东天山秋格明塔什-黄山韧性剪切带特征与成矿综述  

Review of the characteristics and mineralization of Qiugemingtashi-Huangshan (Qiu-Huang) ductile shear zone located in East Tianshan

作　　者：郑镝[1] 和志军[2] 董少波[2] 

机构地区：[1]中国地质大学(北京),北京100083 [2]有色金属矿产地质调查中心,北京100012

出　　处：《矿产与地质》2009年第2期110-113,共4页Mineral Resources and Geology

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...

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 

分 类 号：P612[天文地球—矿床学]