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中国东北部陆缘地处华北地台东部、中亚造山带东段,西太平洋大陆边缘的北端,是我国内生金矿床较为发育的地区之一,以其成矿作用复杂、蕴藏丰富的金资源量备受国内外经济地质学家关注和研究。前人曾对该区的各类典型金矿床进行了地质、地球化学特征、成岩及成矿时代等方面的系统研究(邓晋福等,1994;毛景文等,2000,2005;吴福元等,1999,2003;王义文等,
The continental margin of Northeast China is located in the eastern part of North China Platform, the eastern section of the Central Asian orogenic belt and the northern end of the western Pacific margin. It is one of the more developed endogenous gold deposits in China. Due to its complicated metallogenesis and abundant gold Resources have been domestic and foreign economic geologists attention and research. The predecessors have carried out systematic studies on the geological and geochemical characteristics, diagenesis and metallogenic epoch of various typical gold deposits in the area (Deng Jinfu et al., 1994; Mao Jingwen et al., 2000, 2005; Wu Fuyuan et al., 1999, 2003 ; Wang Yiwen, etc.,