江苏下扬子区的海相中—古生界构造演化经历了前扬子板块、稳定地台和西太平洋活动陆缘等三大阶段。
Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.
显生宙期间，中国南部的构造属性曾几经转化。
The tectonic nature of southern China has Changed again and again in the Phanerozoic.
叠加褶皱与拼接带具有成生联系，且各自代表了不同构造部位的变形特点。
Therefore, the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in different structural positions.
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