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柴达木盆地早已为我国石油地质工作者与大地构造学家所关注。在1955年黄汲清就指出柴达木盆地的基底是“硬化了的加里东褶皱带”;1956年张文佑认为:“柴达木基底是由太古代结晶岩系构成的,它在古生代和中生代初期可能与塔里木相连,由于燕山运动使阿尔金山沿断裂上升,二者被隔开”;1957年朱夏比较系统地总结了当时的地质成果, 将柴达木盆地自北而南划分为“阿尔金山—南祁连陆背斜,柴达木陆向斜,北昆仑华力西
The Qaidam Basin has long been of concern to Chinese petroleum geologists and tectonics. Huang Jiqing in 1955 pointed out that the basement of the Qaidam Basin is a ”hardened Caledonian fold belt.“ In 1956, Zhang Wenyou said: ”The Qaidam basement is composed of Archean crystalline rocks, Paleozoic and early Mesozoic may be connected with the Tarim, due to the Yanshan movement so that the Altun Mountains along the fault rise, the two were separated “; 1957 Zhu Xia systematically summarized the geological results at that time, the Qaidam Basin from north to south For the ”Altun Mountains - South Qilian continental anticline, Qaidam continental syncline, North Kunlun Warisi