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For some rocks, the only real Component of the P-T route recorded within the mineral assemblage and texture of the rock is definitely the 'peak' of metamorphism -- the problems with the thermal most (i.e., the most temperature as well as the stress at the most temperature). If your rock had a sedimentary or volcanic protolith, you are able to infer which the rock started off with the surface, arrived at peak problems at some temperature and depth inside the Earth, and returned towards the area (the place the rock was collected).

Crystals that have distinctive areas with different compositions are zoned . A quite common zoning sample requires a change in composition of here a mineral's Centre (core) as compared to its rim, and concentric rings of different compositions organized in between the Main and the rim (Fig. five). Minerals that ordinarily present such a zoning in the main or trace things are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of those, garnet and plagioclase are relevant to scientific studies of metamorphic P-T paths, and zircon is applicable to dedication with the timing of petrologic occasions.

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