台北硬碟救援 - An Overview

An unzoned mineral that is often zoned at very low-medium metamorphic grades has either professional substantial temperature circumstances or was hardly ever zoned (owing to an easy response historical past at restricted P-T or to growth entirely at higher-T). Reaction textures Some metamorphic rocks contain proof for incomplete reactions or other textural evidence for Portion of the P-T path. A straightforward illustration may be the partial replacement of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof can also be helpful in instances where by the reactants are entirely consumed if the shape of a number of reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An illustration of a more sophisticated response texture involves the formation of coronas , which encompass a number of shells (rims, moats) of the mineral or minerals about a central (reactant) period (Fig. 6e). In lots of cases, coronas also entail the good-scale intergrowth of minerals within a texture often known as symplectite (Figs. 6e-file).

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of other minerals. For example, garnets typically incorporate read more inclusions of minerals which were present within the rock matrix since the garnet grew, but which were not wholly eliminated by metamorphic reactions in the course of progressive metamorphism.

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