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造山带演化可分为两个阶段：造山期和成山期。造山期地质调查一直是我国区调工作的重点，调查的内容以区内基础地质特征研究为主。而成山期地质调查过去一直被忽视，这也正是当前“扩大区调服务领域”所要探讨的问题。造山带成山期区域地质调查重点是：①造山带隆升的过程与特点；②山脉隆升的环境效应；③造山带现代构造运动与地质灾害。笔者结合东昆仑造山带１∶２５万冬给措纳湖幅和兴海县幅区调，对成山运动和环境变化进行讨论。
The orogenic belt evolution can be divided into two stages: the orogeny and the Chengshan period. Geological survey of orogenic period has always been the focus of China’s regional transfer work, the content of the survey is based on the study of basic geological features in the area. However, the geological survey of Chengshan period has been neglected in the past, which is exactly the issue to be discussed in the current “area expansion and adjustment of service area”. The major geological survey of orogenic belt in the orogenic belt is: ①the process and characteristics of the uplift of the orogenic belt; ② the environmental effect of the uplift of the mountain; ③ the modern tectonic movement and geological disasters of the orogenic belt. The author combined the East Kunlun orogenic belt 1: 250,000 winter to Zona Lake amplitude and Xinghai County amplitude adjustment, Chengshan movement and environmental changes are discussed.