变质核杂岩是构造上被低角度正断层拆离的、呈孤立的平缓穹形或拱形强烈变形的变质岩和侵入岩构成的隆起，往往出现在造山带的核部。
Meanwhile, its emplacement is closely related to the Liaonan metamorphic core complex, so this point provides an uncommon opportunity to studying the tectonic mechanism of the early Cretaceous magmatism.
同时，该花岗岩的侵位与辽南变质核杂岩密切相关，这为我们研究早白垩世岩浆活动的构造体制提供了难得的机会。
参考来源 - 中国东部早白垩世岩浆作用的伸展构造背景—以辽东半岛南部饮马湾山岩体为例·2,447,543篇论文数据，部分数据来源于NoteExpress
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.
江浪铜矿田位于扬子地台西缘江浪变质核杂岩穹隆构造中。
The Jianglang copper deposit is hosted in the extension ductile shear zones of the Jianglang metamorphic core complexes in southwestern margin of Yangtze platform.
李伍富铜矿床赋存在江浪变质核杂岩之中，矿化受滑脱断层控制。
The Liwu copper-rich deposit is located in the Jianglang metamorphic core complex, and its mineralization is controlled by slide surface.
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