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内蒙古新地沟金矿床黄铁矿热电性特征及深部找矿意义

刘华南, 刘家军, 李小伟, 刘冲昊, 代鸿章, 陶银龙, 王建锋, 杜映东, 范云飞. 2018. 内蒙古新地沟金矿床黄铁矿热电性特征及深部找矿意义[J]. 中国地质, 45(4): 819-838. doi: 10.12029/gc20180412
引用本文: 刘华南, 刘家军, 李小伟, 刘冲昊, 代鸿章, 陶银龙, 王建锋, 杜映东, 范云飞. 2018. 内蒙古新地沟金矿床黄铁矿热电性特征及深部找矿意义[J]. 中国地质, 45(4): 819-838. doi: 10.12029/gc20180412
LIU Huanan, LIU Jiajun, LI Xiaowei, LIU Chonghao, DAI Hongzhang, TAO Yinlong, WANG Jianfeng, DU Yingdong, FAN Yunfei. 2018. Thermoelectric characteristics of pyrite from the Xindigou gold deposit in Inner Mongolia and its significance on deep prospecting[J]. Geology in China, 45(4): 819-838. doi: 10.12029/gc20180412
Citation: LIU Huanan, LIU Jiajun, LI Xiaowei, LIU Chonghao, DAI Hongzhang, TAO Yinlong, WANG Jianfeng, DU Yingdong, FAN Yunfei. 2018. Thermoelectric characteristics of pyrite from the Xindigou gold deposit in Inner Mongolia and its significance on deep prospecting[J]. Geology in China, 45(4): 819-838. doi: 10.12029/gc20180412

内蒙古新地沟金矿床黄铁矿热电性特征及深部找矿意义

  • 基金项目:
    中国地质调查局新兴产业资源战略调查评价专项工程项目(1212011220673)资助
详细信息
    作者简介: 刘华南, 男, 1988年生, 博士生, 主要从事金属矿床地球化学研究; E-mail:northchina1@163.com
    通讯作者: 刘家军, 男, 1963年生, 教授, 博士生导师, 主要从事矿床研究与教学工作; E-mail:liujiajun@cugb.edu.cn
  • 中图分类号: P678.51

Thermoelectric characteristics of pyrite from the Xindigou gold deposit in Inner Mongolia and its significance on deep prospecting

  • Fund Project: Supported by the project evaluation of emerging industry resources strategic investigation of China Geological Survey (No. 1212011220673)
More Information
    Author Bio: LIU Huanan, male, born in 1988, doctor candidate, engages in the study of ore deposit geochemistry; E-mail:northchina1@163.com .
    Corresponding author: LIU Jiajun, male, born in 1963, professor and supervisor of doctor candidates, engages in the study of ore deposit geochemistry.E-mail:liujiajun@cugb.edu.cn
  • 内蒙古新地沟金矿是中型绿岩型金矿床,但已属于严重资源危机的矿山,急待寻找接替资源,因此对新地沟金矿床进行深部远景预测具有十分重要的意义。本文根据找矿矿物学和成因矿物学理论,利用显微镜、电子探针及热电仪系统分析新地沟金矿床不同标高和矿段中黄铁矿的热电型标型特征,研究结果表明:新地沟金矿床中黄铁矿的晶型以立方体、五角十二面体及聚形为主;热电系数变化主要集中在-331.10~340.20 μV·℃-1范围内,导电型多以N型为主,约占总含量的80%;成矿温度主要集中于250~340℃,属于中温矿床。黄铁矿热电性参数XNP变化范围较大,估算矿体剥蚀率为67.96%~74.31%。通过对黄铁矿导型的空间分布规律和矿体剥蚀分析表明:油篓沟矿段位于矿体中底部,向深部可能有小规模延伸,小西沟矿段钻孔ZK106在深部有较大规模的延伸,其矿化前景最好;小西沟矿段钻孔ZK102深部矿化前景次之;大汗青矿段钻孔ZK2802其深部矿化前景较差。综合分析认为,该矿床深部具有较好的找矿潜力。

  • 加载中
  • 图 1  大青山新地沟金矿区域地质简图(据胡凤祥等,2002)

    Figure 1. 

    图 2  新地沟金矿矿区地质简图(据内蒙古沃野矿冶技术开发公司,2009)

    Figure 2. 

    图 3  新地沟金矿矿脉地质剖面图(据内蒙古沃野矿冶技术开发公司,2009)

    Figure 3. 

    图 4  新地沟金矿床矿石类型

    Figure 4. 

    图 5  新地沟金矿黄铁矿特征
    Py—黄铁矿;Qz—石英;Au—金;

    Figure 5. 

    图 6  新地沟金矿床各钻孔及矿体黄铁矿热电系数直方图

    Figure 6. 

    图 7  新地沟金矿床各钻孔及油篓沟矿体P型黄铁矿出现率垂向变化趋势图

    Figure 7. 

    图 8  新地沟金矿床黄铁矿热电系数−温度图解

    Figure 8. 

    图 9  新地沟金矿床黄铁矿温度直方图

    Figure 9. 

    图 10  新地沟金矿金品位与离散度、P型黄铁矿概率关系图

    Figure 10. 

    图 11  新地沟金矿床黄铁矿热电系数离散度-P型黄铁矿概率关系图

    Figure 11. 

    图 12  新地沟金矿床黄铁矿热电系数离散度-标高关系图

    Figure 12. 

    表 1  新地沟金矿黄铁矿物电子探针数据(%)

    Table 1.  Electron microprobe analyses of pyrite in the Xindigou gold deposit (%)

    下载: 导出CSV

    表 2  油篓沟中段黄铁矿热电性系数值

    Table 2.  Thermoelectric coefficients of pyrites from Youlougou orebody

    下载: 导出CSV

    表 3  钻孔ZK102黄铁矿热电性系数值

    Table 3.  Thermoelectric coefficients of pyrites from drill hole ZK102

    下载: 导出CSV

    表 4  钻孔ZK106黄铁矿热电性系数值

    Table 4.  Thermoelectric coefficients of pyrites from drill hole ZK106

    下载: 导出CSV

    表 5  钻孔ZK2802黄铁矿热电性系数值

    Table 5.  Thermoelectric coefficients of pyrites from drill hole ZK2802

    下载: 导出CSV
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收稿日期:  2016-05-30
修回日期:  2018-05-16
刊出日期:  2018-08-25

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