The 2-Minute Rule for 台中硬碟救援

An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has both seasoned substantial temperature situations or was never ever zoned (owing to a straightforward response record at limited P-T or to expansion fully at significant-T). Response textures Some metamorphic rocks comprise proof for incomplete reactions or other textural evidence for Component of the P-T route. A straightforward case in point is the partial replacement of andalusite by sillimanite (Fig. 6a) from the polymorphic transformation of andalusite to sillimanite. Textural evidence can also be beneficial in situations where the reactants are already absolutely consumed if The form of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a far more complex reaction texture will involve the development of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals all around a central (reactant) phase (Fig. 6e). In lots of situations, coronas also entail the wonderful-scale intergrowth website of minerals within a texture generally known as symplectite (Figs. 6e-f).

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