曾庆栋,刘铁兵,李光明,沈远超,申萍,陆学良.新疆布尔克斯岱金矿床成矿远景[J].地质与勘探,2004,(4):17-20 |
新疆布尔克斯岱金矿床成矿远景 |
METALLOGENIC PROSPECTING IN THE BUERKESIDAI GOLD DEPOSIT, XINJIANG |
修订日期:2003-03-31 |
DOI: |
中文关键词: 蚀变岩型金矿 EH4连续电导率测量 布尔克斯岱金矿床 新疆 |
英文关键词: altered type gold ore,EH4 electrical conductivity measurement,Buerkesidai gold deposit,Xinjiang |
基金项目:国家科技攻关项目,中国科学院知识创新工程项目 |
曾庆栋 刘铁兵 李光明 沈远超 申萍 陆学良 |
[1]中国科学院地质与地球物理研究所,北京100029 [2]新疆鄯善金矿,鄯善838200 |
摘要点击次数: 2137 |
全文下载次数: 1165 |
中文摘要: |
新疆布尔克斯岱金矿床产于下石炭统黑山头组细碎屑岩中,矿体产出受EW向断裂构造控制.矿石类型主要为构造蚀变岩型.EH4连续电导率测量表明,该矿床深部存在明显的地球物理异常,异常长度大于900 m,宽度大于10 m,延伸大于1000 m,展示了金矿床深部具有良好的成矿前景,是一个有利的大型金矿找矿靶区. |
英文摘要: |
The Buerkesidai gold deposit occurs within lower Carboniferous carbon-bearing rocks. The ore bodies are controlled by E-W strike fault structure. The ore types are mainly structural altered rock type. The results of EH4 Electrical Conductivity Imaging system measurement show that there is a clear geophysical anomaly in depth of the Buerkesidai deposit. The anomaly exceeds 900m in length,10m in width and 1000m in depth. It is indicated that the Buerkesidai gold deposit has a good metallogenic prospects and might become a big type exploration target for gold. |
查看全文
查看/发表评论 下载PDF阅读器 |
关闭 |
|
|
|