For that reason, Despite the fact that subduction zone rocks can observe several paths through subduction and exhumation, analyzing the precise path that a particular exhumed subduction zone rock adopted is crucial for knowledge subduction dynamics.
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Crystals which have distinct locations with unique compositions are zoned . A quite common zoning pattern entails a difference in composition of a mineral's Heart (core) when compared with its rim, and concentric rings of different compositions arranged involving the Main and the rim (Fig. Click This Link five). Minerals that ordinarily exhibit this kind of zoning in the most important or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of those, garnet and plagioclase are appropriate to scientific studies of metamorphic P-T paths, and zircon is pertinent to determination of the timing of petrologic events.
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