tianshan orogenic belt

基本解释

The uplifting of the Late Cretaceous was limited in the area of the Kuqa Depression and had no effect on the Tianshan orogenic belt.
晚白垩世的隆升事件局限在库车坳陷内部，没有影响到天山造山带。
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The Tianshan orogenic belt has a W-shape, composed of the V-shape Southern Tianshan and Northern Tianshan with different orogenic models.
天山造山带呈W形结构，由V形结构的南天山和北天山复合而成。两者具有不同的造山模式。
The tectonic evolution and framework of northern part of the Tarim Basin was controlled, obviously, by the creation and evolution of the South Tianshan collisional orogenic belt.
塔里木盆地北部的构造演化和构造格局直接受控于南天山碰撞造山带的形成与演化过程。

天山造山带
The early-middle Permian sedimentation of northwestern margin of Tarim Basin responsed timely to the collisinal orogeny of south Tianshan Orogenic Belt, which offers new evidence for the belt.
塔里木盆地西北缘早-中二叠世的沉积特征对南天山造山带的碰撞造山作用具有良好的沉积响应,为南天山造山带的研究提供了新的沉积学证据。