The seasonal changes of AOT are obviously in south Xinjiang Basin and middle-west region of Inner Mongolia, but not obviously in Sichuan Basin and the lower reaches of Yangzi river and Yellow river.
南疆盆地和内蒙古中东部地区AOT值随季节变化明显，而四川盆地、长江黄河下游地区AOT值没有明显的季节变化。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
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