An Unbiased View of 台北硬碟救援

An unzoned mineral that is often zoned at minimal-medium metamorphic grades has both expert superior temperature problems or was never zoned (owing to a simple response heritage at confined P-T or to growth entirely at high-T). Reaction textures Some metamorphic rocks include proof for incomplete reactions or other textural evidence for Portion of the P-T route. A straightforward case in point is definitely the partial alternative of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof could also be useful in instances exactly where the reactants have already been totally eaten if the shape of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a far more complicated response texture consists of the development of coronas , which include a number of shells (rims, moats) of a mineral or minerals around a central (reactant) phase (Fig. 6e). In lots of cases, coronas also involve the wonderful-scale intergrowth of minerals in the texture often known as symplectite (Figs. Click Here 6e-f).

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