辽东半岛南部变质核杂岩构造展布于旅顺、大连、金州、庄河、普兰店地区。

The metamorphic core-complex structure distributed in Lushun-Dalian-Jinzhou-Zhuanghe-Pulandian area in the south of Liaodong Peninsula.

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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.

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不少学者用变质核杂岩模式解释豫西后造山阶段的基底隆起和与之相伴的盆岭构造的构造格局。

Using metamorphic core complex (MCC) models, many geologists interpret the tectonic framework featuring the basement dome and the basin-and-range tectonics in western Henan in the postorogenic stage.

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