东昆仑黄羊岭锑矿床地质特征与成矿规律

Jindong Kunlun Huangyangling sb deposit geological characteristics and metallogenic regularity

在我国新疆位于黄羊岭中心地带,是近几年来地质学家新发现的锑矿区,这里锑矿藏丰富。受多年风化累积岩性是由岩屑砂岩与隔档层页岩形成的岩性圈闭,因此是锑矿成矿的基础条件。本文通过对东昆仑锑矿区地质特征与成矿规律的研究,总结出新疆东昆仑黄羊岭地区符合锑矿发展条件,并且具有巨大的发展潜力。

In our country, Xinjiang is located in Huangyangling center, in recent years, geologists discovered in antimony mine, antimony mineral rich here. By years of weathering accumulation lithology is lithologic traps formed by lithic sandstone and shale barrier layer, it is the basic condition of antimony mineralization. In this paper, through study on geological characteristics and metallogenic regularity of antimony mine area in East Kunlun, summed up the Xinjiang East Kunlun Huangyangling area with antimony mine development, and has great potential for development.