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五十年代前,有些学者认为塔里木地台中央是一个古隆起,或在古地理方面作为古生代时期的剥蚀古陆,呈椭园状居于塔里木中央地区。从50年末,地质部与石油部的重磁力资料,认为塔里木地台在古生代是一个拗陷区。后来,由于石油地质工作不断地深入发展,尤其是1983—1984年我国石油部与美国石油公司合作开展了横穿塔克拉玛干沙漠地震大剖面工
Before the 1950s, some scholars think that the central Tarim Basin is a paleohigh, or in the paleogeography of the Paleozoic erosion of the ancient land, oval-shaped living in the central Tarim. From the end of 1950, the heavy and magnetic information of the Ministry of Geology and the Ministry of Petroleum, that the Tarim platform in the Paleozoic is a depression area. Later, due to the continuous deepening development of petroleum geology work, especially in 1983-1984, the Chinese Ministry of Petroleum and the United States National Petroleum Company conducted a large cross-section of workers across the Taklamakan earthquake