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根据水准测量的结果以及地层、岩石、矿物方面的地质证据对华北与扬子地块的拼合界线和郯庐断裂的性质进行了讨论。
Based on the results of the leveling survey and geological evidences of stratigraphy, rock and mineral, the boundary between the north China and the Yangtze block and the nature of the Tanlu fault are discussed.