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An unzoned mineral that is often zoned at low-medium metamorphic grades has either skilled large temperature problems or was hardly ever 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 route. A simple example will be the partial alternative of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof could also be practical in cases where the reactants happen to be totally consumed if the shape of one or more reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An example of a more intricate response texture includes the formation of coronas , which include one or more shells (rims, moats) of the mineral or minerals close to a central (reactant) phase (Fig. 6e). In several cases, coronas also entail the high-quality-scale intergrowth of minerals within a texture often called symplectite (Figs. 6e-file).

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The length of the path from start off (onset of metamorphism) to finish (publicity of the rock with the Earth's area) will vary from rock to rock depending on the tectonic historical past

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仔建抖帥�?~惜惜練教 :章文的趣興有能可您 。賽出再法無定確季本,健復刀開傷手因卻但,手投援救力主任擔隊磯落多拉羅科在輝錦曹,季球年 。

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