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For a few rocks, the sole part of the P-T route recorded during the mineral assemblage and texture on the rock would be the 'peak' of metamorphism -- the situations from the thermal maximum (i.e., the most temperature and also the pressure at the most temperature). In case the rock had a sedimentary or volcanic protolith, you can infer which the rock started off with the surface area, reached peak conditions at some temperature Check This Out and depth during the Earth, and returned towards the floor (where the rock was collected).

Crystals that have distinctive areas with distinctive compositions are zoned . A quite common zoning pattern entails a variation in composition of the mineral's Middle (core) as compared to its rim, and concentric rings of different compositions organized concerning the Main plus the rim (Fig. five). Minerals that ordinarily show this type of zoning in the major or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are pertinent to experiments of metamorphic P-T paths, and zircon is appropriate to resolve in the timing of petrologic situations.

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