首页> 外文期刊>世界地质(英文版) >Application of high-frequency magnetotelluric method in porphyry copper deposit exploration: a case study of Duobaoshan deposit area
【24h】

Application of high-frequency magnetotelluric method in porphyry copper deposit exploration: a case study of Duobaoshan deposit area

机译:高频大地电磁法在斑岩型铜矿床勘探中的应用-以多宝山矿床区为例

获取原文
获取原文并翻译 | 示例
       

摘要

The Duobaoshan mine area in Heilongjiang is located in the northeast section of Xingmeng orogenic belt and is in the west side of Hegang Mountain-Heihe fault zone .There exist many deposits in this area , and its metallogenic conditions are superior , which has been one of the hotspots in geological prospecting and metal -logenic research in Northeast China .On the basis of previous studies , the authors used the EH-4 electromagnet-ic imaging system to carry out the data acquisition of three survey lines in Woduhe Village , Duobaoshan Town , Nenjiang County .Through the analysis of apparent resistivity section under TE and TM polarization modes , in-tegrating regional geological data , it is concluded that:①the electrical characteristics of the metal ore in this area show a relatively low resistance , and according to its resistivity difference with surrounding rocks , the geo-metrical structures and apparent resistivity parameters of the low resistivity bodies in the lower section of the sur -vey line are defined , and the electrical anomalies can be identified;②faults F1 and F2 may have a good metal-logenic environment , so they are recommended for further exploration;③low resistance metal ore bodies have good correlation with local small structures or faults , which may play an iconic role for the delineation of key target areas;④in the process of using apparent resistivity to define the geometric structures of ore bodies un -derground , comprehensive analysis integrating the advantages of TE and TM models should be carry out to achieve more reliable inversion results .
机译:黑龙江多宝山矿区位于兴蒙造山带东北段,在鹤岗山-黑河断裂带的西侧,该地区有大量矿床,成矿条件优越,是东北地区的重要矿床之一。东北地区地质勘探和金属成矿研究的热点。在以往研究的基础上,作者利用EH-4电磁成像系统对多宝山镇沃都河村的3条测量线进行了数据采集。嫩江县。通过对TE和TM极化模式下视电阻率剖面的分析,综合区域地质资料,得出以下结论:①该地区金属矿的电学特征表现为电阻较低,并根据电阻率与围岩的差异,下部低电阻率体的几何结构和表观电阻率参数;确定了测量线,可以识别出电气异常;②断层F1和F2可能具有良好的成矿环境,因此建议进一步勘探;③低电阻金属矿体与局部小构造或断层,可能对关键目标区域的划定起标志性作用;④在利用视电阻率确定地下矿体几何结构的过程中,应进行综合分析,结合TE和TM模型的优点获得更可靠的反演结果。

著录项

  • 来源
    《世界地质(英文版)》 |2017年第4期|246-252|共7页
  • 作者单位

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-19 03:54:00
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号