| 李艳艳,石明,陈伟民.内蒙古953高地金矿区岩石地球化学特征与深部找矿预测[J].矿产勘查,2016,7(5):805-813 |
| 内蒙古953高地金矿区岩石地球化学特征与深部找矿预测 |
| Characteristics of rock geochemistry and prospectingprediction in the depth of No.953 Highland gold area, Inner Mongolia |
| 投稿时间：2016-02-18 |
| DOI： |
| 中文关键词: 953高地金矿床 原生晕 深部找矿预测 内蒙古 |
| 英文关键词: No.953 Highland gold deposit area, primary halo, prospecting prediction at depth, Inner Mongolia |
| 基金项目: |
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| 摘要点击次数: 1982 |
| 全文下载次数: 1023 |
| 中文摘要: |
| 文章通过对953高地金矿区野外调研,总结了矿床地质特征,对该矿床原生晕分布特征和规律进行了专题研究,确定该矿床成矿元素组合为Au-Ag-Pb-Zn,前缘晕由As、Sb组成,尾晕为Mo。多元统计分析结果和指示元素的变化特征说明矿床经历了多期次的热液活动和地质改造作用,预测钻孔ZK601深部可能有盲矿体。 |
| 英文摘要: |
| Based on field investigation on the No.953 highland gold deposit area and summarization of its geological charaiteristics, a special study on the distribution characteristics and regularity of primary halos in this ore deposit was conducted. The metallogenic element combination is defined as Au-Ag-Pb-Zn assoication, and the front halo is composed of As-Sb elements,whereas the rear halo comprises Mo element. Multivariate statistical analysis result and the variation characteristics of the indicator elements suggest that the ore deposit underwent a long and multiple role of hydrothermal activities and geological transformation, and there might exist concealed gold ore bodies in the depth of ZK601 drill hole. |
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