Actually, Keping fault-uplift, under which there exists a paleouplift as a part of Bachu fault-uplift, is an overthrust belt formed during Neocene Kuche period.

• 柯坪断隆实际上是上新世库车期形成的逆掩推覆带，其下尚隐伏着与巴楚断隆连为一体的古隆起。