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Crystals that have distinct areas with distinctive compositions are zoned . A quite common zoning pattern entails a variance in composition of the mineral's Heart (core) in comparison with its rim, and concentric rings of different compositions organized in between the core plus the rim (Fig. 5). Minerals that normally show this kind of zoning in the most important or trace factors are garnet, plagioclase, zircon, click here and tourmaline (Fig. five). Of such, garnet and plagioclase are pertinent to scientific tests of metamorphic P-T paths, and zircon is appropriate to determination with the timing of petrologic occasions.
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