昆明筇竹寺地区地质构造特征及演化  

The Characteristics and Evolution of Geologic Structures at Qiongzhu Temple District,Kunming

作　　者：龚生权[1] 

机构地区：[1]昆明工学院地质系

出　　处：《昆明工学院学报》1991年第6期1-9,共9页

摘　　要：本文根据较多的野外典型露头资料,综合分析研究,首次提出了本区三次构造运动的看法,并建立了各期主压应力方位.结合褶皱、断层形成的基本力学原理,较合理的分析了现今地质构造特征的形成过程.用褶皱、断层在形成演化过程中相互制约的观点,合理的解释了区内褶皱、断层在不同部位其形态、规模、性质等方面的差异,并总结了浅部构造层次它们相互制约的一般关系.Acording to many data of typical exposures at field and comprehensive investigation,the author put forward first the version of three time tectogenesises at the district,and determined the azimuth of primipal stress each time.Applying the basic dynamic principles on which fold and fault forms the author analysed reasonably the process that geologic structures formed.The differences of the shape, size,nature of fold and fault at different places were reasonably explained by means of the outlook that fold and fault controlled each other during their formation and evolution,and the common relatiorships that shallow structure layers clntrolled each other were summed.

关 键 词：地质构造 演化 构造运动 昆明市 

分 类 号：P542[天文地球—构造地质学]