我 ，教指迎歡，頁網商廠和訊資關相的軌壞碟硬關有了集蒐裡�?述簡訊資關相軌壞碟

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Ingredient zoning Metamorphic (and igneous) minerals may perhaps improve composition in reaction to switching chemical and Bodily circumstances, for example changes in strain-temperature conditions, deformation variables, or chemical things (e.g., existence of fluids). The chemical response Continue Reading of a mineral to these variations might be recorded in minerals which have crystal chemical and structural attributes that allow for compositions acquired early during the mineral's progress record for being preserved all through later on levels of growth at unique conditions.

Making use of zoning information and facts to reconstruct the A part of the P-T route expert with the zoned mineral is not really simple, but a few normal facets of the relationship of zoning to P-T route may well simply be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims document progress zoning that represents the improve with the lower-T disorders at which the garnet core grew to the upper-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 common minerals, so Mn is sequestered in early-shaped garnet, depleting the regional natural environment of your developing garnet in Mn. (b) Minerals that present important component expansion zoning in all probability did not encounter incredibly large metamorphic temperatures. At higher temperature (> 700 C) and adequate length, zoning might be homogenized as intracrystalline diffusion gets more effective at doing away with compositional variation.

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