| 郭克剑,许令兵,刘国华.豫西潭玉沟银多金属矿地质特征与勘查评价[J].矿产勘查,2015,6(6):725-731 |
| 豫西潭玉沟银多金属矿地质特征与勘查评价 |
| Geological characteristics and prospecting assessment for the Tanyugou silver polymetallic deposit in west Henan |
| 投稿时间：2015-02-26 |
| DOI： |
| 中文关键词: 银多金属矿床 成矿地质特征 勘查评价 豫西潭玉沟 |
| 英文关键词: silver polymetallic deposit, metallogenic characteristics, prospecting assessment, Tanyugou in the west Henan |
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| 中文摘要: |
| 潭玉沟银多金属矿床为构造蚀变岩型矿床,银矿石类型主要为多金属硫化物—钾长石型银矿石、多金属硫化物—石英脉型银矿石、多金属硫化物—白云石型银矿石等3类；矿石中的主要有用组分为银,以独立银矿物或含银铜矿物形式存在,矿石中有用组分银、铅(锌)分布不均匀且交互变化。在矿床勘查评价中,应加强综合研究,在科学论证的基础上,制定矿床综合工业指标,确定矿石的工业利用前景。 |
| 英文摘要: |
| The Tanyugou silver polymetallic deposit is a fracture altered rock type deposit. Main silver ore types are as followings:polymetallic sulfide-k-feldspar type silver ore, polymetallic sulfide-quartzvein type silver ore, and polymetallic sulfide-dolomite type silver ore. The main useful component of the ore is silver which exists as independent silver mineral or silver-containing copper minerals. The concentration distribution of useful components of silver and lead (zinc) in the ore is unevenly and changes interactively. Therefore, the comprehensive study should be strengthened during prospecting assessment. On the basis of scientific verification, the comprehensive industrial indicators of the deposit, and the industrial use of the ore deposit can be determined. |
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