摘要
米仓山地区前震旦纪基底韧性剪切带内断层岩的组构分析结果显示，结晶基底与褶皱基底的岩组特征存在差异。
The petrofabric analysis on the fault rocks in the ductile shear zones in Presinian basement of Micangshan area reveals that the petrofabric characteristics in the crystalline basement are different from those in the folded basement. It is considered that the different deformation environments of the two basements lead to their petrofabric discrepancy.
出处
《矿物岩石》
CAS
CSCD
北大核心
1998年第S1期73-77,共5页
Mineralogy and Petrology
基金
国家计委"八.五"重点攻关项目
关键词
组构分析
岩组
滑移系
变形环境
fabric analysis petrofabrics slip system deformation environment
