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金属矿山 ›› 2016, Vol. 45 ›› Issue (04): 95-100.

• 地质与测量 • 上一篇    下一篇

黟县胡家门地区锡多金属矿地质特征与成矿条件

王西荣1,2,潘家永1,李绍侠2   

  1. 1.东华理工大学地球科学学院,江西 南昌 330013;2.安徽省地质实验研究所,安徽 合肥230001
  • 出版日期:2016-04-15 发布日期:2016-08-16
  • 基金资助:

    基金项目 安徽省地矿局地质勘查基金项目(编号:DD20140429,DD20060528)。

Geological Characteristics and Metallogenic Conditions of Tin-polymetallic Deposit of the Hujiameng Area in Yixian County

Wang Xirong1,2,Pan Jiayong1,Li Shaoxia2   

  1. 1.College of Earth Sciences,East China Institute of Technology,Nanchang 330013,China;2.Geological Experiment Institute of Anhui Province,Hefei 230001,China
  • Online:2016-04-15 Published:2016-08-16

摘要: 黟县胡家门地区位于安徽省南部,区内锡多金属矿位于“江南古陆”北东段北缘。对区内锡多金属矿区进行了高精度磁法测量和1∶10 000土壤地球化学测量,测量数据反演计算结果表明:①区内异常分为北、中、南(M-1#、M-2#,M-3#)等3个区,北区以低缓磁异常分布为特征,强度均在50 nT以下,中区以强度高(多大于100 nT)、异常相连分布为特征,南区以中等强度异常分散分布为特征,根据异常分布形态、强度及地质特征,推测存在2条隐伏断层和2个隐伏岩体。②区内微量元素分布特征与地质背景密切相关,区内北部Sn含量明显高于南部,Sn含量高值分布区域与花岗岩类岩体(M-1#异常区)基本一致,区内共圈定了7处锡异常,锡矿找矿潜力巨大。在上述分析的基础上,进一步讨论认为区内岩石越破碎,含量矿性越好,W、Mo、Sn含量从岩体内部向接触带有逐渐升高的现象,区内地处江南过渡带“菱形”格局的北东交汇部位,成矿条件有利,寻找到类似祁门东源的斑岩型钨钼矿的可能性较大。

关键词: 高精度磁法测量, 土壤地球化学测量, 异常分布, 成矿条件, 斑岩型钨钼矿

Abstract: The Hujiameng area in Yixian county is located in the south of Anhui province,the tin-polymetallic of the Hujiameng area is also located in the northern margin of the north eastern section of "Jiannan ancient continent ",the high-precision magnetic measurement and 1∶10 000 soil geochemical survey are conducted in the Hujiameng area,the inversion calculation results of the measured data show that:①the anomaly area in the Hujiameng area is divided into three anomaly areas,they are northern anomaly area,middle anomaly area and southern anomaly area (M-1#,M-2#,M-3#),the northern anomaly area is characterized by the distribution of relatively low magnetic anomaly,the anomaly intensity is lower than 50 nT,the middle anomaly area is characterized by high anomaly intensity (more than 100 nT) and continuous distribution,the southern anomaly area is characterized by moderate anomaly intensity scattered distribution,according to the distribution pattern,intensity and geological characteristics of anomaly areas,it is inferred that there are two hidden faults and two concealed rock bodies are existed in the area.②The distribution characteristics distribution of the trace element is closely related to geological background in the area,the Sn contents in the northern anomaly area is higher than that of the southern anomaly area,the distribution area of the high values of Sn contents is almost the same as the granite type of rock mass (M-1#anomaly area),seven tin anomaly areas are circled in the area,therefore,the tin deposit prospecting potential in the area is huge.Based on the above results,it is further show that the higher the degree of rock crushing,the better of the ore contents,the contents of Mo,Sn and W are increased gradually from the inner of the rock mass to the margin of the rock mass,the Hujiameng area is located in the northeast intersection of the "diamond" structure of Jiangnan transition zone,the metallogenic conditions is favorable,it is more likely to find the porphyry deposit that is similar to the porphyry type tungsten molybdenum deposit.

Key words: High-precision magnetic measurement, Soil geochemical survey, Anomaly distribution, Metallogenic conditions, Porphyry type tungsten molybdenum deposit