该类型构造形成于加里东期末，是该区加里东造山期后隆升背景的产物。
This kind of structure is the product under background of the uplift in Caledonian postorogenic phase formed at the end of the Caledonian Stage.
造山带核部上中地壳存在着规模很大的岩浆岩体的显示，与造山期后的地质作用有关。
The manifestations of large-scale magmatic intrusions occurring in the upper-mid crust in the cores of the orogenic belt were related to post-orogenic geological processes.
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