探讨青海省都兰县香日德地区小庙岩组岩石特征及变质地层特征  

Characteristics of small temple rock group rock and metamorphic strata in Dulan County of Qinghai province Xiangride area

作　　者：靳旭亮[1] 马林 杨文军[1] 白旭东[1] 赵永寿 

机构地区：[1]青海省地质调查院区域地质调查研究所,青海西宁810001

出　　处：《世界有色金属》2017年第15期190-190,192,共2页World Nonferrous Metals

摘　　要：香日德地区小庙岩组位于古元古代白沙河岩群片麻岩岩段以南,岩群组为断裂层生长,同时也有矿石类的物质在各个时段逐渐渗入及通过蚀化作用进入岩体,在该环境下生长出了蛇绿混合岩体,大面积分布的是沉积地层。本文对香日德地区小庙岩组变质岩岩石特征进行了探讨。The Xiangride area of small temple rock group is located in the Paleoproterozoic Baishahe rock group gneiss rock section of South rock group for fracture layer growth, but also has ore material in each period and by gradually infiltrated into the corrosion effects into the rock, in the environment of the growth of a mixed ophiolitic rock mass, large area distribution is sedimentary strata. This paper discusses the characteristics of rock temple rock group metamorphic rocks in Xiangride area.

关 键 词：香日德 小庙岩组 变质岩岩石特征 

分 类 号：P588.2[天文地球—岩石学]