台中硬碟救援 Fundamentals Explained

An unzoned mineral that is often zoned at small-medium metamorphic grades has either knowledgeable substantial temperature ailments or was hardly ever zoned (owing to a simple reaction background at constrained P-T or to progress fully at superior-T). Response textures Some metamorphic rocks contain proof for incomplete reactions or other textural proof for Component of the P-T route. A straightforward example will be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof may be helpful in situations wherever the reactants have been entirely consumed if the shape of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a far more intricate response texture entails the development of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals all around a central (reactant) section (Fig. 6e). In lots of circumstances, coronas also require the good-scale intergrowth of minerals inside of a texture called symplectite (Figs. 6e-file).

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