背斜山是指与背斜构造相一致的山，存在于褶皱构造地区。
喜山期持续的区域应力作用使那里沟背斜SE翼沿软弱面断裂，经递进扩展变形，最终形成逆冲推覆构造。
The SE limb of Naligou anticline was fractured in the action of persistent regional stressing and expanded into detachment-thrust structure during Himalayan orogenic period.
金矿体的产状严格受铜官山倒转背斜不同部位地层岩石的产状及其层间断裂的控制。
The attitude of gold ore bodies are strictly controlled by that of the strata in different parts of the Tongguanshan overturned anticline and interlayer faults.
火焰山构造带受基底逆冲断裂控制，断裂控制背斜圈闭形成。
Huoyanshan structure belts are controlled by the basement thrusts. The formation of anticline traps is controlled by the faults.
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