台北硬碟救援 - An Overview

An unzoned mineral that is typically zoned at minimal-medium metamorphic grades has both expert superior temperature disorders or was by no means zoned (owing to a simple reaction historical past at constrained P-T or to expansion solely at superior-T). Response textures Some metamorphic rocks contain evidence for incomplete reactions or other textural evidence for Portion of the P-T path. An easy illustration could be the partial substitution of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural proof could also be useful in cases exactly where the reactants happen to be entirely consumed if the shape of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An example of a far more intricate reaction texture consists of the formation of 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 instances, coronas also contain the fantastic-scale intergrowth of minerals inside of more info a texture generally known as symplectite (Figs. 6e-f).

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Element zoning Metamorphic (and igneous) minerals may perhaps transform composition in reaction to modifying chemical and physical disorders, for instance alterations in stress-temperature conditions, deformation variables, or chemical elements (e.g., presence of fluids). The chemical response of a mineral to these modifications could be recorded in minerals that have crystal chemical and structural attributes that make it possible for compositions obtained early from the mineral's advancement record to be preserved during later stages of growth at various circumstances.

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