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An unzoned mineral that is usually zoned at small-medium metamorphic grades has either skilled large temperature ailments or was hardly ever zoned (owing to a simple reaction historical past at confined P-T or to expansion fully at high-T). Response textures Some metamorphic rocks include proof for incomplete reactions or other textural evidence for Component of the P-T route. An easy case in point is definitely the partial substitution of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be beneficial in circumstances where by the reactants are actually completely consumed if the shape of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a more sophisticated reaction texture will involve the development of coronas , which encompass a number of shells (rims, moats) of the mineral or minerals around a central (reactant) phase (Fig. 6e). In several cases, coronas also involve the fine-scale intergrowth of minerals inside a texture referred to as symplectite (Figs. 6e-f).

硬碟 損傷傷損理物了生產上軌磁碟硬的你示表:述簡復修的軌道壞與用使確正的碟硬.速快用後區輯邏個一為作間空碟硬的剩所將再，區分輯邏的決解來況情用使的區扇或區分碟硬改更過通能只，傷損理物了生產上軌磁碟硬的你示表:述簡)道知要定一但，論大篇長(養保及常異的碟硬.頭磁後以，了好修被快很就碟硬的軌壞理物重嚴有個一，啟重

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In Figure 3, kyanite inclusions arise in garnet in a very rock which includes only sillimanite in the matrix, indicating the rock was Check Out Your URL Earlier from the kyanite steadiness area but that P-T situations transformed. In the event the matrix of your rock (including the garnet rim) equilibrated, the rock was inside the silliminate steadiness field (Fig. 4).

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