库鲁克·塔格地区震旦系发育三层冰碛岩，分别是贝义西组、特瑞爱肯组、汉格尔·乔克组。

Three layers of tillites are developed in the Beiyixi formation, Teriaikan formation and Hangeerqiaoke formation of the Neoproterozoic in Quruqtagh region.

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典型的义敦岛弧与沙鲁里山岩浆弧之间的弧-弧碰撞模式及其外延到整个东特提斯构造域内都是很普遍的。

There is a typical example for arc-arc collision between the Yidun island arc andShalulishan magmatic arc, or even throughout eastern Tethys.

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