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For some rocks, the sole Element of the P-T path recorded during the mineral assemblage and texture from the rock could be the 'peak' of metamorphism -- the conditions on the thermal most (i.e., the maximum temperature plus the strain at the maximum temperature). In the event the rock experienced a sedimentary or volcanic protolith, you can infer that Continued the rock started off in the area, reached peak circumstances at some temperature and depth within the Earth, and returned for the area (exactly where the rock was gathered).

Crystals which have various locations with various compositions are zoned . A quite common zoning pattern includes a distinction in composition of the mineral's center (Main) in comparison to its rim, and concentric rings of various compositions arranged involving the core plus the rim (Fig. 5). Minerals that generally show this sort of zoning in the foremost or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of those, garnet and plagioclase are relevant to reports of metamorphic P-T paths, and zircon is appropriate to determination of the timing of petrologic functions.

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