There are various indications that the Liuling Group belongs to the stable continental margin deposits of the north of the Yangtse plate.
冬种迹象表明，刘岭群应属扬子板块北部的稳定大陆边缘沉积。
Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.
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。
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