文章摘要
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
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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.
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