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一九四五年,黄汲清教授在《中国主要地质构造单位》一书中,把吉林省北部地槽区划为古亚洲构造域天山——兴安地槽区的吉黑褶皱系和内蒙——大兴安岭褶皱系。然而,从六十年代以来,由于区域地质工作的不断深入,积累了丰富的区域地质资料。笔者在中国地质科学院任纪舜、姜春发同志的具体指导下,于1981-1984年对吉林省及其邻区前人积累的区域地质资料进行了综合分析研究,认为吉林省北部地槽区是以递进式转化的华力西地槽(早) 印支褶皱带。
In 1945, Professor Huang Jiqing, in “China’s Major Geological Structure Unit,” divides the northern part of Jilin Province into the Jihei fold system of the Tianshan-Xing’an Trough area of the ancient Asian tectonics and the Inner Mongolia- Daxinganling folds Department. However, since the 1960s, due to the deepening of regional geological work, a wealth of regional geological data has been accumulated. Under the specific guidance of Comrade Ji Jishun and Jiang Chunfa of the Chinese Academy of Geological Sciences, the author conducted a comprehensive analysis of the regional geological data accumulated by Jilin and its predecessors in 1981-1984 and concluded that the geo-trough area in the northern part of Jilin Province is a Transformed Variscan trough (Early) Indosinian fold belt.