Qianmiqiao buried hill in Banqiao structural belt of HuanghuaDepression was formed by stretch-faulting on the basis of fold-obduction.
千米桥潜山构造位于黄骅坳陷北大港构造带，千米桥潜山构造是在中生代的褶皱-逆冲作用的基础上经历伸展正断作用后形成的。
参考来源 - 千米桥潜山构造凝析气藏的初步分析 ANALYSIS OF CONDENSATE GAS POOLS IN QIANMIQIAO BURIED HILL·2,447,543篇论文数据，部分数据来源于NoteExpress
凹陷北部斜坡带的变形机制主要是山前重力滑动和山麓逆冲作用。
So in the northern slope of the depression developed gravitation gliding tectonics and fold and thrust structures.
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.
研究发现，西缘逆冲带砂体经历了浅埋藏弱压实和溶蚀作用，储集物性最优；
The Permian high quality reservoir was formed in the western thrust belt and underwent weak compaction with shallow burial and dissolution.
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