Wensu uplift as part of Tabei uplift was an inheriting paleo-uplift during geologic epoch.It has been separated from Tahei uplift by the huge Kalayuergun fault since Paleocene epoch.

• 温宿凸起在地质历史时期曾与塔北隆起连为一体，是长期继承性发育的古凸起，古近纪卡拉玉尔滚大型走滑断层将其与塔北隆起分开。