Turn off MathJax
Article Contents
Article Navigation >  Rhhz Test  > 2022  > Accepted Manuscript
YU Xi-huan, SHI Guo-ming, FU An-zong, LI Xin-peng, SUN Jiang-jun, YIN Guo-liang, LIN Ze-fu. ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE[J]. Rhhz Test. doi: 10.13686/j.cnki.dzyzy.2022.05.002
Citation: YU Xi-huan, SHI Guo-ming, FU An-zong, LI Xin-peng, SUN Jiang-jun, YIN Guo-liang, LIN Ze-fu. ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE[J]. Rhhz Test. doi: 10.13686/j.cnki.dzyzy.2022.05.002
shu

ZIRCON U-PB AGE AND TECTONIC SETTING OF THE MIDDLE ORDOVICIAN INTRUSIVE ROCKS IN DUOBAOSHAN AREA, HEILONGJIANG PROVINCE

doi: 10.13686/j.cnki.dzyzy.2022.05.002

  • Natural Resources Survey Institute of Heilongjiang Province, Harbin 150036, China

  • Received Date: 2021-06-02
  • Rev Recd Date: 2021-07-12
    • Available Online: 2022-11-09
    Abstract
  • The Duobaoshan area is located in Zhalantun-Duobaoshan island arc tectonic belt in the eastern section of Xing'an-Mongolian orogenic belt, with the Early Paleozoic geological bodies developed and closely related to regional mineralization. The formation age, tectonic setting and mineralization are discussed based on the study of petrography, lithogeochemistry and isotopic chronology of the Middle Ordovician intrusive rocks in Duobaoshan area. The LA-MC-ICP-MS zircon U-Pb age of granodiorites is 488±3 Ma, indicating that the granodiorites were formed in the Middle Ordovician. The magma source is mainly mantle origin with some crust-derived materials. With intensive tectonic thermal events and magmatic intrusion-eruption activities, a large number of deep fluids bring metallogenic elements such as Au and Cu to form Duobaoshan Cu-Mo deposit under favorable minerogenetic conditions and expanded space.

     

    • FullText(HTML)
  • loading
    • References(29)
  • [1]
    赵忠海, 郑卫政, 曲晖, 等. 黑龙江多宝山地区铜金成矿作用及成矿规律[J]. 矿床地质, 2012, 31(3): 601-614.

    Zhao Z H, Zheng W Z, Qu H, et al. Cu-Au mineralization and metallogenic regularity of Duobaoshan area, Heilongjiang Province[J]. Mineral Deposits, 2012, 31(3): 601-614.
    [2]
    (in Chinese) 杜琦, 赵玉明, 卢秉刚, 等. 多宝山斑岩铜矿床[M]. 北京: 地质出版社, 1988: 62-74.

    Du Q, Zhao Y M, Lu B G, et al. Porphyry copper deposit in Duobaoshan [M]. Beijing: Geological Publishing House, 1988: 62-74.
    [3]
    赵一鸣, 毕承思, 邹晓秋, 等. 黑龙江多宝山、铜山大型斑岩铜(钼)矿床中辉钼矿的铼-锇同位素年龄[J]. 地球学报——中国地质科学院院报, 1997, 18(1): 61-67.

    Zhao Y M, Bi C S, Zou X Q, et al. The Re-Os isotopic age of molybdenite from Duobaoshan and Tongshan porphyry copper (molybdenum) deposits[J]. Acta Geoscientia Sinica — Bulletin of the Chinese Academy of Geological Sciences, 1997, 18(1): 61-67.
    [4]
    尹冰川, 冉清昌. 多宝山超大型铜矿床的成矿构造环境[J]. 矿物学报, 1997, 17(2): 220-224.

    Yin B C, Ran Q C. The tectonic environments of metallogenesis of Duobaoshan superlarge copper deposit[J]. Acta Mineralogica Sinica, 1997, 17(2): 220-224.
    [5]
    (in Chinese) 韩振新, 徐衍强, 郑庆道. 黑龙江省重要金属和非金属矿产的成矿系列及其演化[M]. 哈尔滨: 黑龙江人民出版社, 2004: 69-76.

    Han Z X, Xu Y Q, Zheng Q D. Metallogenic series and evolution of significant metallic and non-metallic minerals in Heilongjiang Province [M]. Harbin: Heilongjiang People's Publishing House, 2004: 69-76.
    [6]
    (in Chinese) 杜琦, 马晓阳, 韩成满, 等. 斑岩铜矿成因探讨[M]. 北京: 地质出版社, 2008: 15-22.

    Du Q, Ma X Y, Han C M, et al. Discussion on the genesis of porphyry copper deposit[M]. Beijing: Geological Publishing House, 2008: 15-22.
    [7]
    王宝权. 黑龙江省争光岩金矿床地质特征及找矿标志[J]. 地质与资源, 2016, 25(3): 244-249, 253.

    Wang B Q. Geological characteristics and prospecting indicators of the Zhengguang gold deposit in Heilongjiang Province[J]. Geology and Resources, 2016, 25(3): 244-249, 253.
    [8]
    李成禄, 曲晖, 赵忠海, 等. 黑龙江省霍龙门地区成矿地质特征及潜力分析[J]. 地质与资源, 2013, 22(4): 273-278, 329.

    Li C L, Qu H, Zhao Z H, et al. Metallogenic characteristics and potential of Huolongmen area in Heilongjiang Province[J]. Geology and Resources, 2013, 22(4): 273-278, 329.
    [9]
    杨福深, 李成禄, 石国明, 等. 试论黑龙江省多宝山-霍龙门地区早古生代NW向造山带的存在及其控岩控矿意义[J]. 矿产与地质, 2019, 33(2): 191-202.

    Yang F S, Li C L, Shi G M, et al. Existence of early Paleozoic NW-trending orogenic belt and its geo-significance in Duobaoshan-Huolongmen area, Heilongjiang[J]. Mineral Resources and Geology, 2019, 33(2): 191-202.
    [10]
    崔根, 王金益, 张景仙, 等. 黑龙江多宝山花岗闪长岩的锆石SHRIMP U-Pb年龄及其地质意义[J]. 世界地质, 2008, 27(4): 387-394.

    Cui G, Wang J Y, Zhang J X, et al. U-Pb SHRIMP dating of zircons from Duobaoshan granodiorite in Heilongjiang and its geological significance[J]. Global Geology, 2008, 27(4): 387-394.
    [11]
    曲晖, 赵忠海, 李成禄, 等. 黑龙江永新金矿地质特征及成因[J]. 地质与资源, 2014, 23(6): 520-524.

    Qu H, Zhao Z H, Li C L, et al. Geology and genesis of the Yongxin gold deposit in Heilongjiang Province[J]. Geology and Resources, 2014, 23(6): 520-524.
    [12]
    向安平, 杨郧城, 李贵涛, 等. 黑龙江多宝山斑岩Cu-Mo矿床成岩成矿时代研究[J]. 矿床地质, 2012, 31(6): 1237-1248.

    Xiang A P, Yang Y C, Li G T, et al. Diagenetic and metallogenic ages of Duobaoshan porphyry Cu-Mo deposit in Heilongjiang Province [J]. Mineral Deposits, 2012, 31(6): 1237-1248.
    [13]
    赵焕利, 朱春艳, 刘海洋, 等. 黑龙江多宝山铜矿床中花岗闪长岩锆石SHRIMP U-Pb测年及其构造意义[J]. 地质与资源, 2012, 21 (5): 421-424.

    Zhao H L, Zhu C Y, Liu H Y, et al. Zircon SHRIMP U-Pb dating and its tectonic implications of the granodiorite in Duobaoshan copper deposit, Heilongjiang Province[J]. Geology and Resources, 2012, 21 (5): 421-424.
    [14]
    刘军, 周振华, 何哲峰, 等. 黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征[J]. 矿床地质, 2015, 34(2): 289-308.

    Liu J, Zhou Z H, He Z F, et al. Zircon U-Pb dating and geochemistry of ore-bearing tonalite in Tongshan copper deposit, Heilongjiang Province[J]. Mineral Deposits, 2015, 34(2): 289-308.
    [15]
    张璟, 邵军, 杨宏智, 等. 东北扎兰屯奥陶纪碱性辉长岩锆石U-Pb年代学证据[J]. 中国地质, 2017, 44(3): 616-617.

    Zhang J, Shao J, Yang H Z, et al. U-Pb chronological evidence from zircons of Ordovician essexite in Zhalantun area, Northeast China [J]. Geology in China, 2017, 44(3): 616-617.
    [16]
    汪岩, 杨晓平, 那福超, 等. 嫩江-黑河构造带中花岗质糜棱岩的确定及地质意义[J]. 地质与资源, 2013, 22(6): 452-459.

    Wang Y, Yang X P, Na F C, et al. Determination and geological implication of the granitic mylonite in Nenjiang-Heihe tectonic belt [J]. Geology and Resources, 2013, 22(6): 452-459.
    [17]
    刘宝山, 杨晓平, 李成禄. 黑龙江省嫩江三合屯韧性剪切带与金矿化[J]. 矿产与地质, 2017, 31(3): 503-506, 513.

    Liu B S, Yang X P, Li C L. Ductile shear zone and gold mineralization of Sanhetun gold deposit in Nenjiang, Heilongjiang Province[J]. Mineral Resources and Geology, 2017, 31(3): 503-506, 513.
    [18]
    郝士龙, 李成禄, 胡忠贤. 黑龙江省嫩江市播根里地区地球化学异常特征及找矿潜力[J]. 地质与资源, 2020, 29(5): 419-428, 410.

    Hao S L, Li C L, Hu Z X. Geochemical anomaly characteristics and prospecting potential in Bogenli area of Nenjiang City, Heilongjiang Province[J]. Geology and Resources, 2020, 29(5): 419-428, 410.
    [19]
    宋国学, 秦克章, 王乐, 等. 黑龙江多宝山矿田争光金矿床类型、U-Pb年代学及古火山机构[J]. 岩石学报, 2015, 31(8): 2402-2416.

    Song G X, Qin K Z, Wang L, et al. Type, zircon U-Pb age and paleovolcano edifice of Zhengguang gold deposit in Duobaoshan orefield in Heilongjiang Province, NE-China[J]. Acta Petrologica Sinica, 2015, 31(8): 2402-2416.
    [20]
    杨晓平, 汪岩, 那福超, 等. 嫩江-黑河晚古生代碰撞过程的岩石构造建造学响应[J]. 世界地质, 2017, 36(4): 1064-1071.

    Yang X P, Wang Y, Na F C, et al. Petrologic-tectonic formation response of Late Paleozoic collision process in Nenjiang-Heihe area [J]. Global Geology, 2017, 36(4): 1064-1071.
    [21]
    杨泽黎, 王树庆, 胡晓佳. 1∶ 2 500 000华北侵入岩地质图空间数据库[J]. 中国地质, 2020, 47(S1): 1-10.

    Yang Z L, Wang S Q, Hu X J. Spatial Database of 1∶ 2 500 000 Geologic Map of the Intrusions in North China[J]. Geology in China, 2020, 47 (S1): 1-10.
    [22]
    张国宾, 韩超, 杨言辰, 等. 完达山地块跃进山矽卡岩型铜金矿区酸性侵入岩锆石U-Pb年龄、地球化学特征及成因[J]. 中国地质, 2018. 45(5): 977-991.

    Zhang G B, Han C, Yang Y C, et al. Zircon U-Pb age, geochemistry and genesis of acid intrusive rocks in the Yuejinshan skarn type copper-gold deposit, Wandashan block[J]. Geology in China, 2018, 45(5): 977-991.
    [23]
    于喜洹, 李新鹏, 陈旭峰, 等. 大兴安岭潮满林场地区新元古代花岗质片麻岩——锆石U-Pb测年、地球化学特征及构造环境探讨[J]. 地质与资源, 2022, 31(2): 123-130.

    Yu X H, Li X P, Chen X F, et al. The Neoproterozoic granitic gneiss in Chaoman Forest Farm area of Daxinganling Mountains: Zircon U-Pb dating, geochemistry and tectonic environment[J]. Geology and Resources, 2022, 31(2): 123-130.
    [24]
    Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643.
    [25]
    Rickwood P C. Boundary lines within petrologic diagrams which use oxides of major and minor elements[J]. Lithos, 1989, 22(4): 247-263.
    [26]
    (in Chinese) 韩振新, 郝正平, 侯敏, 等. 黑龙江省主要成矿带矿床成矿系列[M]. 哈尔滨: 哈尔滨工程大学出版社, 1996: 97-106, 151.

    Han Z X, Hao Z P, Hou M, et al. Metallogenic series of main metallogenic belts in Heilongjiang Province[M]. Harbin: Harbin Engineering University Press, 1996: 97-106, 151.
    [27]
    刘宝山, 程招勋, 张春鹏. 构造演化对嫩江多宝山矿集区的叠加与改造作用初探[J]. 矿产与地质, 2019, 33(1): 54-62.

    Liu B S, Cheng Z X, Zhang C P. Preliminary discussion on the effect of tectonic evolution on the superposition and transformation of the ore concentration area in Duobaoshan, Nenjiang[J]. Mineral Resources and Geology, 2019, 33(1): 54-62.
    [28]
    刘永江, 冯志强, 蒋立伟, 等. 中国东北地区蛇绿岩[J]. 岩石学报, 2019, 35(10): 3017-3047.

    Liu Y J, Feng Z Q, Jiang L W, et al. Ophiolite in the eastern Central Asian Orogenic Belt, NE China[J]. Acta Petrologica Sinica, 2019, 35(10): 3017-3047.
    [29]
    Pearce J A, Harris N B W, Andrew G T. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4): 959-983.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 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
    Get Citation
    PDF
    XML

    Article Metrics

    Article views (66) PDF downloads(0) Cited by()
    Proportional views
    Related

    Copyright © 2009《 石油钻探技术 》 All Rights Reserved.

    Address：North-Star Times Tower, No.8 Beichendong Road, Chaoyang District, Beijing, China China Pos：102206

    Tel：010-61771525, 61771524, 59462775, 59462779 Fax：021-64253812 Email：syzt@vip.163.com

    Beijing public network security equipment 11010502036328　Beijing ICP backup 17033152

    Supported by: Beijing Renhe Information Technology Co., Ltd.  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return