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Crystals which have various areas with distinct compositions are zoned . A quite common zoning sample consists of a change in composition of the mineral's center (core) in comparison to its rim, and concentric rings of different compositions arranged amongst the Main plus the rim (Fig. five). Minerals that ordinarily show this type of zoning in the major or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, å°ä¸ç¡¬ç¢Ÿæ•‘æ´ garnet and plagioclase are pertinent to reports of metamorphic P-T paths, and zircon is appropriate to dedication in the timing of petrologic gatherings.
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simply because we would like just as much P-T path data as feasible, so as in order to interpret the thermal/tectonic processes and record likewise as is possible. This can be bad
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