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A couple of typical strategies for inferring P-T path segments are: Mineral inclusions Some minerals have inclusions
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Crystals which have different areas with distinctive compositions are zoned . A very common zoning sample requires a change in composition of a mineral's Centre (core) when compared to its rim, and concentric rings of different compositions arranged amongst the Main as well as the rim (Fig. five). Minerals that typically demonstrate this type of zoning in the most important or trace Do you agree elements are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are related to scientific tests of metamorphic P-T paths, and zircon is applicable to dedication in the timing of petrologic gatherings.
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