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针对塔里木盆地原型研究中的“泛前陆”倾向，根据前陆盆地的概念和特点，指出了它在时间和空间上的局限性。对志留—泥盆纪、晚二叠世—侏罗纪和晚中生代—新生代几个时期在塔里木盆地是否存在前陆进行了讨论，认为塔里木盆地是一个克拉通断块上的经历了多开合旋回的复杂结构盆地。
Aiming at the “Pan-Foreland” tendency in the prototype study of the Tarim Basin, it is pointed out its limitations in time and space according to the concept and characteristics of the foreland basin. The existence of the foreland in the Tarim-Devonian, Late Permian-Jurassic and Late Mesozoic-Cenozoic periods was discussed in the Talimu Basin, suggesting that the Tarim Basin is a craton block experienced more Opening and closing of the complex structure of the basin.