台中硬碟救援 No Further a Mystery

An unzoned mineral that is often zoned at lower-medium metamorphic grades has both seasoned high temperature conditions or was under no circumstances zoned (owing to a straightforward reaction record at confined P-T or to advancement solely at higher-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural evidence for A part of the P-T path. An easy instance may be the partial alternative of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof may be handy in conditions where by the reactants have been completely consumed if the shape of one or more reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An example of a more sophisticated reaction texture includes the formation of coronas , which include one or more shells (rims, moats) of a mineral or minerals close to a central (reactant) stage (Fig. 6e). In lots of circumstances, coronas also entail the fantastic-scale intergrowth of minerals within a texture called symplectite (Figs. 6e-f).

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