The 2-Minute Rule for 台北硬碟救援



An unzoned mineral that is often zoned at lower-medium metamorphic grades has either experienced higher temperature situations or was under no circumstances zoned (owing to an easy response record at constrained P-T or to expansion solely at superior-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or other textural evidence for Portion of the P-T path. An easy illustration could be the partial substitution of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural proof may also be helpful in instances in which the reactants are already fully eaten if The form of a number of reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a far more elaborate response texture will involve the development of coronas , which encompass a number of shells (rims, moats) of the mineral or minerals all-around a central (reactant) section (Fig. 6e). In several conditions, coronas also contain the fine-scale intergrowth of minerals in a texture known read more as symplectite (Figs. 6e-f).

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Several frequent approaches for inferring P-T route segments are: Mineral inclusions Some minerals incorporate inclusions

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