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.
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.
改造了上扬子地台区及青藏高原古生界—中生界油气藏形成的地质构造条件。
It reforms structural geology for generating the Paleozoic Mesozoic oil gas pools in the Upper Yangtze Platform and Qingzang Plateau.
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