变质核杂岩是大陆流变伸展的重要表现形式。
The metamorphic core complex is an important rheologic pattern of continental extension.
赣湘地区的变质核杂岩和变质穹窿构造中，晚期脆性断裂与早期低序次韧性构造间存在着明显的相关联系。
In the metamorphic core complex (MCC) and the metamorphic arch, Jiangxi and Hunan area, there is an obvious correlation between the late brittle fault and the early subordinate ductile structure.
对该变质核杂岩的研究，将对滇东南地区的地壳演化认识及矿田勘查有重要意义。
The study of the metamorphic core complex has important significance for the understanding of the crustal evolution and mineral exploration in southeastern Yunnan.
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