摘要
广西桂平—武宣基底地层世代构造变形以震旦—寒武系中的顺层固态流变构造群落的发育为代表。这套构造组合的发现和厘定,对于重新认识该区及邻区早古生代早、中期构造变形性质的演化,可能有较大的意义。
The development of bedding solid rheological structure groups in Sinian-Cambrian system represents the generational structure deformation of Guiping—Wuxian, Guangxi. The discovery and regularization of this set of structure association are likely of great significance in renewing the realization to the characteristic evolution of the structure deformation in the early and middle stage of palaeozoic era in this region and its neighbors.
出处
《广西地质》
1997年第4期25-29,共5页
Guangxi Geology
关键词
下泥盆统
第一世代
变形特征
固态流
构造变形
recumbent fold, stretching lineation, structural style, bedding rheological structure