Volume 42 Issue 2
Mar.  2023
Turn off MathJax
Article Contents
Hai Lianfu, Tao Rui, Zhang Xiaojun, Liu Anlu, Liu Jinke, Wei Junhao, Bai Jinhe, Li Haifeng. Prospecting model and metallogenic prediction of the Jinchangzi gold deposit in the Weiningbeishan area, Ningxia[J]. Bulletin of Geological Science and Technology, 2023, 42(2): 19-32. doi: 10.19509/j.cnki.dzkq.2022.0250
Citation: Hai Lianfu, Tao Rui, Zhang Xiaojun, Liu Anlu, Liu Jinke, Wei Junhao, Bai Jinhe, Li Haifeng. Prospecting model and metallogenic prediction of the Jinchangzi gold deposit in the Weiningbeishan area, Ningxia[J]. Bulletin of Geological Science and Technology, 2023, 42(2): 19-32. doi: 10.19509/j.cnki.dzkq.2022.0250

Prospecting model and metallogenic prediction of the Jinchangzi gold deposit in the Weiningbeishan area, Ningxia

doi: 10.19509/j.cnki.dzkq.2022.0250
  • Received Date: 12 May 2022
  • The Weiningbeishan area in the eastern section of the North Qilian orogenic belt is one of the areas with the best metallogenic conditions and the most metallogenic signs of gold polymetallic deposits in Ningxia. In recent years, the Jinchangzi gold deposit is one of the breakthroughs in exploration work in this area. Based on the previous data, this paper summarizes the ore-controlling factors and prospecting indicators of the Jinchangzi gold deposit. A multielement comprehensive prospecting model based on geological-geophysical-geochemical prospecting was constructed, and the mining area and surrounding prospecting target areas were delineated. The research shows that the ore-controlling factors of the Jinchangzi gold deposit are mainly stratigraphic and structural. Stratigraphic factor is mainly manifested in specific strata and lithological combinations, and structural factor is mainly controlled by east-west regional faults and their secondary fissures. Hematitization-limonitization, silicification, sericitization, pyritization, jarosite alteration and other surrounding rock alterations, Au-Ag-As-Sb geochemical anomalies, and medium resistivity and medium-high polarizability anomalies are the main prospecting indicators in this area. Based on ore-controlling factors and prospecting indicators, a comprehensive gold prospecting model suitable is proposed for this area. 6 prospecting target areas and 3 deep prospecting target areas are delineated based on this model. Through the geochemical profile and the deep drilling of the target area, the rationality of target area has been confirmed, providing a well tool for future prospecting work in this area.

     

  • loading
  • [1]
    海连富, 刘安璐, 陶瑞, 等. 宁夏卫宁北山金场子金矿床流体来源及矿床成因: 来自流体包裹体和C-H-O同位素证据[J]. 地球科学, 2021, 46(12): 4272-4290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202112005.htm

    Hai L F, Liu A L, Tao R, et al. Source of fluid and genesis of Jinchangzi gold deposit in Weiningbeishan, Ningxia: Evidence from fluid inclusions and C-H-O isotopes[J]. Earth Science, 2021, 46 (12): 4272-4290(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202112005.htm
    [2]
    徐国风. 论宁夏金场子渗流热卤水-表生改造型金矿床的矿源[J]. 地球科学: 中国地质大学学报, 1988, 13(2): 147-153. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198802006.htm

    Xu G F. On the ore source of Jinchangzi seepage hot brine-supergene reformed gold deposit, Ningxia[J]. Earth Science: Journal of China University of Geosciences, 1988, 13(2): 147-153(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198802006.htm
    [3]
    邱朝霞. 宁夏金场子金矿床氧化带中微细金球特征[J]. 地质与勘探, 1989, 25(8): 39-42. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT198908011.htm

    Qiu Z X. Characteristics of fine gold spheres in the oxidation zone of the Jinchangzi gold deposit, Ningxia[J]. Geology and Exploration, 1989, 25(8): 39-42(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT198908011.htm
    [4]
    刘勇, 李廷栋, 王彦斌, 等. 宁夏卫宁北山金场子闪长玢岩岩脉地质特征及SHRIMP锆石U-Pb年龄[J]. 中国地质, 2010, 37(6): 1575-1583. doi: 10.3969/j.issn.1000-3657.2010.06.004

    Liu Y, Li T D, Wang Y B, et al. Geological characteristics and SHRIMP zircon U-Pb age of Jinchangzi diorite porphyrite dikes in Beishan, Weining, Ningxia[J]. Geology in China, 2010, 37(6): 1575-1583(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2010.06.004
    [5]
    艾宁, 任战利, 李文厚, 等. 宁夏卫宁北山地区矿床类型及成矿时代[J]. 矿床地质, 2011, 30(5): 941-948. doi: 10.3969/j.issn.0258-7106.2011.05.015

    Ai N, Ren Z L, Li W H, et al. Metallogenic epoch and ore-forming types of ore deposits in Weiningbeishan area, Ningxia[J]. Mineral Deposits, 2011, 30(5): 941-948(in Chinese with English abstract). doi: 10.3969/j.issn.0258-7106.2011.05.015
    [6]
    艾宁. 宁夏卫宁北山金场子金矿矿床地质与地球化学研究[D]. 西安: 西北大学, 2014.

    Ai N. Studies on the geochemical and geological characteristics of Weiningbeishan Jingcahngzi gold deposit[D]. Xi'an: Northwest University, 2014(in Chinese with English abstract).
    [7]
    仲佳鑫, 李欢, 李鹏, 等. 宁夏卫宁北山金场子金矿床地质特征与控矿因素分析[J]. 西北地质, 2012, 45(3): 81-92. doi: 10.3969/j.issn.1009-6248.2012.03.011

    Zhong J X, Li H, Li P, et al. Geological characteristics and ore-controlling factors of Jinchangzi gold deposit in Beishan, Weining, Ningxia[J]. Northwest Geology, 2012, 45(3): 81-92(in Chinese with English abstract). doi: 10.3969/j.issn.1009-6248.2012.03.011
    [8]
    朱丹, 刘天佑, 代小强. 宁夏卫宁北山金场子-二人山岩体重磁资料处理解释[J]. 工程地球物理学报, 2015, 12(6): 766-771. https://www.cnki.com.cn/Article/CJFDTOTAL-GCDQ201506011.htm

    Zhu D, Liu T Y, Dai X Q, et al. Processing and interpretation of gravity magnetic data of Jinchangzi-Erren Mountain rocks in Weining Beishan, Ningxia[J]. Journal of Engineering Geophysics, 2015, 12(6): 766-771(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GCDQ201506011.htm
    [9]
    翟裕生, 邓军, 李晓波. 区域成矿学[M]. 北京: 地质出版社, 1999.

    Zhai Y S, Deng J, Li X B. Regional mineralogy[M]. Beijing: Geological Publishing House, 1999(in Chinese).
    [10]
    潘桂棠, 陆松年, 肖庆辉, 等. 中国大地构造阶段划分和演化[J]. 地学前缘, 2016, 23(6): 1-23. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201606006.htm

    Pan G T, Lu S N, Xiao Q H, et al. The division and evolution of tectonic stages in China[J]. Geoscience Frontier, 2016, 23(6): 1-23(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201606006.htm
    [11]
    霍福臣, 潘行适, 尤国林, 等. 宁夏地质概论[M]. 北京: 科学出版社, 1989.

    Huo F C, Pan H S, You G L, et al. Introduction to Ningxia geology[M]. Beijing: Science Press, 1989(in Chinese).
    [12]
    郭佩, 刘池洋, 韩鹏, 等. 鄂尔多斯盆地西南缘下-中侏罗统碎屑锆石U-Pb年代学及其地质意义[J]. 大地构造与成矿学, 2017, 41(5): 892-907. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201705008.htm

    Guo P, Liu C Y, Han P, et al. Lower-Middle Jurassic detrital zircon U-Pb chronology of the southwestern margin of the Ordos Basin and its geological significance[J]. Geotectonics and Mineralization, 2017, 41(5): 892-907(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201705008.htm
    [13]
    徐志刚. 中国成矿区带划分方案[M]. 北京: 地质出版社, 2008.

    Xu Z G. China's metallogenic belt division scheme[M]. Beijing: Geological Publishing House, 2008(in Chinese).
    [14]
    敬万林, 徐国风. 宁夏中卫县金场子金矿床控矿条件及成因研究报告[R]. 银川: 宁夏地矿局矿产地质调查所, 1987.

    Jing W L, Xu G F. Research report on ore-controlling conditions and genesis of the Jinchangzi gold deposit in Zhongwei County, Ningxia[R]. Yinchuan: Mineral Geological Survey, Ningxia Bureau of Geology and Mineral Resources, 1987(in Chinese).
    [15]
    Cao H, Sun Z, Jiang Z, et al. Source origin and ore-controlling factors of hydrothermal sulfides from the Tianzuo hydrothermal field, Southwest Indian Ridge[J]. Ore Geology Reviews, 2021, 134(8): 104168.
    [16]
    Muchez P, Corbella M. Factors controlling the precipitation of copper and cobalt minerals in sediment-hosted ore deposits: Advances and restrictions[J]. Journal of Geochemical Exploration, 2012, 118: 38-46. doi: 10.1016/j.gexplo.2012.04.006
    [17]
    赵鹏大, 池顺都, 李志德, 等. 矿床勘查理论与方法[M]. 武汉: 中国地质大学出版社, 2001.

    Zhao P D, Chi S D, Li Z D, et al. Theory and method of ore exploration[M]. Wuhan: China University of Geosciences Press, 2001(in Chinese).
    [18]
    迟清华, 鄢明才. 应用地球化学元素丰度数据手册[M]. 北京: 地质出版社, 2007.

    Chi Q H, Yan M C. Applied geochemical element abundance data handbook[M]. Beijing: Geological Publishing House, 2007(in Chinese).
    [19]
    李水平, 袁杨森, 司建涛, 等. 坦桑尼亚姆瓦莫拉金矿综合找矿模式[J]. 中国地质, 2016, 43(4): 1409-1419. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201604025.htm

    Li S P, Yuan Y S, Si J T, et al. Comprehensive prospecting model of Mwamora gold deposit in Tanzania[J]. Geology in China, 2016, 43(4): 1409-1419(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201604025.htm
    [20]
    Zheng Y Y, Sun X, Gao S B, et al. Analysis of stream sediment data for exploring the Zhunuo porphyry Cu deposit, southern Tibet[J]. Journal of Geochemical Exploration, 2014, 143: 19-30.
    [21]
    Darehshiri A, Panji M, Mokhtari A R. Identifying geochemical anomalies associated with Cu mineralization in stream sediment samples in Gharachaman area, northwest of Iran[J]. Journal of African Earth Sciences, 2015, 110: 92-99.
    [22]
    Zuluaga M C. Stream sediment geochemical mapping of the Mount Pinatubo-Dizon Mine area, the Philippines: Implications for mineral exploration and environmental risk[J]. Journal of Geochemical Exploration, 2017, 175: 18-35.
    [23]
    Gong Q J, Li J Z, Xiang Y C, et al. Determination and classification of geochemical anomalies based on backgrounds and cutoff grades of trace elements: A case study in South Nanling Range, China[J]. Journal for Geochemical Exploration, 2018, 194: 44-51.
    [24]
    Farahbakhsh E, Chandra R, Eslamkish T, et al. Modeling geochemical anomalies of stream sediment data through a weighted drainage catchment basin method for detecting porphyry Cu-Au mineralization[J]. Journal for Geochemical Exploration, 2019, 204: 13-32.
    [25]
    Yang F, Wang G, Santosh M, et al. Delineation of potential exploration targets based on 3D geological modeling: A case study from the Laoangou Pb-Zn-Ag polymetallic ore deposit, China[J]. Ore Geology Reviews, 2017, 89: 228-252.
    [26]
    娄渝明. 基于地质三维建模的西藏雄村矿区2号矿体深部资源定量预测[D]. 成都: 成都理工大学, 2019.

    Lou Y M. Quantitative prediction of deep resources of Xiongcun No. 2 deposit based on geological 3D modeling[D]. Chengdu: Chengdu University of Technology, 2019(in Chinese with English abstract).
    [27]
    陈麒玉, 刘刚, 何珍文, 等. 面向地质大数据的结构-属性一体化三维地质建模技术现状与展望[J]. 地质科技通报, 2020, 39(4): 51-58. doi: 10.19509/j.cnki.dzkq.2020.0407

    Chen Q Y, Liu G, He Z W, et al. Current situation and prospect of structure-attribute integrated 3D geological modeling technology for geological big data[J]. Bulletin of Geological Science and Technology, 2020, 39(4): 51-58 (in Chinese with Englishabstract). doi: 10.19509/j.cnki.dzkq.2020.0407
    [28]
    陈国旭, 田宜平, 张夏林, 等. 基于勘探剖面的三维地质模型快速构建及不确定性分析[J]. 地质科技情报, 2019, 38(2): 275-280. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201902033.htm

    Chen G X, Tian Y P, Zhang X L, et al. Rapid construction and uncertainty analysis of 3D geological models based on exploration sections[J]. Geological Science and Technology Information, 2019, 38(2): 275-280(in Chinese with English abstract https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201902033.htm
    [29]
    李章林, 吴冲龙, 张夏林, 等. 地质科学大数据背景下的矿体动态建模方法探讨[J]. 地质科技通报, 2020, 39(4): 59-68. doi: 10.19509/j.cnki.dzkq.2020.0408

    Li Z L, Wu C L, Zhang X L, et al. Discussion on dynamic ore-body modeling with geological science big data[J]. Bulletin of Geological Science and Technology, 2020, 39(4): 59-68(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2020.0408
    [30]
    Wang C, Wang G, Liu J, et al. 3D geochemical modeling for subsurface targets of Dashui Au deposit in western Qinling (China)[J]. Journal of Geochemical Exploration, 2019, 203: 59-77.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article Views(448) PDF Downloads(83) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return