In Yingjisha area, affected by the actions of intraplate squeezing and X-conjugate shear, the structural patterns of thin-skinned structure and nappe outlier had been formed.

• 在英吉沙（克孜勒）地区，受喜山期“陆内榨挤”（朱夏，1991）构造作用，以及由此伴生大型“共轭”剪切（走滑）作用影响，分别出现“薄皮构造”和“飞来峰”构造样式。