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An unzoned mineral that is often zoned at very low-medium metamorphic grades has both knowledgeable higher temperature problems or was hardly ever zoned (owing to a straightforward response record at constrained P-T or to advancement completely at superior-T). Response textures Some metamorphic rocks include proof for incomplete reactions or other textural evidence for part of the P-T path. A straightforward instance is the partial alternative of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural evidence may be beneficial in cases wherever the reactants have already been absolutely consumed if The form of one or more reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An illustration of a more elaborate response texture involves the development of coronas , which consist of a number of shells (rims, moats) of a mineral or minerals around a central (reactant) period (Fig. 6e). In many scenarios, coronas also include the great-scale intergrowth of minerals in the texture known here as symplectite (Figs. 6e-file).

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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 。