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现代矿业 ›› 2025, Vol. 41 ›› Issue (05): 171-176.

• 地质·测量 • 上一篇    下一篇

安徽省黄屯S-Fe-Au-Cu矿床黄铁矿与黄铜矿电性特征及找矿意义

赵永建1 王浩阳2 张萌萌3 申俊峰2 陈 强4   

  1. 1. 安徽省金鼎矿业股份有限公司;2. 中国地质大学(北京)地球科学与资源学院; 3. 中国地质大学(北京)珠宝学院;4. 北京中育神州数据科技有限公司
  • 出版日期:2025-05-25 发布日期:2025-07-30

Electrical Characteristics and Prospecting Significance of Pyrite and Chalcopyrite in the S-Fe-Au-Cu Deposit in Huangtun,Anhui Province

  1. 1. Anhui Jinding Mining Co.,Ltd.;2. School of Earth Sciences and Resources,China University of Geo⁃ sciences,Beijing;3. School of Gemology,China University of Geosciences,Beijing;4. Beijing Zhongyu Shenzhou Data Technology Co.,Ltd.
  • Online:2025-05-25 Published:2025-07-30

摘要: 安徽省庐江县黄屯 S-Fe-Au-Cu矿床位于长江中下游成矿带庐枞盆地东北缘,原为大 型硫铁矿床,近年来新发现了厚大的隐爆角砾岩型金铜矿体,是庐枞盆地发现的首例该类型矿床。 新矿体的发现丰富了庐枞盆地内的矿床类型,为区域内金、铜的找矿勘查提供了新的启示。在矿床 基本特征研究的基础上,采集矿区内9个钻孔中矿石/蚀变岩,共计220件样品,利用矿物热电仪与热 电阻仪系统研究了黄屯矿区隐爆角砾岩筒内、外黄铁矿和黄铜矿的热电性与热电阻特征。结果显 示,随着活化温度的升高(50~80 ℃),隐爆角砾岩筒内样品黄铜矿测点的热电性特征有95%的概率会 消失,而隐爆角砾岩筒外黄铜矿的热电性并不出现该现象。相比于角砾岩筒外黄铁矿和黄铜矿的热 电阻范围(分别为 0~10 Ω·m和 0~5 Ω·m),角砾岩筒内黄铁矿和黄铜矿热电阻率范围明显较为宽泛 (分别为0~40 Ω·m和0~25 Ω·m)。因此,基于黄铁矿和黄铜矿的电性特征能够有效识别区域隐爆角 砾岩成矿条件下的黄铁矿与黄铜矿,对黄屯矿区乃至庐枞盆地内进一步寻找隐爆角砾岩型金铜矿化 具有重要指导意义,对发现庐枞盆地内新的矿化线索具有借鉴意义。

关键词: 黄铁矿, 黄铜矿, 热电性, 热电阻, 找矿预测

Abstract: The Huangtun S-Fe-Au-Cu deposit in Lujiang County,Anhui Province is located on the northeastern margin of the Luzong Basin in the middle and lower reaches of the Yangtze River mineralization belt. It is originally a large pyrite deposit. In recent years,a thick and large hidden explosive breccia-type gold and copper deposit has been newly discovered,which is the first deposit of this type in the Luzong Ba⁃ sin. The discovery of the new ore body has enriched the types of ore deposits in the Luzong Basin and provid⁃ ed new inspirations for the exploration of gold and copper in the region. Based on the study of the basic char⁃ acteristics of the deposit,a total of 220 samples of ore/altered rock from 9 boreholes in the mining area were collected. The thermoelectric and thermal resistance characteristics of pyrite and chalcopyrite inside and out⁃ side the hidden explosion breccia cylinder in the Huangtun mining area were studied by using the mineral thermoelectric instrument and thermal resistance instrument system. The results show that with the increase of activation temperature (50~80 ℃),there is a 95% probability that the thermoelectric characteristics of the sample chalcopyrite measurement points in the hidden explosion breccia cylinder will disappear,while this phenomenon does not occur in the thermoelectric properties of chalcopyrite outside the hidden explosion breccia cylinder. Compared with the thermal resistance ranges of pyrite and chalcopyrite outside the breccia cylinder (0~10 Ω·m and 0~5 Ω·m respectively),the thermal resistance rate ranges of pyrite and chalcopy⁃ rite inside the breccia cylinder are significantly broader (0~40 Ω·m and 0~25 Ω·m respectively). There⁃ fore,based on the electrical characteristics of pyrite and chalcopyrite,it is possible to effectively identify py⁃ rite and chalcopyrite under the mineralization conditions of regional hidden explosion breccia. This is of great guiding significance for further searching for hidden explosion breccia-type gold and copper mineral⁃ ization in the Huangtun mining area and even the Luzong Basin,and it also has reference significance for discovering new mineralization clues in the Luzong Basin.

Key words: pyrite, chalcopyrite, thermoelectric property, thermal resistance, mineral prospecting