摘要
东天山"秋格明塔什-黄山韧性剪切带"是一条多期活动且持续时间很长的韧性剪切变形变质带,介于北部的康古尔塔格-黄山断裂和南部的雅满苏-苦水断裂之间。在研究其空间展布特征、变形组构、演化序列、力学性质、剪切位移量以及变形时代的基础上,对其与成矿的关系进行了初步探讨。
Qiugemingtashi-Huangshan ductile shear zone located in East Tianshan is a deformation and metamorphism zone which came through long-term multi-stages activities.The shear zone is situated in the area between northern Kanggu ertage Huangshan fracture and southern Yamansu-kushui fault.The paper has preliminarily discussed the relationship between the shear zone and mineralization on the basis of learning the spacial distribution,deformation structure,evolution sequence,mechanical properties,shearing displacem...
出处
《矿产与地质》
2009年第2期110-113,共4页
Mineral Resources and Geology
关键词
韧性剪切变形变质带
变形组构
剪切位移量
成矿
秋格明塔什-黄山
ductile shear zone with deformation and metamorphism
deformation structure
shearing displacement
mineralization
Qiugemingtashi-Huangshan
