The smart Trick of 台中硬碟救援 That No One is Discussing

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For some rocks, the one A part of the P-T route recorded during the mineral assemblage and texture on the rock is the 'peak' of metamorphism -- the situations with the thermal highest (i.e., the most temperature and also the force at the maximum temperature). In case the rock experienced a sedimentary or volcanic protolith, you'll be able to infer which the rock began with the surface, attained peak ailments at some temperature and depth in the Earth, and returned on the area (exactly where the rock was gathered).

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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at each and every stage of the path from the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic aspects associated with the energetics of nucleation and growth of minerals, Whilst these things could possibly be crucial for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T read more situations equivalent to the stability industry of sillimanite illustrates the sluggish kinetics on the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its steadiness subject. It is vital to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain energy) may perhaps aid reactions.

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