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塔北隆起是一个形成于加里东期－海西期的前中生代潜伏隆起，包括４隆２凹．垂向上由加里东期－海西早期的台背斜和海西晚期的逆冲－褶皱系叠置而成，横向上（南北方向上）自北而南隆起幅度逐渐降低；纵向上（东西方向上）东段发育向南扩展的前冲型叠瓦扇，西段发育向北道冲的反冲型逆冲断层．控制塔北隆起构造格局的主要因素包括持续的自北而南的区域性挤压作用、加里东期－海西早期形成的古隆起的隆起幅度以及南天山洋自东而西的剪刀式闭合作用等。
The Tabei uplift is a pre-Mesozoic uplift formed in the Caledonian-Hercynian period, including 4 Long 2 Concave. Vertical from the Caledonian - Hercynian early stage anticline and Hercynian late thrust-fold system stack made of laterally (north-south direction) from north to south uplift gradually reduce the amplitude; longitudinal (east-west direction ) Developed in the eastern segment of the southward extension of the former Chong-shaped laminated fan, the western section of the development of the North Road red thrust thrust. The main factors that control the tectonic uplift of North Tarim Basin include the continuous north-south regional crustal extrusion, the paleo-uplift uplift formed in the Caledonian-Hercynian and the east-west scissor closure in the southern Tianshan Ocean Wait.