范家山汞矿地质特征与成矿规律研究  

Geological characteristics of the Fanjiashan Hg deposit with a research on its ore-forming rules

作　　者：伍守荣[1] 

机构地区：[1]昆明理工大学国土资源工程学院

出　　处：《矿产与地质》2007年第6期618-625,共8页Mineral Resources and Geology

摘　　要：范家山汞矿是万山汞矿区南部唯一的大型汞矿床,矿体形态简单,矿石品位高(O.658%),埋藏深(337～706m).伴生有苴组分硒,达到中型矿床规模,硒矿体与汞矿体完全重合.对该矿的地质特征及成矿规律进行总结和分析,认为该区具有进一步寻找深部新的汞、硒矿产资源潜力.The Fanjiashan Hg deposit is the only large scale Hg deposit in southern part of the Wanshan Hg ore area with its orebody shape being simple,ore grade being high and orebody being embeded deeply(337-706M).The deposit of an associated benificial element Se,of which the orebody is perfect superposition with that of Hg deposit,has reached middle scale.It has concluded and analyzed the geological characteristics and ore-forming rules of the Fanjiashan deposit,and believed that there is a great potential of further prospecting for new Hg,Se resources in this ore area.

关 键 词：汞矿床 成矿规律 地质特征 范家山 

分 类 号：P618.68[天文地球—矿床学]