5 Essential Elements For 台北硬碟救援

An unzoned mineral that is typically zoned at minimal-medium metamorphic grades has both expert superior temperature circumstances or was under no circumstances zoned (owing to a straightforward response history at minimal P-T or to expansion entirely at superior-T). Response textures Some metamorphic rocks have evidence for incomplete reactions or other textural proof for Section of the P-T route. An easy example would be the partial alternative of andalusite by sillimanite (Fig. 6a) from the polymorphic transformation of andalusite to sillimanite. Textural proof may additionally be helpful in conditions the place the reactants happen to be wholly consumed if the shape of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An illustration of a more complex response texture requires the development of coronas , which include one or more shells (rims, moats) of the mineral or minerals all around a central (reactant) stage (Fig. 6e). In several circumstances, coronas also involve the high-quality-scale intergrowth of minerals within a texture often known as symplectite (Figs. 6e-file).

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compared to situations of the height of metamorphism symbolize disequilibrium. Usually, on the other hand, the evidence for disequilibrium can be extremely practical since it can be read more employed to reconstruct P-T path segments.