Considerations To Know About 台中硬碟救援

An unzoned mineral that is usually zoned at lower-medium metamorphic grades has possibly professional high temperature problems or was by no means zoned (owing to an easy response heritage at minimal P-T or to growth fully at superior-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or other textural evidence for Section of the P-T route. An easy instance may be the partial substitute of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be beneficial in circumstances the place the reactants are already wholly eaten if the shape of one or more reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An example of a more advanced reaction texture involves the development of coronas , which include one or more shells (rims, moats) of a mineral or minerals close to a central (reactant) stage (Fig. 台北硬碟救援 6e). In many cases, coronas also involve the fine-scale intergrowth of minerals inside a texture called symplectite (Figs. 6e-f).

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