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paths The idealized check out of P-T paths is the fact that mineral assemblages equilibrate at every phase of The trail with Click This Link the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic things relevant to the energetics of nucleation and expansion of minerals, Though these elements can be vital for some metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T problems equivalent to the stability area of sillimanite illustrates which the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its steadiness subject. It is vital to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain Electrical power) may well aid reactions.

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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