台北硬碟救援 Fundamentals Explained

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Crystals which have distinctive regions with distinctive compositions are zoned . A quite common zoning pattern includes a variation in composition of a mineral's Centre (core) when compared to its rim, and here concentric rings of different compositions organized between the core as well as rim (Fig. 5). Minerals that commonly display this sort of zoning in the major or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are suitable to research of metamorphic P-T paths, and zircon is appropriate to determination in the timing of petrologic situations.

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