摘要
新城 -黄陂断裂是桐柏山地区重要的断裂之一。而合河—殷店段韧性剪切带是其重要的组成部分。本文从剪切带构造岩的分带特征、运动特征及动力、形成条件、化学成分及微量元素分布特征等 4个方面 ,论述了合河—殷店段韧性剪切带在几何学、运动学、动力学和流变学等方面的基本特征。
The Xincheng-Huangpi fault is one of the most important faults in the Tongbai Mountain area, and the Hehe-Yindian shear zone constitutes its very important part. The authors dissertate systematically the zoning and movement features, forming conditions, petrochemical and trace-element features of tectonite and geometrical, dynamic and kinetic features as well as rheology of the Hehe-Yindian shear zone.
出处
《华南地质与矿产》
CAS
2001年第1期60-69,共10页
Geology and Mineral Resources of South China
基金
湖北省地质矿产局科研项目<湖北省随州市北部金 (银 )成矿地质条件及找矿方向研究>(91- 0 0 42 - 16 0 10 0 0 3)的部分成果
