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.

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红河断裂带两侧古地磁结果表明，羌塘地体与扬子地台至少从早白垩世以来已连接为一个整体。

Paleomagnetic results from the both sides of Honghe fault zone have shown that the Yangzi block has been united with the Qiangtang terrane since Cretaceous.

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扬子(地台)东南缘，自江西乐平向北一直缺少上、下古生界之间角度不整合接触关系的报道。

Unconformity between the Upper and Lower Paleozoic is absent from Leping of Jiangxi all the way upward, on the southeastern margin of the Yangtze platform.

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