|
|
The application of integrated geophysical prospecting method to the prospecting for concealed orebodies in the northern area of the Weilasituo copper polymetallic deposit |
Zhen-Liang WANG1,2, You-Mao DENG1,2, Yin-Sheng MENG1,2, Rui-De LIU1,2 |
1. Key Laboratory of Geochemical Exploration, Ministry of Natural Resources, Langfang 065000,China 2. Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang 065000,China |
|
|
Abstract The northern area of the Weilasituo copper polymetallic deposit is covered seriously. It is difficult to find concealed orebody with the surface geological means; therefore, in this paper, based on the study of geological data, the authors investigated the study area by using the comprehensive exploration methods such as gravity, magnetic survey, induced polarization in median gradient array and CSAMT. On such a basis, three faults were detected through inference, two metallogenic prediction target areas were delineated and, by drilling, a concealed orebody was successfully found. The combinational technologies and methods in the search for concealed orebodies in the coverage area was summarized.
|
Received: 27 May 2019
Published: 25 October 2019
|
|
|
|
|
|
The geological setting of the south Great Xing’an Range[33]
|
|
Simplified geological map of the study area
|
岩矿石名称 | 块数 | 密度/(g/cm3) | 磁化率/10-6 SI | 剩磁强度/(/10-3 A/m) | 电阻率/(Ω·m) | 极化率/% | 变化范围 | 平均值 | 变化范围 | 平均值 | 变化范围 | 平均值 | 变化范围 | 平均值 | 变化范围 | 平均值 | 闪长岩 | 31 | 2.544~2.854 | 2.655 | 7.4~9025.9 | 664.5 | 0.1~3576.5 | 153.0 | 925.3~5205.7 | 2832.4 | 0.1~1.2 | 0.4 | 片麻岩 | 35 | 2.618~2.890 | 2.712 | 25.1~10222.7 | 658.1 | 0.1~4314.8 | 157.3 | 198.3~7180.0 | 2690.1 | 0.1~54.0 | 2.7 | 基性脉岩(矿化) | 4 | 3.000~4.514 | 3.500 | 629.2~178041.1 | 46599.8 | 13.8~9448.0 | 3386.7 | 53.5~2174.6 | 773.3 | 0.3~84.9 | 52.1 | 闪长岩(矿化) | 4 | 2.874~4.650 | 3.728 | 54.2~15624.3 | 4076.3 | 0.3~3586.3 | 902.5 | 54.9~257.3 | 147.4 | 6.7~79.7 | 56.0 | 闪锌矿 | 8 | 3.260~4.871 | 4.289 | 4692.4~327656.5 | 58987.0 | 212.7~23488.8 | 8858.2 | 42.0~185.5 | 90.3 | 26.6~94.4 | 71.6 | 铜锌矿 | 6 | 3.699~4.381 | 3.992 | 4008.3~27642.1 | 10874.1 | 22.8~2988.1 | 1112.9 | 18.8~61.2 | 41.4 | 70.7~89.8 | 80.8 | 黄铜矿 | 1 | | 4.227 | | 39632.9 | | 15206.8 | | 40.8 | | 90.5 | 矿体 | 3 | 2.951~4.124 | 3.670 | 15896.4~374226.3 | 135800.0 | 356.5~47985.2 | 17021.3 | | | | |
|
Statistical table of the Rock (Ores) physical properties at the study area
|
|
Engineering layout map of the study area
|
|
Bouguer gravity contour map of the study area (the red dotted lines show inferred faults)
|
|
Magnetic contour map of the study area
|
|
Magnetic contour map of 500 m up extension of the study area
|
|
The contour map of IP apparent polarizability of the study area
|
|
The contour map of IP apparent resistivity of the study area
|
|
Resistivity inversion profile map of CSAMT on Line No.0
|
[1] |
刘翼飞, 樊志勇, 蒋胡灿 , 等. 内蒙古维拉斯托—拜仁达坝斑岩—热液脉状成矿体系研究[J]. 地质学报, 2014,88(12):2373-2385.
|
[1] |
Lie Y F, Fan Z Y, Jiang H C , et al. Genesis of the Weilasituo-Bairendaba porphyry-hydrothermal vein yype system in Inner Mongolia, China[J]. Acta Geologica Sinica, 2014,88(12):2373-2385.
|
[2] |
王玉往, 曲丽莉, 王丽娟 , 等. 大井锡多金属矿床矿化中心的探讨[J]. 地质与勘探, 2002,38(2):23-27.
|
[2] |
Wang Y W, Qu L L, Wang L J , et al. Study on the mineralization center of dajing Tin-Polymetallic deposit, Inner Mongolia[J]. Geology and Prospecting, 2002,38(2):23-27.
|
[3] |
张乾, 战新志, 裘愉卓 , 等. 内蒙古孟恩陶勒盖银铅锌铟矿床的铅同位素组成及矿石铅的来源探讨[J]. 地球化学, 2002,31(3):253-258.
|
[3] |
Zhang Q, Zhan X Z, Qiu Y Z , et al. Lead isotopic composition and lead source of the Meng’entaolegai Ag Pb Zn In deposit in Inner Mongolia[J]. Geochimica, 2002,31(3):253-258.
|
[4] |
陶则熙 . 内蒙古自治区阿尔哈达铅锌矿矿床地质特征[J]. 地质找矿论丛, 2006,21(z1):74-76.
|
[4] |
Tao Z X . Geological characteristics of Arhada lead & Zinc deposit in Dongwuqi county, Inner Mongolia, China[J]. Contributions to Geology and Mineral Resources Research, 2006,21(z1):74-76.
|
[5] |
李振祥, 谢振玉, 刘召 , 等.内蒙古西乌珠穆沁旗花敖包特银铅锌矿矿床地质特征及成因初探[J].地质与资源, 2008, 17(4): 277, 278-281.
|
[5] |
Li Z X, Xie Z Y, Liu Z , et al. Geology and genesis of the HuaaobaoTe lead-Zinc deposit Inner Mongolia [J]. Geology and Resources, 2008, 17(4): 277, 278-281.
|
[6] |
潘小菲, 王硕, 侯增谦 , 等. 内蒙古道伦达坝铜多金属矿床特征研究[J]. 大地构造与成矿学, 2009,33(3):402-410.
|
[6] |
Pan X F, Wang S, Hou Z Q , et al. Geology and metallogenesis of daolundaba copper polymetallic deposits, Inner Mongolia[J]. Geotectonica Et Metallogenia, 2009,33(3):402-410.
|
[7] |
刘军, 武广, 钟伟 , 等. 黑龙江省多宝山斑岩型铜(钼)矿床成矿流体特征及演化[J]. 岩石学报, 2010,26(5):1450-1464.
|
[7] |
Liu J, Wu G, Zhong W , et al. Fluid inclusion study of the Duobaoshan porphyry Cu (Mo) deposit,Heilongjiang Province,China[J]. Acta Petrologica Sinica, 2010,26(5):1450-1464.
|
[8] |
江思宏, 聂凤军, 刘翼飞 , 等. 内蒙古拜仁达坝及维拉斯托银多金属矿床的硫和铅同位素研究[J]. 矿床地质, 2010,29(1):101-112.
|
[8] |
Jiang S H, Niu F J, Liu Y F , et al. Sulfur and lead isotopic compositions of Bairendaba and Weilasituo silver-polymetallic deposits, Inner Mongolia[J]. Mineral Deposits, 2010,29(1):101-112.
|
[9] |
刘翼飞, 聂凤军, 江思宏 , 等. 内蒙古拜仁达坝铅—锌—银矿床:元素分带及其成因[J]. 吉林大学学报:地球科学版, 2012,42(4):1055-1068.
|
[9] |
Liu Y F, Nie F J, Jiang S H , et al. Bairendaba Pb-Zn-Ag Polymetallic deposit in Inner Mongolia:the Mineralization zoning and its origin[J]. Journal of Jilin University:Earth Science Edition, 2012,42(4):1055-1068.
|
[10] |
匡永生, 郑广瑞, 卢民杰 , 等. 内蒙古赤峰市双尖子山银多金属矿床的基本特征[J]. 矿床地质, 2014,33(4):847-856.
|
[10] |
Kuang Y S, Zheng G R, Lu M J , et al. Basic characteristics of Shuangjianzishan sliver polymetallic deposit in Chifeng city, Inner Mongolia[J]. Mineral Deposits, 2014,33(4):847-856.
|
[11] |
吴冠斌, 刘建明, 曾庆栋 , 等. 内蒙古双尖子山铅锌银矿床银的赋存状态及其指示意义[J]. 地学前缘, 2014,21(5):105-115.
|
[11] |
Wu G B, Liu J M, Zeng Q D , et al. Occurrences of silver in the Shuangjianzishan Pb-Zn-Ag deposit and its implications for mineral processing[J]. Earth Science Frontiers, 2014,21(5):105-115.
|
[12] |
陈祥, 肖力 . 内蒙古额仁陶勒盖银矿床地球化学研究[J]. 贵金属地质, 1999,8(3):171-178.
|
[12] |
Chen X, Xiao L . The geochemistry study of erentaolegai silver deposit in inner Mongolia[J]. Journal of Precious Metallic Geology, 1999,8(3):171-178.
|
[13] |
储雪蕾, 霍卫国, 张巽 . 内蒙古林西县大井铜多金属矿床的硫、碳和铅同位素及成矿物质来源[J]. 岩石学报, 2002,18(4):566-574.
|
[13] |
Chu X L, Huo W G, Zhang X S , C, and Pb isotopes and sources of metallogenetic elements of the Dajing Cu-polymetallic deposit in Linxi county, Inner Mongolia[J]. China: Acta Petrologica Sinica, 2002,18(4):566-574.
|
[14] |
朱笑青, 张乾, 何玉良 , 等. 内蒙古孟恩陶勒盖银铅锌铟矿床成因研究[J]. 矿床地质, 2004,23(1):52-60.
|
[14] |
Zhu X Q, Zhang Q, He Y L , et al. Genesis of Meng’entaolegai Ag-Pb-Zn-In polymetallic deposit in Inner Mongolia[J]. Mineral Deposits, 2004,23(1):52-60.
|
[15] |
Beaudoin G, Sangster D F . A descriptive model for silver-lead-zinc veins in clastic meta sedimentary terranes[J]. Economic Geology, 1992,87:1005-1021.
|
[16] |
郑翻身, 蔡红军, 张振法 . 内蒙古拜仁达坝维拉斯托超大型银铅锌矿的发现及找矿意义[J]. 物探与化探, 2006,28(5):13-20,25.
|
[16] |
Zheng F S, Cai H J, Zhang Z F . The discovery of superlarge Silver-Lead-Zinc deposits in Bairendaba and Weilasituo, Inner Mongolia, and its ore-prospecting significance[J]. Geophysical and Geochemical Exploration, 2006,28(5):13-20, 25.
|
[17] |
常勇, 赖勇 . 内蒙古银都银铅锌多金属矿床成矿流体特征及成矿年代学研究[J]. 北京大学学报:自然科学版, 2010,46(4):581-593.
|
[17] |
Chang Y, Lai Y . Study on characteristics of ore forming fluid and chronology in the Yindu Ag-Pb-Zn polymetallic ore deposit, Inner Mongolia[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2010,46:581-593.
|
[18] |
王新宇, 侯青叶, 王瑾 , 等. 内蒙古维拉斯托矿床花岗岩类SHRIMP年代学及Hf同位素研究[J]. 现代地质, 2013,27(1):67-78.
|
[18] |
Wang X Y, Hou Q Y, Wang J , et al. SHRIMP geochronology and Hf Isotope of Zircons from Granitoids of the Weilasituo deposit in Inner Mongolia[J]. Geoscience, 2013,27(1):67-78.
|
[19] |
孙丰月, 王力 . 内蒙拜仁达坝银铅锌多金属矿床成矿条件[J]. 吉林大学学报:地球科学版, 2008,38(3):376-383.
|
[19] |
Sun F Y, Wang L . Ore-forming conditions of bairendaba Ag-Pb-Zn polymetallic ore deposit, Inner Mongolia[J]. Journal of Jilin University:Earth Science Edition, 2008,38(3):376-383.
|
[20] |
郭利军, 葛昌宝, 冯贞 , 等. 内蒙古锡林浩特东部拜仁达坝银铅多金属矿勘查过程及远景评述[J]. 物探与化探, 2004,( 5):394-397,401.
|
[20] |
Guo L J, Ge C B, Feng Z , et al. The exploration process and prospects of the Bairendaba Ag-Pb polymetallic deposit in eastern xilin hot, inner Mongolia[J]. Geophysical and Geochemical Exploration, 2004,( 5):394-397,401.
|
[21] |
刘家军, 邢永亮, 王建平 , 等. 内蒙拜仁达坝超大型Ag-Pb-Zn多金属矿床中针硫锑铅矿的发现与成因意义[J]. 吉林大学学报:地球科学版, 2010,40(3):565-572.
|
[21] |
Liu J J, Xing Y L, Wang J P , et al. Discovery of falkmanite from the Bairendaba superlarge Ag-Pb-Zn polymetallic deposit, Inner Mongolia and its origin significance[J]. Journal of Jilin University:Earth Science Edition, 2010,40(3):565-572.
|
[22] |
邵济安, 刘福田, 陈辉 , 等. 大兴安岭—燕山晚中生代岩浆活动与俯冲作用关系[J]. 地质学报, 2001,75(1):56-63.
|
[22] |
Shao J A, Liu F T, Chen H , et al. Relationgship between mesozoic magmatism and subduction in Da Hinggan-Yanshan area[J]. Acta Geologica Sinica, 2001,75(1):56-63.
|
[23] |
刘建明, 张锐, 张庆洲 . 大兴安岭地区的区域成矿特征[J]. 地学前缘, 2004,11(1):269-277.
|
[23] |
Liu J M, Zhang R, Zhang Q Z . The regional metallogeny of Da Hinggan Ling, China[J]. Earth Science Frontiers, 2004,11(1):269-277.
|
[24] |
孟银生, 杨立强, 张瑞忠 , 等. 第四系覆盖区深部热液脉型矿体综合地球物理方法定位预测——内蒙古维拉斯托矿区北侧隐伏矿体勘查例析[J]. 地球学报, 2016,37(6):745-755.
|
[24] |
Meng Y S, Yang L Q, Zhang R Z , et al. Application of integrated geophysical methods to the prospecting for concealed hydrothermal vein-type orebodies beneath Quaternary Sediments:a case study of the northern area of the Weilasituo Copper polymetallic deposit[J]. Acta Geoscientia Sinica, 2016,37(6):745-755.
|
[25] |
Guo F, Fan W, Li C , et al. Early cretaceous highly positive Nd felsic volcanic rocks from the Hinggan Mountains, NE China: origin and implications for Phanerozoic crustal growth[J]. International Journal of Earth Sciences, 2009,98(6):1395-1411.
|
[26] |
Zheng J H, Gao S, Ge W C , et al. Geochronology of the Mesozoic volcanic rocks in the Great Xing’an Range, northeastern China: Implications for subduction-induced delamination[J]. Chemical Geology, 2010,276(3-4):144-165.
|
[27] |
毛景文, 谢桂青, 张作衡 , 等. 中国北方中生代大规模成矿作用的期次及其地球动力学背景[J]. 岩石学报, 2005,21(1):168-188.
|
[27] |
Mao J W, Xie G Q, Zhang Z H , et al. Mesozoic large-scale metallogenic pulses in north China and corresponding geodynamic settings[J]. Acta Petrologica Sinica, 2005,21(1):168-188.
|
[28] |
Jahn B M, Wu F Y, Chen B . Granitoids of the central Asian Orogenic Belt and continental growth in the Phanerozoic[J]. Transactions of the Royal Society of Edinburgh. Earth Sciences, 2000,91:181-193.
|
[29] |
Zhao D, Maruyama S, Omori S . Mantle dynamics of western pacific and east Asia: insight from seismic tomography and mineral physics[J]. Gondwana Research, 2007,11(1-2):120-131.
|
[30] |
Zhu R, Zheng T . Destruction geodynamics of the north China craton and its paleoproterozoic plate tectonics[J]. Science Bulletin, 2009,54(19):3354-3366.
|
[31] |
孙爱群, 牛树银, 马宝军 , 等. 内蒙古拜仁达坝与维拉斯托银多金属矿床成矿构造对比[J]. 吉林大学学报:地球科学版, 2011,41(6):1784-1793.
|
[31] |
Sun A Q, Niu S Y, Ma B J , et al. A comparative study of ore-forming structures in Bairendaba and Weilasituo Silver-Polymetallic deposits of Inner Mongolia[J]. Journal of Jilin University:Earth Science Edition, 2011,41(6):1784-1793.
|
[32] |
Meng Q R . What drove late Mesozoic extension of the northern China-mongolia tract?[J]. Tectonophysices, 2003,369:155-174.
|
[33] |
Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Pennian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt [J]. Tectonic, 2003, 22(6): l- 8, 20.
|
[34] |
郭灵俊, 赵志军, 崔来旺 , 等. 内蒙古阿巴嘎旗北部铜多金属矿地质矿产特征及找矿方向[J]. 地球学报, 2011,32(1):57-63.
|
[34] |
Guo L J, Zhao Z J, Cui L W , et al. Geological and mineral resource characteristics and oreprospect of Cu-polymetallic deposits in the northern part of Abag Banner, Inner Mongolia[J]. Acta Geoscientica Sinica, 2011,32(1):57-63.
|
[35] |
熊小松, 高锐, 张兴洲 , 等. 深地震探测揭示的华北及东北地区莫霍面深度[J]. 地球学报, 2011,32(01):46-56.
|
[35] |
Xiong X S, Gao R, Zhang X Z , et al. The moho depth of north China and northeast China revealed by seismic detection[J]. Acta Geoscientica Sinica, 2011,32(01):46-56.
|
[36] |
Yang L Q, Deng J, Guo L N , et al. Origin and evolution of ore fluid, and gold-deposition processes at the giant Taishang gold deposit, Jiaodong Peninsula, eastern China[J]. Ore Geology Reviews, 2016,72:585-602.
|
[37] |
王长明, 张寿庭, 邓军 . 大兴安岭南段铜多金属矿成矿时空结构[J]. 成都理工大学学报 :自然科学版, 2006,33(05):478-484.
|
[37] |
Wang C M, Zhang S T, Deng J . The metallogenic space-time structure of copper-polymetallic deposits in the southern segment of Da Hinggan Mountains, China[J]. Journal of Chengdu University of Technology:Science & Technology Edition, 2006,33(05):478-484.
|
[38] |
张万益, 聂凤军, 刘树文 , 等. 大兴安岭南段西坡金属矿床特征及成矿规律[J]. 中国地质, 2013,40(5):1583-1599.
|
[38] |
Zhang W Y, Nie F J, Liu S W , et al. Characteristics and metallogenic regularities of ore deposits on the western slope of the southern section of the Da Hinggan Mountains metallogenic belt[J]. Geology in China, 2013,40(5):1583-1599.
|
[1] |
CHEN Da-Lei, WANG Run-Sheng, HE Chun-Yan, WANG Xun, YIN Zhao-Kai, YU Jia-Bin. Application of integrated geophysical exploration in deep spatial structures: A case study of Jiaodong gold ore concentration area[J]. Geophysical and Geochemical Exploration, 2022, 46(1): 70-77. |
[2] |
YANG Jing, GUO Liang-Hui. A modified interpolation-iteration method for gravity anomaly continuation from undulating surface to plane[J]. Geophysical and Geochemical Exploration, 2022, 46(1): 123-129. |
|
|
|
|