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现代矿业 ›› 2026, Vol. 42 ›› Issue (03): 177-181.

• 地质·测量 • 上一篇    下一篇

班戈县玉古拉铁多金属矿地质特征及找矿方向分析

郝 明 张 伟 夏富富   

  1. 辽宁省冶金地质勘查研究院有限责任公司
  • 出版日期:2026-03-25 发布日期:2026-04-20

Analysis of Geological Characteristics and Prospecting Direction of Yugula Iron Polymetallic Deposit in Bange County

  1. Liaoning Provincial Institute of Metallurgical Geological Exploration Co.,Ltd.
  • Online:2026-03-25 Published:2026-04-20

摘要: 玉古拉铁多金属矿位于西藏最重要的成矿带之一的班公湖—怒江成矿带中段,该带 近年来不断取得找矿突破,已成为全国重要的铜、铁、金多金属资源接替基地,成矿地质条件优越, 但受高原地区地理条件制约,该矿床工作程度较低,资源潜力尚不明确。为摸清矿床找矿前景和 找矿潜力,在 1∶1 000 实测地质剖面、1∶2 000 地质测量、磁法测量、槽探及钻探验证等基础上,对矿 床地质特征和矿体赋存规律进行综合研究,系统分析矿床成因,总结找矿标志,并明确下一步找矿 方向。结果表明,矿区已发现的 FeⅠ号、FeⅡ号主矿体均充填于断层破碎带中,呈似层状产出,且沿 超基性岩体分布,成矿作用与基性-超基性岩体侵位及后期构造活动密切相关;矿床成因为岩浆熔 离型,发现的 2 个主矿体铁矿石资源量已初具小型矿床规模,矿区具备较好的找矿前景和找矿潜 力;蛇绿岩带、超基性岩、蛇纹石化强烈部位及构造发育处是下一步找矿的重点方向,其中Ⅰ号、Ⅲ号 磁异常带为找矿重点区域,磁法与重力勘探结合可提高隐伏矿体预测精度。

关键词: 铁多金属矿, 地质测量, 矿床成因, 找矿方向

Abstract: The Yugula iron polymetallic deposit is located in the middle of the Bangong Lake-Nuji‐ ang River metallogenic belt,one of the most important metallogenic belts in Tibet.In recent years,the belt has made breakthroughs in prospecting and has become an important base for the replacement of copper, iron and gold polymetallic resources in China.The geological conditions for mineralization are superior,but due to the geographical conditions of the plateau area,the degree of work of the deposit is low and the re‐ source potential is not clear. In order to find out the prospecting prospect and prospecting potential of the deposit,on the basis of 1∶1 000 measured geological profile,1∶2 000 geological survey,magnetic sur‐ vey,trenching and drilling verification,the geological characteristics of the deposit and the occurrence law of the ore body are comprehensively studied,the genesis of the deposit is systematically analyzed,the prospecting criteria are summarized,and the next prospecting direction is clarified. The results show that the main ore bodies of Fe I and Fe II found in the mining area are filled in the fault fracture zone,which are layered and distributed along the ultrabasic rock mass. The mineralization is closely related to the em‐ placement of basic-ultrabasic rock mass and the later tectonic activity. The genesis of the deposit is mag‐ matic liquation type. The iron ore resources of the two main ore bodies that have been found have begun to have a small deposit scale,and the mining area has good prospecting prospects and prospecting potential. The ophiolite belt,ultrabasic rock,strong serpentinization and structural development are the key direc‐ tions for further prospecting. Among them,No.I and No.III magnetic anomaly belts are the key areas for prospecting. The combination of magnetic method and gravity exploration can improve the prediction accu‐ racy of concealed ore bodies.

Key words: iron polymetallic mine, geological surveying, deposit genesis, prospecting direction