| 赵东宏,李长安,杨合群,张白志.甘肃省肃南县摆浪沟矿化区找矿潜力分析[J].地质找矿论丛,2003,(4):233-236 |
| 甘肃省肃南县摆浪沟矿化区找矿潜力分析 |
| ANALYSIS ON THE PROSPECTING POTENTIALITY OF BAILANGGOU MINERALIZED REGION |
| 投稿时间：2003-05-08 修订日期：2003-10-05 |
| DOI：10.6053/j.issn.1001-1412.2003.4. 005 |
| 中文关键词: 甘肃省 摆浪沟 铜矿 找矿潜力 |
| 英文关键词:copper mineralization prospecting potentiality Bailanggou Gansu Provice |
| 基金项目: |
| 作者 | 单位 | | 赵东宏 | 西安地质矿产研究所, 陕西, 西安, 710054 | | 李长安 | 西安地质矿产研究所, 陕西, 西安, 710054 | | 杨合群 | 西安地质矿产研究所, 陕西, 西安, 710054 | | 张白志 | 西安地质矿产研究所, 陕西, 西安, 710054 |
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| 中文摘要: |
| 摆浪沟地区地处北祁连山西段奥陶纪弧后盆地火山岩带内,区内古火山机构保留完整,火山岩系为蛇绿岩套上部火山岩的组成部分,岩相发育齐全,与铜矿化密切相关的喷流岩——红碧玉岩发育,沿火山机构铜矿化发育普遍,既有与构造破碎带有关的铜矿化,也有与喷流岩有关的火山块状硫化物矿化存在,显示了该区寻找富铜块状硫化物矿床的巨大前景。 |
| 英文摘要: |
| Bailanggou mineralized region is located in the Ordovician back-arc basin volcanic rock belt along the west sectoin of North Qilian mountains. The palevolcanic edifice is preserved completely. The volcanic rock belong to the upper part of the opholite suite with the volcanic lithofacies entirely developed and the copper mineralitation-reloted eruptive flow of red jasper widely developed. The copper mineralitation is geneally found in the palevolcanic edifice, closely related to cataclasite and the erupted flow volcanics. It shows quite large potential for prospecting rich-copper volicanic massive sulfide deposits in the region. |
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