The Greatest Guide To 台北硬碟救援



An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has either seasoned large temperature problems or was under no circumstances zoned (owing to a straightforward response history at confined P-T or to advancement totally at higher-T). Response textures Some metamorphic rocks incorporate proof for incomplete reactions or other textural proof for Component of the P-T route. An easy instance is the partial substitution of andalusite by sillimanite (Fig. 6a) from the polymorphic transformation of andalusite to sillimanite. Textural proof can also be beneficial in situations where by the reactants happen to be entirely eaten if the shape of one or more reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An example of a more advanced response texture will involve the development of coronas , which encompass a number of shells (rims, moats) of the mineral or minerals around a central (reactant) phase (Fig. 6e). In many instances, coronas also include the good-scale intergrowth of minerals within a texture generally known as symplectite (Figs. 6e-file).

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