摘要
本文从基本构造特征与运动机制、变形变质作用与构造层次及形成时代等方面,阐述了江西九岭南坡韧性剪切带与推覆构造的各自特征及其关系。指出:两者无直接的成因联系,前者并不是后者的根带,它们是不同运动机制、不同构造层次、不同地质时代的产物。
This paper discusses its features and the relationship of ductile shear zone with nappe structure in southern slope of Jiuling mountain,Jiangxi Province, according to its basic tectonic feature with move mechanism, deformation and metamorphism with tectonic arrangement and forming age,etc. The authors indicate that both of them have not any relationship in formation. The former is not the root belt of the latter,but they are the result of different move mechanism and tectonic arrangements and geological eras.
出处
《资源调查与环境》
2002年第4期244-249,共6页
Resources Survey & Environment
关键词
成因联系
韧性剪切带
推覆构造
运动机制
构造层次
地质时代
江西
九岭造山带
ductile shear zone
nappe structure
move mechanism
tectonic arrangement
geological era
the southern slope of Jiuling mountain
Jiangxi Province
