摘要
东昆仑构造带是我国著名的成矿带之一,素有"金腰带"之称,是我国重要的矿产资源基地。阿斯哈金矿床是近年来在东昆仑东段岩体中发现的较具代表性的典型矿床,通过研究区域矿床地质特征和成矿分析,认为矿床成因为受断裂控制的岩浆热液型金矿床。
Eastern Kunlun tectonic belt is one of the famous metallogenic belts to be known as the＂golden belt＂. It is also an important mineral resource base. Gold deposits were found in recent years in the east of Eastern Kunlun rock in more representative of typical ore. We have made an analysis of regional geological characteristics in metallogenic discussion to find that the deposit is subject to fracture of magmatic hydrothermal gold deposits.
出处
《中国锰业》
2017年第4期48-51,共4页
China Manganese Industry
基金
青海省地质勘查基金项目(200931)
关键词
阿斯哈金矿
地质特征
成矿分析
Ashar gold mine
Geological characteristics
Mineralization analysis
