摘要
范庄金银多金属矿床位于熊耳山西段,通过对矿床地质特征及化探异常研究,认为本区金银矿脉分布具有分带性,且与异常分布相吻合,受区内拆离断层和北东向脆性断裂控制,矿床类型为构造蚀变岩型矿床,并对区内找矿标志进行了总结,对区内找矿潜力进行了分析。
Fanzhuang Gold and Silver Polymetallic Deposit is located in the west section of the Xiongershan. Studyon the geochemical anomaly and the geological characteristics of the deposit thinks that gold and silver lode distribu-tion in this area has zonation and goes with the anomaly distribution. It is controlled by detachment faults and NE tren-ding brittle fracture, and the deposit type is tectonic alteration rock type deposit. The prospecting indicators are summa-rized and the prospecting potentials in the area are analyzed.
出处
《黄金》
CAS
2015年第8期18-22,共5页
Gold
基金
河南省国土资源厅国土资源科技计划项目(2013-114)
关键词
矿床特征
化探异常
金银矿床
找矿标志
找矿潜力
范庄金银多金属矿床
deposit characteristics
geochemical anomaly
gold and silver deposit
prospecting indicator
pros-pecting potentials
Fanzhuang Gold and Silver Polymetallic Deposit