Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (6): 1720-1739.doi: 10.13278/j.cnki.jjuese.20200250

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Analysis of Structural Characteristics of Mineralization Period in Qingchengzi Baiyun Gold Deposit in Eastern Liaoning

Yu Hua1, Zhao Guochun1, Liu Jianmin2,3, Zhang Jiaqi1, Bi Guangyuan1, Guo Qi1, Fang Xing2,3, Xu Gang2,3, Liu Fuxing4, Huo Yanda1, Bian Huihui1   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. Laboratory of Dynamic Diagenesic and Metallogenesis Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;
    3. Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China;
    4. 103 Brigade of Non-Ferrous Geological Bureau of Liaoning Province, Dandong 118008, Liaoning, China
  • Received:2020-11-03 Online:2021-11-26 Published:2021-11-24
  • Supported by:
    Supported by the National Deep Resource Exploration and Mining Special Project (2016YFC0600108)

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Abstract: The Qingchengzi gold ore concentrated area is located in the Paleoproterozoic Liao-Ji rift zone in the eastern section of the northern margin of the North China craton, it is one of the important gold-rich areas in China, and the Baiyun gold deposit is a representative of the Qingchengzi gold ore concentrated area. The mineral area has large reserves and shallow mining with great prospecting potential. Through methods such as field survey, underground observation, data collection and indoor testing, and the combination of field conditions and indoor analysis, and the combination of macro and micro research methods, the distribution of ore bodies, surrounding rock alteration and mineralization period structural characteristicsare analyzed. The studies show that the deposit is mainly developed in mica schist and metagranulite of the Gaixian Formation in the Liaohe Group. It is a hydrothermal altered rock type gold deposit. The ore body is mainly controlled by the fault structures, and their main trend is east-west and mid-low angle to south, in gentle waves, or long lotus root joints, with the characteristics of reappearance of sharp extinction. The surrounding rocks of ore bodies are altered mainly through silicification, sericinization, graphitization, and chloritization, which are controlled by faults. The ore-conducting and ore-hosting structures are mainly near east-west thrust faults and their derived secondary structures. Through the analysis of the ore-controlling faults in the mineralization period and the distribution of Au grade, it is believed that the tectonic stress field in the mineralization period squeezed in the direction of NW-SE, so the ore bodies are lateral to SW.

Key words: Baiyun gold deposit, structural characteristics, ore body morphology, wall rock alteration, hydrothermal altered rock type gold deposit

CLC Number: 

  • P613
[1] 代军治. 青城子小佟家堡子、林家金矿成矿流体特征及成矿机制[J]. 地质评论,2006,52(6):836-842. Dai Junzhi. The Characteristics of Ore-Forming Fluids and Metallogenic Mechanism of the Xiaotongjiapuzi and Linjia Gold Deposits in Qingchengzi[J]. Geological Review, 2006, 52(6):836-842.
[2] 刘志远,徐学纯. 辽东青城子金银多金属成矿区综合信息找矿模型及找矿远景分析[J]. 吉林大学学报(地球科学版),2007,37(3):437-443. Liu Zhiyuan, Xu Xuechun. Synthetic Information Models and Analyses of Prospecting Perspective of the Qingchengzi Polymetal Metallogenic Mine in Eastern Liaoning Province[J]. Journal of Jilin University(Earth Science Edition), 2007, 37(3):437-443.
[3] 关广岳,金成洙. 白云金矿床的成因[J]. 地质与勘探,1983,10(3):10-20. Guan Guangyue, Jin Chengzhu. Genesis of Baiyun Gold Deposit[J]. Geology and Exploration, 1983, 10(3):10-20.
[4] 赵鸿志,杨沈生,李辉. 白云金矿床地质特征及成因探讨[J]. 有色矿冶,2009,25(3):4-7. Zhao Hongzhi, Yang Shensheng, Li Hui. Discussion on the Geological Characteristics and Genesis of the Baiyun Gold Deposit[J]. Non-Ferrous Mining and Metallurgy, 2009, 25(3):4-7.
[5] 杨新库. 辽宁白云金矿床地质特征及深部找矿的新认识[J]. 矿产与地质,2011,25(5):376-379. Yang Xinku. Geological Characteristics of Baiyun Gold Deposit in Liaoning and New Understanding of Deep Ore Prospecting[J]. Mineral Resources and Geology, 2011, 25(5):376-379.
[6] 魏军,王恩德,刘福兴,等. 辽宁凤城白云金矿带地质特征、矿床成因及找矿方向[J]. 金属矿山, 2019,53(8):120-130. Wei Jun, Wang Ende, Liu Fuxing,et al. Geological Characteristics, Deposit Genesis and Prospecting Direction of Baiyun Gold Ore Belt in Fengcheng, Liaoning[J]. Metal Mine, 2019, 53(8):120-130.
[7] 国家辉,程德琳. 辽宁白云金矿床黄铁矿标型特征及其找矿意义[J]. 贵金属地质,1993,2(2):127-136. Guo Jiahui, Cheng Delin. The Typomorphic Characteristics of Pyrite from Baiyun Gold Deposit in Liaoning and Its Prospecting Significance[J]. Geology of Precious Metals, 1993, 2(2):127-136.
[8] 郝立波,赵昕,赵玉岩. 辽宁白云金矿床稳定同位素地球化学特征及矿床成因[J]. 吉林大学学报(地球科学版),2017,47(2):442-451. Hao Libo, Zhao Xin, Zhao Yuyan. Stable Isotope Geochemical Characteristics and Deposit Genesis of Baiyun Gold Deposit in Liaoning[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(2):442-451.
[9] 赵岩,杨宏智,杨凤超,等. 辽东半岛青城子矿田典型金矿成因:来自硫、氢、氧同位素的证据[J]. 地质与资源,2020,29(1):21-28. Zhao Yan, Yang Hongzhi, Yang Fengchao,et al. Genesis of Typical Gold Deposits in Qingchengzi Ore Field in Liaodong Peninsula:Evidence from Sulfur, Hydrogen and Oxygen Isotopes[J]. Geology and Resources, 2020, 29(1):21-28.
[10] 田豫才. 辽东小佟家堡子金矿床地质特征及成矿机理探讨[J]. 有色金属矿产与勘查,1999,8(5):264-269. Tian Yucai. Discussion on the Geological Characteristics and Metallogenic Mechanism of the Xiaotongjiapuzi Gold Deposit in Eastern Liaoning[J]. Nonferrous Metals Minerals and Prospecting, 1999, 8(5):264-269.
[11] 刘国平,艾永富. 辽宁白云金矿床成矿时代探讨[J]. 岩石学报,2000,16(4):627-632. Liu Guoping, Ai Yongfu. Discussion on the Mineralization Age of the Baiyun Gold Deposit in Liaoning[J]. Acta Petrologica Sinica, 2000, 16(4):627-632.
[12] 张朋,李斌,李杰,等. 辽东裂谷白云金矿载金黄铁矿Re-Os定年及其地质意义[J]. 大地构造与成矿学,2016,40(4):731-738. Zhang Peng, Li Bin, Li Jie, et al. Re-Os Dating of Golden Iron Ore from Baiyun Gold Deposit in Eastern Liaoning Rift and Its Geological Significance[J]. Geotectonica et Metallogenia, 2016, 40(4):731-738.
[13] 杨凤超,宋运红,柴鹏,等. 辽宁白云金矿床成矿流体特征、成矿物质来源及成因研究[J]. 矿物岩石,2017,37(1):30-39. Yang Fengchao, Song Yunhong, Chai Peng, et al.Research on the Characteristics of Ore-Forming Fluids, Sources and Genesis of the Baiyun Gold Deposit in Liaoning[J]. Journal of Mineralogy and Petrology, 2017, 37(1):30-39.
[14] 申永治,胡霭琴. 辽宁中部辽河群K-Ar年龄等值图及其地质意义[J]. 地球化学,1986,15(1):36-41. Shen Yongzhi, Hu Aiqin. K-Ar Age Map of the Liaohe Group in Central Liaoning and Its Geological Significance[J]. Geochemistry, 1986, 15(1):36-41.
[15] 张亚楠,姚富强. 辽宁凤城白云金矿硅钾蚀变岩型金矿的发现及其意义[J]. 西北地质,2013,46(3):122-128. Zhang Yanan, Yao Fuqiang. Discovery and Significance of Silicon-Potassium Altered Rock Type Gold Deposit in Baiyun Gold Deposit, Fengcheng, Liaoning[J]. Northwest Geology, 2013, 46(3):122-128.
[16] 戴立军,樊秉鸿. 辽南早元古宙变质热液型金矿床成矿机理探讨[J]. 辽宁地质,1990,7(2):112-123. Dai Lijun, Fan Binghong. Discussion on the Metallogenic Mechanism of the Metamorphic Hydrothermal Gold Deposit in the Early Proterozoic in Southern Liaoning[J]. Liaoning Geology, 1990,7(2):112-123.
[17] 刘国平,艾永富. 辽宁青城子铅锌银金矿田控矿构造与找矿方向[J]. 矿床地质,2001,20(2):147-152. Liu Guoping, Ai Yongfu. Ore-Controlling Structure and Prospecting Direction of the Lead-Zinc-Silver-Gold Ore Field in Qingchengzi, Liaoning[J]. Mineral Deposits, 2001, 20(2):147-152.
[18] 赵广繁,孙立民. 青城子矿田小佟家堡子金矿床地质特征及成因机制[J]. 有色金属矿产与勘查,1997,6(4):21-26. Zhao Guangfan, Sun Limin. Geological Characteristics and Genetic Mechanism of Xiaotongjiapuzi Gold Deposit in Qingchengzi Ore Field[J]. Nonferrous Metal Minerals and Prospecting, 1997, 6(4):21-26.
[19] 郎福全,陈贺,刘恒刚. 辽宁凤城白云金矿床地质特征及找矿方向[J]. 黄金, 2007, 28(11):16-20. Lang Fuquan, Chen He, Liu Henggang. Geological Characteristics and Prospecting Direction of Baiyun Gold Deposit in Fengcheng, Liaoning[J]. Gold, 2007, 28(11):16-20.
[20] 郝立波,陆继龙,赵玉岩. 辽宁白云金矿床总结研宄报告[R]. 长春:吉林大学,2012:1-115. Hao Libo, Lu Jilong, Zhao Yuyan. Summary Research Report on Baiyun Gold Deposit in Liaoning[R]. Changchun:Jilin University, 2012:1-115.
[21] 孙立民,孙文涛,赵广繁. 青城子矿田小佟家堡子金银矿床地质特征及成矿物质来源探讨[J]. 黄金, 1997,18(12):13-18. Sun Limin, Sun Wentao, Zhao Guangfan. The Geological Characteristics of the Xiaotongjiapuzi Gold-Silver Deposit in Qingchengzi Ore Field and Discussion on the Source of Ore-Forming Materials[J]. Gold, 1997, 18(12):13-18.
[22] 陈旭瑞,刘建明,杨思道,等. 华北克拉通北缘与盆地流体有关的若干矿床实例[J]. 矿物岩石地球化学通报,2000,19(2):109-113. Chen Xurui, Liu Jianming, Yang Sidao,et al. Some Examples of Deposits Related to Basin Fluids in the Northern Margin of the North China Craton[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2000, 19(2):109-113.
[23] 张森,张迪,沙德喜,等. 辽东林家三道沟-小佟家堡子地区金(银)矿成矿特征及成因[J]. 吉林大学学报(地球科学版),2012,42(3):725-732. Zhang Sen, Zhang Di, Sha Dexi,et al. Metallogenetic Characteristics and Genesis of the Gold(Silver) Mineralization in Linjiasandaogou-Xiaotongjiapuzi Area, Eastern Liaoning Province[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(3):725-732.
[24] 徐英奎. 论辽宁凤城白云金矿床动力成矿作用[C]//中国地质科学院沈阳地质矿产研究所文集. 北京:中国地质学会,1991:79-88. Xu Yingkui. On the Dynamic Mineralization of Baiyun Gold Deposit in Fengcheng, Liaoning[C]//Collected Works of Shenyang Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences. Beijing:Geological Society of China, 1991:79-88.
[25] 张宝华,屈奋雄,张鹏程,等. 论韧性剪切带对金矿的控制规律:以辽宁省白云金矿为例[J]. 地质找矿论丛,1996,11(1):8-17. Zhang Baohua, Qu Fenxiong, Zhang Pengcheng, et al. On the Control Law of Ductile Shear Zone on Gold Deposits:Taking Baiyun Gold Deposit in Liaoning Province as an Example[J]. Contributions to Geology and Mineral Resources Research, 1996, 11(1):8-17.
[26] 张拴宏,胡国辉,李建锋,等. 辽东白云-小佟家堡子矿集区控矿构造及成矿有利区预测[J]. 地球科学,2020,45(11):3885-3899. Zhang Shuanhong, Hu Guohui, Li Jianfeng,et al. Liaodong Baiyun-Xiaotongjiapuzi Ore Concentration Area Ore-Controlling Structure and Prediction of Ore-Forming Favorable Areas[J]. Earth Science, 2020, 45(11):3885-3899.
[27] 骆辉,李俊建. 辽东裂谷Au、Ag、Pb、Zn、Cu、Co金属矿床地质特征和成矿条件[J]. 前寒武纪研究进展,2002,25(3/4):240-245. Luo Hui, Li Junjian. Geological Characteristics and Metallogenic Conditions of Au, Ag, Pb, Zn, Cu, Co Metal Deposits in the Eastern Liaoning Rift[J]. Progress in Precambrian Research, 2002, 25(3/4):240-245.
[28] Luo Yan,Sun Min,Zhao Guochun, et al. La-ICP-MS Zircon Ages of the Liaohe Group in the Eastern Block of the North China Craton:Constraints on the Ebolution of the Jiao-Liao-Ji Belte[J]. Precambrian Research, 2004, 134:349-371.
[29] 耿国建,马宝军,丛颖,等.辽宁青城子逆冲推覆构造变形与金矿控矿作用探讨[J]. 黄金科学技术,2016,24(4):26-31. Geng Guojian, Ma Baojun, Cong Ying, et al. Discussion on the Deformation of the Thrust Nappe Structure and the Ore-Controlling Effect of Gold Deposits in Qingchengzi, Liaoning[J]. Gold Science and Technology, 2016, 24(4):26-31.
[30] 王文清,曲亚军. 辽东古元古宙金矿地质特征及成矿模式[J]. 辽宁地质,2000,17(3):161-172. Wang Wenqing, Qu Yajun. Geological Characteristics and Metallogenic Model of Paleoproterozoic Gold Deposits in Eastern Liaoning[J]. Liaoning Geology, 2000, 17(3):161-172.
[31] 翟安民,沈保丰,杨春亮,等. 辽吉古裂谷地质演化与成矿[J]. 地质调查与研究,2005,28(4):213-220. Zhai Anmin, Shen Baofeng, Yang Chunliang, et al. Geological Evolution and Mineralization of Ancient Rifts in Liaoji[J]. Geological Survey and Research, 2005, 28(4):213-220.
[32] 王玉往,解洪晶,李德东,等. 矿集区找矿预测研究:以辽东青城子铅锌-金-银矿集区为例[J]. 矿床地质,2017,36(1):1-24. Wang Yuwang, Xie Hongjing, Li Dedong, et al.Study on Prospecting Prediction of Ore Concentration Area:Taking Qingchengzi Lead-Zinc-Gold-Silver Ore Concentration Area of Liaodong as an Example[J]. Mineral Deposits, 2017, 36(1):1-24.
[33] 刘辉,金成珠. 辽河群片岩建造中构造蚀变带型金矿床成矿条件[J]. 沈阳黄金学院学报,1991,10(3):16-24. Liu Hui, Jin Chengzhu. Metallogenic Conditions of Structural Alteration Zone Type Gold Deposits in the Schist Construction of the Liaohe Group[J]. Journal of Shenyang Institute of Gold Technology, 1991, 10(3):16-24.
[34] 周国超. 辽东白云金矿床成因研究[D]. 昆明:昆明理工大学,2017. Zhou Guochao. Research on the Genesis of Baiyun Gold Deposit in Eastern Liaoning[D]. Kunming:Kunming University of Science and Technology, 2017.
[35] 刘开慧,刘福兴,苏建飞,等. 辽宁凤城荒甸子金矿床地质特征及成因探讨[J]. 吉林地质,2012,31(1):35-40. Liu Kaihui, Liu Fuxing, Su Jianfei, et al. Geological Characteristics and Genesis of the Huangdianzi Gold Deposit in Fengcheng, Liaoning[J]. Jilin Geology, 2012, 31(1):35-40.
[36] 董存杰,张宝琛,董立军. 青城子矿田硅质岩成因探讨[J]. 矿产与地质,2010,24(2):166-171. Dong Cunjie, Zhang Baochen, Dong Lijun. Discussion on the Genesis of Siliceous Rock in Qingchengzi Ore Field[J]. Mineral Resources and Geology, 2010, 24(2):166-171.
[37] 辽宁省有色地质局一零三队. 辽宁省凤城市白云金矿接替资源勘查报告[R]. 凤城:辽宁招金白云黄金矿业有限公司,2011:13-41. No. 103 Team, Non-Ferrous Geology Bureau of Liaoning Province. Investigation Report on Replacement Resources of Baiyun Gold Mine, Fengcheng City, Liaoning Province[R]. Fengcheng:Liaoning Zhaojin Baiyun Gold Mining Limited company, 2011:13-41.
[38] Yu Gang, Chen Jiangfeng, Xue Chunji, et al. Geochronological Framework and Pb, Sr Isotope Geochemistry of the Qingchengzi Pb-Zn-Ag-Au Orefield, Northeastern China[J]. Ore Geology Reviews, 2009, 35(3/4):367-382.
[39] 李德东,罗照华,周久龙,等. 岩墙厚度对成矿作用的约束:以石湖金矿为例[J]. 地学前缘,2011,18(1):166-178. Li Dedong, Luo Zhaohua, Zhou Jiulong, et al. Constraints of Dike Thicknesses on the Metallogenesis and Its Application to the Shihu Gold Deposit[J].Earth Science Frontiers, 2011, 18(1):166-178.
[40] Hawkings A B,Mcconnell B J. Sensitivity of Sandstone Strength and Deformability to Changes in Moisture Content[J]. Quarterly Journal of Engineering Geology and Hydrogeology,1992, 25(2):115-130.
[41] 胡家杰,程小久,曹兴男. 金矿的控矿构造概述[J]. 地质科技情报,1986,5(3):110-113. Hu Jiajie, Cheng Xiaojiu, Cao Xingnan. Overview of the Ore-Controlling Structure of Gold Mines[J]. Geological Science and Technology Information, 1986,5(3):110-113.
[42] 翟裕生,林新多. 矿田构造学[M]. 北京:地质出版社,1993. Zhai Yusheng, Lin Xinduo. Ore Field Tectonics[M]. Beijing:Geological Publishing House, 1993.
[43] 李德东,王玉往,张志超,等. 辽宁白云金矿床成矿构造与成矿结构面特征浅析[J]. 地质力学学报,2019,25(增刊1):10-20. Li Dedong, Wang Yuwang, Zhang Zhichao, et al.Analysis on the Characteristics of Metallogenic Structure and Structural Surface of Baiyun Gold Deposit in Liaoning[J]. Journal of Geomechanics, 2019, 25(Sup.1):10-20.
[44] 胡铁军. 青城子地区金银成矿作用、控矿因素及找矿思路[J]. 地质找矿论丛,2001,16(3):187-191. Hu Tiejun. Gold and Silver Mineralization, Ore-Controlling Factors and Prospecting Ideas in Qingchengzi Area[J]. Contributions to Geology and Mineral Resources Research, 2001, 16(3):187-191.
[45] 曾庆栋,陈仁义,杨进辉,等. 辽东地区金矿床类型、成矿特征及找矿潜力[J]. 岩石学报,2019,35(7):1939-1963. Zeng Qingdong, Chen Renyi, Yang Jinhui, et al. Gold Deposit Types, Metallogenic Characteristics and Prospecting Potential in Eastern Liaoning[J]. Acta Petrologica Sinica, 2019, 35(7):1939-1963.
[46] 林成贵,姚晓峰,程志中,等.辽宁省桃源铅锌矿床成矿物质来源:硫、铅同位素组成特征[J].吉林大学学报(地球科学版),2021,51(1):81-94. doi:10.13278/j. cnki.jjuese.20190117. Lin Chenggui, Yao Xiaofeng, Cheng Zhizhong,et al. Source of Ore-Forming Materials in Taoyuan Pb-Zn Deposit in Liaoning Province:Characteristics of S and Pb Isotopic Compositions[J]. Journal of Jilin University (Earth Science Edition), 2021,51(1):81-94. doi:10.13278/j.cnki.jjuese.20190117.
[47] 陈木森,董永胜,王鹏森,等. 辽东黄花甸地区古元古代变辉绿岩的特征及成因[J].世界地质,2020,39(2):306-321. Chen Musen,Dong Yongsheng,Wang Pengsen,et al. Characteristics and Genesis of Paleoproterozoic Metamorphic Diabase in Huanghuadian Area,Eastern Liaoning Province[J]. Global Geology,2020,39(2):306-321.
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[10] ZHANG Guang-xin, DENG Wei, HE Yan, RAMSIS Salama. An Application of Hydrological Response Units in Assessment of Soil Salinization Risks[J]. J4, 2005, 35(03): 356 -0360 .
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