摘要
哀牢山是云贵高原和横断山脉的重要分界线,形成于中生代燕山运动时期至第四纪喜马拉雅运动时期,是较为年轻的山脉。哀牢山经过了较为复杂的地质变化,岩层结构的中深变质岩系对其地质条件影响很大,文章将对中深变质岩系的构造变形特征和演变进行分析,为哀牢山的地质研究提供一些思考和启示。
The important dividing line between the yungui plateau and the hengduan mountains formed during the Mesozoic yanshan movement period and the quaternary Himalayan movement period, is the younger mountain range. Complex geological changes after the ailaoshan, deep metamorphic rock series in the formations of the on the geological conditions, the article will have on the deep metamorphic rock series in the analysis of the characteristics of tectonic deformation and evolution of ailaoshan geological research to provide some thinking and enlightenment.
出处
《世界有色金属》
2017年第22期257-257,259,共2页
World Nonferrous Metals
关键词
哀牢山
中深变质岩系
构造
特征
演变
Mourning mountain
Mesometamorphic rock series
Structure
Characteristic
The evolution of
