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本文以我国云南西部(红河-金沙江以西)新生代陆内造山带(滇西造山带)为例,探讨陆内新生代造山带的演化过程。提出:滇西造山带是经过挤压对冲、夷平、隆升与裂解作用的过程才完成的;在我国现有的造山带中,包括天山、祁连山、秦岭-大别山、太行山和燕山等,绝大多数是新生代的造山带,其形成与演化的过程与滇西造山带基本相同。
In this paper, taking the Cenozoic intracontinental orogenic belt (western Yunnan) as an example, the evolution of the intracontinental Cenozoic orogenic belt is discussed. It is proposed that the western Yunnan orogenic belt was completed through the processes of extrusion hedge, raze, uplift and cracking. In the existing orogenic belts in China, including Tianshan, Qilian Mountains, Qinling Mountains, Dabie Mountains, Taihang Mountains and Yanshan Mountains, Most of them are Cenozoic orogenic belts, and their formation and evolution are basically the same as the western Yunnan orogenic belt.