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遂安石的微结构主要表现为位错、相畴及调置结构，这些结构反映了矿床变质作用的热历史，这一过程表现为升温及升温后的退火作用。
The microstructure of Sui’an rock is mainly composed of dislocations, phase domains and tuned structures. These structures reflect the thermal history of the metamorphism of the deposit. This process is characterized by the effects of heating and post-heating annealing.