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A couple of typical strategies for inferring P-T path segments are: Mineral inclusions Some minerals include inclusions

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Crystals which have distinctive locations with diverse compositions are zoned . A Click This Link quite common zoning sample includes a big difference in composition of a mineral's center (Main) as compared to its rim, and concentric rings of different compositions organized involving the Main as well as the rim (Fig. 5). Minerals that typically show such a zoning in the most important or trace aspects are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are related to research of metamorphic P-T paths, and zircon is relevant to resolve with the timing of petrologic functions.

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