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For many rocks, the sole A part of the P-T path recorded during the mineral assemblage and texture on the rock may be the 'peak' more info of metamorphism -- the circumstances of the thermal most (i.e., the utmost temperature as well as the pressure at the most temperature). In case the rock had a sedimentary or volcanic protolith, you can infer which the rock started out in the area, achieved peak situations at some temperature and depth within the Earth, and returned into the floor (in which the rock was gathered).
Crystals that have various areas with various compositions are zoned . A quite common zoning pattern involves a variance in composition of the mineral's Middle (core) compared to its rim, and concentric rings of various compositions organized involving the Main and the rim (Fig. five). Minerals that ordinarily exhibit this sort of zoning in the key or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of such, garnet and plagioclase are related to studies of metamorphic P-T paths, and zircon is appropriate to perseverance on the timing of petrologic activities.
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for the reason that we would like as much P-T route data as you possibly can, In order in order to interpret the thermal/tectonic processes and heritage too as possible. This is certainly negative
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