摘要
通过对北山地区金矿赋矿围岩——碳质板岩、浅变质含碳碎屑岩及主要载金矿物黄铁矿和石英的微量元素、稀土元素特征研究，认为北山地区金矿床是在含金建造的成矿物质基础上，经后期深源热液能量叠加的金矿床。
Based on the characteristics of trace elements and REE in surrounding rocks and pyrite and quartz from the Baishan gold deposits, the authors suggest that the gold deposits in Beishan are formed by addition energies of deep source hydrothermal solution on the minerogenetic materials of gold bearing formation.
出处
《成都理工学院学报》
CSCD
1998年第1期83-86,共4页
Journal of Chengdu University of Technology
基金
地矿部资源与环境科技攻关项目
关键词
围岩
黄铁矿
石英
金矿床
矿物
地球化学
surrounding rocks
pyrite
quartz
REE
trace element
gold deposit
Beishan
