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Thus, Though subduction zone rocks can adhere to many paths for the duration of subduction and exhumation, deciding the specific path that a selected exhumed subduction zone rock adopted is essential for knowledge subduction dynamics.

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Crystals that have different areas with distinctive compositions are zoned . A very common zoning sample entails a variance in composition of a mineral's Centre (core) as compared to its rim, and concentric rings of different compositions organized between the Main and also the rim (Fig. five). Minerals that typically present such a zoning in the key or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are related to reports of metamorphic P-T paths, and zircon is relevant to willpower of your timing of petrologic activities.

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