摘要
在分析了陕西旬北浅变质沉积岩区、甘肃白银厂浅变质火山—沉积岩区的构造变形特征的基础上 ,得出了构造变形非整体性的认识 ,进而提出构造变形单元体的概念和划分依据 。
Taking Xunyang in Shaanxi (a low grade metamorphic sedimentary area) and Baiying in Gansu (a low grade metamorphic volcano sedimentary district) as examples, the paper analyzed the characters of non harmonic structural deformation. Based on it, the non harmonic structural deformation, the structural deformation unit and inter layer sliding structure in low grade metamorphic areas were presented, and their field features and discernment discussed.
出处
《地质科学》
CAS
CSCD
北大核心
2002年第4期491-494,T003,共5页
Chinese Journal of Geology(Scientia Geologica Sinica)
基金
原中国有色金属工业总公司"八五"-"九五"重点地质项目部分成果