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Therefore, Even though subduction zone rocks can comply with a variety of paths through subduction and exhumation, analyzing the precise route that a specific exhumed subduction zone rock adopted is very important for being familiar with subduction dynamics.

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Crystals which have distinctive locations with different compositions are zoned . A quite common zoning pattern will involve a variation in composition of a mineral's center (Main) when compared with its rim, and concentric rings of various compositions arranged involving the Main along with the rim (Fig. 5). Minerals that normally display this type of zoning in the major or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of such, garnet and plagioclase are appropriate to research of metamorphic P-T paths, and zircon is suitable to dedication of the timing of petrologic activities.

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