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密山——扰顺深断裂带南起沈阳,向东北经抚顺、海龙、桦甸、敦化至密山以远。基本上循浑河、辉发河、牡丹江上游及穆棱河呈北东方向延伸。1959年黄汲清教授最早启用密山——敦化大断裂和抚顺——海龙大断裂,分别代表本断裂带的南北两段;翌年合称为密山——敦化深断裂;1974年黄汲清教授进而将该断裂作为郯城——庐江断裂北延的主体部分。近几年来许多学者(徐嘉炜1978;崔克英1978;吴良士1978;彭玉鲸1879)都对本断裂的性质及成因作过研究,有的认为属郯庐
Mishan - disturbing along the deep fault zone south of Shenyang, northeast by Fushun, Hailong, Huadian, Dunhua to Mishan far. Basically Hunxi River, Hui Fa River, Mudanjiang River and Muling River northbound extension. In 1959, Professor Huang Jiqing first enabled the Mishan-Dunhua Major Fault and the Fushun-Hailong Major Fault to represent the two northern and southern sections of this fault respectively. In the following year, it was jointly known as Mishan-Dunhua Deep Fault. In 1974, The professor then regarded the fault as the main part of the northern extension of Tancheng-Lujiang fault. In recent years, many scholars (Xu Jiawei 1978; Cui Keying 1978; Wu Liangshi 1978; Peng Yu Whale 1879) have studied the nature and causes of this fault,