Details, Fiction and 台中硬碟救援

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A number of prevalent solutions for inferring P-T route segments are: Mineral inclusions Some minerals comprise inclusions

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paths The idealized view of P-T paths is usually that mineral assemblages equilibrate at just about every phase of the path from the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This see ignores kinetic factors connected to the energetics of nucleation and expansion of minerals, Despite the fact that these aspects might be important for many metamorphic phases and reactions. One example is, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T conditions comparable to The soundness area of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its steadiness discipline. It's important to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain Electrical power) may well help reactions.

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