| 杨泓,李珺,张庆元,刘宇宏,解雅君.东昆仑鸭子沟南铁多金属矿床地质特征及成因分析[J].矿产勘查,2018,9(4):564-570 |
| 东昆仑鸭子沟南铁多金属矿床地质特征及成因分析 |
| Geological characteristics and cenetic analysis of the Yazigounan iron-polymetallic deposit in the East Kunlun Mountain |
| 投稿时间：2017-12-14 |
| DOI： |
| 中文关键词: 地质特征 矿床成因 铁多金属矿 鸭子沟南 东昆仑 |
| 英文关键词: geologic feature, deposit genesis, iron-polymetallic deposit,Yazigounan area, east Kunlun mountain |
| 基金项目:青海省科技万重大科技专项柴达木盆地南北缘成矿系统与勘查开发示范项目(编号:2016-SF-A3)资助。 |
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| 中文摘要: |
| 鸭子沟南矿区位于祁漫塔格山,东昆仑造山带古生代—中生代复合岩浆弧的西段,具有较好的成矿背景,区内发现两种矿床类型,即矽卡岩型和热液型,矿石类型为多金属矿石,成矿时代为印支期。通过简要总结该区铁多金属矿床地质特征,分析矿床成因,希望对矿区今后的找矿工作有所借鉴,争取实现找矿突破。 |
| 英文摘要: |
| The Yazigounan area, located in Qimantage mountain and in the west part of palaeozoic and Mesozoic complex magmatic arcs in Dongkunlun Orogen, has a better metallogenic background. Two types of deposit are found in the area, Namely, the skarn type and hydrothermal type. Ore types are polymetallic ores. The mineralization age belongs to indosinian. Through the summary of geological characteristics and genetic analysis, we hope to guide the prospecting work in the future, and strive for more prospecting breakthrough. |
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