The 2-Minute Rule for 台北硬碟救援

An unzoned mineral that is often zoned at small-medium metamorphic grades has either skilled large temperature problems or was under no circumstances zoned (owing to a straightforward reaction history at restricted P-T or to development totally at substantial-T). Response textures Some metamorphic rocks consist of proof for incomplete reactions or other textural proof for Element of the P-T path. A simple example will be the partial substitute of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural proof may additionally be valuable in scenarios wherever the reactants are actually wholly eaten if the shape of a number of reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An illustration of a more complex response texture entails the development of website coronas , which encompass one or more shells (rims, moats) of the mineral or minerals all-around a central (reactant) phase (Fig. 6e). In lots of scenarios, coronas also require the wonderful-scale intergrowth of minerals inside a texture called symplectite (Figs. 6e-file).

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of a metamorphic rock may be the set of all P-T problems expert by a rock all through its metamorphic history (Figure 1).

At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or little) more response befell because the rock cooled and decompressed en route to the Earth's floor.

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