img

Wechat

  • CN 62-1112/TF 
  • ISSN 1005-2518 
  • Founded in 1988
Adv. Search

Application of Induced Polarization Method in a Gold Mine of Muping,Shandong Province

Expand
  • 1.Key Laboratory of Gold Mineralization Processes and Resource Utilization Subordinated to the Ministry of Land and Resources,Jinan   250013,Shandong,China;
    2.Key Laboratory of Metallogenic Geological Process and Resources Utilization in Shandong Province,Jinan   250013,Shandong,China;
    3.Shandong Institute of Geological Sciences,Jinan   250013,Shandong,China

Received date: 2016-03-14

  Revised date: 2016-05-06

  Online published: 2016-10-08

Abstract

Abstract: In order to find out the mineralization distribution characteristics and the deep development of a gold deposit located in Muping of Shandong Province and to definite an optimal prospecting target area,Induced Polarization (IP) method is applied in measuring work.Depth sounding of induced polarization method is carried out in the mining area where four induced polarization anomalies are defined through the middle gradient area measurement.Combining with the geological data in the area,rock ore characteristics and field reconnaissance,the sounding profiles are analyzed.It can be inferred that the delineation of four induced polarization abnormalities are caused by pyrite quartz vein and pyrite mineralization alteration rock,and the mineralize development well in deep,they are favorable gold metallogenic area in this area.The IP survey helps to identify follow-up survey work and find the key area of the mine,and good results have been achieved in the application of this gold mine.

Cite this article

XU Yan,WEI Jian,LUO Wenqiang,YANG Chao,WANG Zhiming,ZHOU Xin,YIN Jiguang,ZHANG Hongliang,WANG Hongjie,WANG Li . Application of Induced Polarization Method in a Gold Mine of Muping,Shandong Province[J]. Gold Science and Technology, 2016 , 24(3) : 35 -39 . DOI: 10.11872/j.issn.1005-2518.2016.03.035

References

[1] 杨立强,邓军,王中亮,等.胶东中生代金成矿系统[J].岩石学报,2013,30(9):2247-2267.
[2] 孔庆友,张天祯,于学峰,等.山东矿床[M].济南:山东科学技术出版社,2007.
[3] 李旭分,刘建朝,张学仁,等.牟平—乳山金矿带构造特征及成矿预测[J].黄金科学技术,2013,21(3):10-15.
[4] 翟明国,杨进辉,刘文军.胶东大型黄金矿集区及大规模成矿作用[J].中国科学(D辑),2001,31(7):545-552.
[5] 贺振,张学仁.山东牟乳金矿带构造控矿特征及综合预测[J].地质与勘探,2006,42(4):41-45.
[6] 杨喜安,赵国春,宋玉波,等.胶东牟平—乳山成矿带拆离断层控矿特征及找矿方向[J].大地构造与成矿学,2011,35(3):339-347.
[7] 李爱民,穆锡川,张琪彬,等.山东牟平磨山金矿床地质特征及找矿方向[J].山东国土资源,2015,31(12):1-4.
[8] 柳玉明,柳楠,张杰,等.山东金青顶金矿区成矿规律综合研究[J].黄金科学技术,2011,19(3):49-54.
[9] 薛建玲,李胜荣,孙文燕,等.胶东邓格庄金矿地质特征与深部预测[J].中国地质,2012,39(1):183-194.
[10] 邹为雷,曾庆栋,李光明.胶东发云夼金矿床地质特征及其金矿类型辨析[J].矿产地质,2003,22(1):88-94.
[11] 傅良魁.电法勘探教程[M].北京:地质出版社,1983.
[12] 李金铭.地电场与电法勘探[M].北京:地质出版社,1983.
[13] 陈绍求,陈明伟.激发极化法在石英脉型金矿探测中的应用[J].矿产与地质,1999,13(4):245-248.
[14] 闭遗山,张小路,罗润林.高精度磁法和大功率激电在金矿探测中的应用[J].工程地球物理学报,2011,8(6):744-749.
[15] 吴国学,李守义,任云生,等.乌拉嘎金矿主要控矿因素与激电法找金效果[J].地球物理学进展,2006,21(4):1248-1251.
[16] 罗文强,张尚坤,杨斌,等.胶东中朱车金矿区激发极化法找矿效果[J].黄金科学技术,2015,23(1):10-16.

Outlines

/