Professional Committee of Rock and Mineral Testing Technology of the Geological Society of China, National Geological Experiment and Testing CenterHost
2022 Vol. 41, No. 2
Article Contents

LIU Wusheng, ZHAO Hong, ZHAO Ruyi, QIN Jinhua, ZHANG Xiong, JIANG Jinchang, ZHAO Chenhui, LI Tingjie, WANG Chenghui. The Constraints of Carbonaceous Mudstone Re-Os and Detrital Zircons U-Pb Isotopic Dating on the Diagenetic and Metallogenic Ages from the Dabaoshan Copper Deposit in Guangdong Province[J]. Rock and Mineral Analysis, 2022, 41(2): 300-313. doi: 10.15898/j.cnki.11-2131/td.202107270085
Citation: LIU Wusheng, ZHAO Hong, ZHAO Ruyi, QIN Jinhua, ZHANG Xiong, JIANG Jinchang, ZHAO Chenhui, LI Tingjie, WANG Chenghui. The Constraints of Carbonaceous Mudstone Re-Os and Detrital Zircons U-Pb Isotopic Dating on the Diagenetic and Metallogenic Ages from the Dabaoshan Copper Deposit in Guangdong Province[J]. Rock and Mineral Analysis, 2022, 41(2): 300-313. doi: 10.15898/j.cnki.11-2131/td.202107270085

The Constraints of Carbonaceous Mudstone Re-Os and Detrital Zircons U-Pb Isotopic Dating on the Diagenetic and Metallogenic Ages from the Dabaoshan Copper Deposit in Guangdong Province

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  • BACKGROUND

    With the development of high-precision negative thermal ionization mass spectrometry (N-TIMS) technology, Re-Os isotopic dating of carbonaceous mudstone is more and more widely used in the determination of sedimentary age. The controversy over the diagenetic and metallogenic ages of the Dabaoshan copper deposit in Guangdong Province has always been a key restricting the study of the genetic mechanism.

    OBJECTIVES

    To constrain the diagenetic and metallogenic ages of the Dabaoshan copper deposit.

    METHODS

    Re-Os isotope ratios were determined by high precision N-TIMS after dissolving carbonaceous mudstone powder by reverse aqua regia in the Carius tube. Zircon U-Pb age was determined by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS).

    RESULTS

    (1) The contents of Re and Os ranged from 0.976×10-9 to 2.997×10-9 and 0.067×10-9 to 0.115×10-9, respectively. The 187Re/188Os ratio varied from 78.236 to 154.799, and the 187Os/188Os ratio varied from 1.642 to 1.885. The Re-Os isotopic isochron age of black carbonaceous mudstone was 195±28Ma (n=6, MSWD=17). (2) The 206Pb/238U age ranged from 2631 to 236Ma, including two Mesozoic zircons, accounting for 2.50% of the total zircons, 19 Paleozoic zircons, accounting for 23.8% of the total zircons, 58 proterozoic zircons, accounting for 73% of the total zircons, 1 Archean zircon, accounting for 1% of the total zircons. The results of detrital zircon U-Pb age were broad and developed multiple peak periods, among which the youngest source magmatic zircon was formed in the Indosinian period.

    CONCLUSIONS

    The diagenetic and metallogenic age of the Dabaoshan copper deposit in Guangdong Province was constrained to the early Yanshanian. The distribution characteristics of detrital zircon U-Pb age further indicate that the Lower Jurassic Jinji Formation was formed at the stable continental margin, and its detrital material comes mainly from the ancient continental basement.

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  • [1] Ravizza G, Turekian K K. Application of the 187Re-187Os system to black shale geochronometry[J]. Geochimca et Cosmochimica Acta, 1989, 53(12): 3257-3262. doi: 10.1016/0016-7037(89)90105-1

    CrossRef Google Scholar

    [2] Shirey S B, Walker R J. The Re-Os isotope system in cosmochemistry and high-temperature geochemistry[J]. Annual Review of Earth and Planetary Sciences, 1989, 26: 423-500.

    Google Scholar

    [3] Selby D, Creaser R A. Direct radiometric dating of the Devonian-Mississippian time-scale boundary using the Re-Os black shale geochronometer[J]. Geology, 2005, 33: 545-548.

    Google Scholar

    [4] 李超, 屈文俊, 王登红, 等. Re-Os同位素在沉积地层精确定年及古环境反演中的应用进展[J]. 地球学报, 2014, 35(4): 405-414.

    Google Scholar

    Li C, Qu W J, Wang D H, et al. The progress of applying Re-Os isotope to dating of organic-rich sedimentary rocks and reconstruction of palaeoenvironment[J]. Acta Geoscientica Sinica, 2014, 35(4): 405-414.

    Google Scholar

    [5] 赵鸿, 李超, 江小均, 等. Re-Os同位素精确厘定长兴"金钉子"灰岩沉积年龄[J]. 科学通报, 2015, 60(23): 2209-2215.

    Google Scholar

    Zhao H, Li C, Jiang X J, et al. Direct radiometric dating of limestone from Changxing Permian—Triassic boundary using the Re-Os geochronometer[J]. China Science Bulluten, 2015, 60(23): 2209-2215.

    Google Scholar

    [6] 刘念, 姜宝玉, 周雪瑶, 等. 粤东盆地早侏罗世金鸡组物源分析及其对华南构造背景的约束[J]. 高校地质学报, 2018, 24(1): 65-76.

    Google Scholar

    Liu J, Jiang B Y, Zhou X Y, et al. Detrital provenance of the Lower Jurassic Jinji Formation and its constrains to the Early Jurassic geodynamic background of South China[J]. Geological Journal of China Universities, 2018, 24(1): 65-76.

    Google Scholar

    [7] 李小兵, 裴先治, 李佐臣, 等. 秦岭南缘勉略带构造属性及晚古生代地质背景: 来自碎屑锆石U-Pb年代学的制约[J]. 岩石学报, 2021, 37(5): 1444-1468.

    Google Scholar

    Li X B, Pei X Z, Li Z C, et al. Tectonic attributes and Late Paleozoic geological background of Mian-Lue belt in the southern margin of Qinling: Constraints from U-Pb geochronology of zircon[J]. Acta Petrologica Sinica, 2021, 37(5): 1444-1468.

    Google Scholar

    [8] 广东省地质矿产局705地质队. 大宝山多金属矿床地质勘探报告[R]. 北京: 地质出版社, 1961: 1-178.

    Google Scholar

    The No. 705 Geological Brigade from Geological Bureau of Guangdong Province. Summary report on geological exploration of the Dabaoshan polymetallic deposit[R]. Beijing: Geological Publishing House, 1961: 1-178.

    Google Scholar

    [9] 刘姤群, 杨世义, 张秀兰, 等. 粤北大宝山多金属矿床成因的初步探讨[J]. 地质学报, 1985, 59(1): 47-60.

    Google Scholar

    Liu G Q, Yang S Y, Zhang X L, et al. A preliminary study on the genesis of the Dabaoshan polymetallic deposit in northern Guangdong[J]. Acta Geologica Sinica, 1985, 59(1): 47-60.

    Google Scholar

    [10] 王磊, 胡明安, 屈文俊, 等. 粤北大宝山多金属矿床LA-ICP-MS锆石U-Pb和辉钼矿Re-Os定年及其地质意义[J]. 中国地质, 2012, 39(1): 29-42.

    Google Scholar

    Wang L, Hu M A, Qu W J, et al. Zircon LA-ICP-MS U-Pb and molybdenite Re-Os dating of the Dabaoshan polymetallic deposit in northern Guangdong Province and its geological implications[J]. Geology in China, 2012, 39(1) : 29-42.

    Google Scholar

    [11] 赵如意, 陈毓川, 王登红, 等. 粤北大宝山矿区次英安斑岩与铜多金属矿之间关系研究[J]. 大地构造与成矿学, 2019, 43(1): 123-140.

    Google Scholar

    Zhao R Y, Chen Y C, Wang D H, et al. Mineralization and the secondary porphyritic dacite in Dabaoshan orefield in the northern Guangdong Province[J]. Geotectonica et Metallogenia, 2019, 43(1): 123-140.

    Google Scholar

    [12] Su S Q, Qin K Z, Li G M, et al. Geochronology and geochemistry of Early Silurian felsic volcanic rocks in the Dabaoshan ore district, South China: Implications for the petrogenesis and geodynamic setting[J]. Geological Journal, 2017, 54: 3286-3303.

    Google Scholar

    [13] Qu H Y, Mao J W, Zhou S M, et al. Metallogenesis of stratiform Cu mineralization in the Dabaoshan polymetallic deposit, northern Guangdong Province, South China[J]. Journal of Geochemical Exploration, 2020, 210, 106448. doi: 10.1016/j.gexplo.2019.106448

    CrossRef Google Scholar

    [14] Wang L, Jin X B, Xu D M, et al. Geochronological, geochemical, and Nd-Hf isotopic constraints on the origin of magmatism in the Dabaoshan ore district of South China[J]. Geological Journal, 2019, 54: 1518-1534. doi: 10.1002/gj.3248

    CrossRef Google Scholar

    [15] 瞿泓滢, 陈懋弘, 杨富初, 等. 粤北大宝山铜多金属矿床中层状铜矿体的成矿时代及其成因意义[J]. 岩石学报, 2014, 30(1): 152-162.

    Google Scholar

    Qu H Y, Chen M H, Yang F C, et al. Metallogenic chronology of the stratform Cu orebody in the Dabaoshan Cu polymetallic deposit, northern Guangdong Province, and its geological significance[J]. Acta Petrologica Sinica, 2014, 30(1): 152-162.

    Google Scholar

    [16] 应立娟, 王登红, 李超, 等. 广东大宝山北部层状矿体硫化物Re-Os测年及指示[J]. 地学前缘, 2017, 24(5): 31-38.

    Google Scholar

    Ying L J, Wang D H, Li C, et al. Re-Os dating of sulfides in the north stratiform ore in Dabaoshan, Guangdong Province and its indication[J]. Earth Science Frontiers, 2017, 24(5): 31-38.

    Google Scholar

    [17] 赵晨辉. 广东大宝山铜多金属矿英安斑岩蚀变分带特征研究[D]. 北京: 中国地质科学院, 2021: 1-112.

    Google Scholar

    Zhao C H. Characteristics of alteration zones of dacite porphyry of the Dabaoshan copper polymetallic deposit in North Guangdong, South China[D]. Beijing: Chinese Academy of Geological Sciences, 2021: 1-112.

    Google Scholar

    [18] 赵如意, 王登红, 王要武, 等. 广东省大宝山斑岩型铜矿床勘查突破及其区域找矿意义[J]. 地质学报, 2020, 94(1): 204-216.

    Google Scholar

    Zhao R Y, Wang D H, Wang Y W, et al. The prospecting break-though and its regional propecting significance of the Dabaoshan porphyry copper deposit in Guangdong Province[J]. Acta Geologica Sinica, 2020, 94(1): 204-216.

    Google Scholar

    [19] 赵晨辉, 王成辉, 赵如意, 等. 广东大宝山铜矿英安斑岩的同位素组成与蚀变特征及其找矿意义[J]. 岩矿测试, 2020, 39(6): 908-920.

    Google Scholar

    Zhao C H, Wang C H, Zhao R Y, et al. Isotopic composition and alteration characteristics of dacite porphyry, and their prospecting significance in the Dabaoshan copper deposit of Guangdong Province[J]. Rock and Mineral Analysis, 2020, 39(6): 908-920.

    Google Scholar

    [20] 向建华, 梁新权, 单业华, 等. 广东大宝山多金属矿床两期成矿: 来自黑色炭质泥岩和辉钼矿Re-Os同位素定年的证据[J]. 大地构造与成矿学, 2018, 42(4): 732-745.

    Google Scholar

    Xiang J H, Liang X Q, Shan Y H, et al. Two phases of mineralization in the Dabaoshan polymetallic deposit, Guangdong Province: Constraints from Re-Os geochronology of black carbonaceous mudstone and molybdenite[J]. Geotectonica et Metallogenia, 2018, 42(4): 732-745.

    Google Scholar

    [21] 陈毓川, 王登红, 徐志刚, 等. 华南区域成矿和中生代岩浆成矿规律概要[J]. 大地构造与成矿学, 2014, 38(2): 219-229.

    Google Scholar

    Chen Y C, Wang D H, Xu Z G, et al. A summary of mineralization and Mesozoic magmatic mineralization laws in South China[J]. Geotectonica et Metallogenia, 2014, 38(2): 219-229.

    Google Scholar

    [22] 张国伟, 郭安林, 王岳军, 等. 中国华南大陆构造与问题[J]. 中国科学: 地球科学, 2013, 43(10): 1553-1582.

    Google Scholar

    Zhang G W, Guo A L, Wang Y J, et al. The structure and problems of the South China continent[J]. Science in China: Earth Science, 2013, 43(10): 1553-1582.

    Google Scholar

    [23] 王登红, 陈振宇, 黄凡, 等. 南岭岩浆岩成矿专属性及相关问题探讨[J]. 大地构造与成矿学, 2014, 38(2): 230-238.

    Google Scholar

    Wang D H, Chen Z Y, Huang F, et al. Discussion on the specificity of Nanling magmatic rock mineralization and related issues[J]. Geotectonica et Metallogenia, 2014, 38(2): 230-238.

    Google Scholar

    [24] Li C Y, Zhang H, Wang F Y, et al. The formation of the Dabaoshan porphyry molybdenum deposit induced by slab rollback[J]. Lithos, 2012, 150(4): 101-110.

    Google Scholar

    [25] Huang W T, Liang H Y, Wu J, et al. Formation of porphyry Mo deposit in a deep fault zone, example from the Dabaoshan porphyry Mo deposit in northern Guangdong, South China[J]. Ore Geology Reviews, 2017, 81: 940-952. doi: 10.1016/j.oregeorev.2016.07.013

    CrossRef Google Scholar

    [26] Mao W, Rusk B, Yang F, et al. Physical and chemical evolution of the Dabaoshan porphyry Mo deposit, South China: Insights from fluid inclusions, cathodoluminescence, and trace elements in quartz[J]. Economic Geology, 2017, 112(4): 889-918. doi: 10.2113/econgeo.112.4.889

    CrossRef Google Scholar

    [27] 李欣尉, 李超, 周利敏, 等. 贵州正安县奥陶系—志留系界线碳质泥岩Re-Os同位素精确厘定及其古环境反演[J]. 岩矿测试, 2020, 39(2): 251-261.

    Google Scholar

    Li X W, Li C, Zhou L M, et al. Accurate determination of the age of the carbonaceous mudstone of the Ordovician—Silurian Boundary in Zheng'an County, Guizhou Province by Re-Os isotope dating method and its application in paleoenvironmental inversion[J]. Rock and Mineral Analysis, 2020, 39(2): 251-261.

    Google Scholar

    [28] 彭晶晶, 罗代洪, 林锴, 等. 基于文献资源的Re-Os同位素定年数据库建设研究[J]. 岩矿测试, 2021, 40(3): 425-434.

    Google Scholar

    Peng J J, Luo D H, Lin K, et al. Study on the construction of journal publication-based Re-Os dating database[J]. Rock and Mineral Analysis, 2021, 40(3): 425-434.

    Google Scholar

    [29] 叶亚康, 周家云, 周雄. 川西塔公松林口岩体LA-ICP-MS锆石U-Pb年龄与地球化学特征[J]. 岩矿测试, 2020, 39(6): 921-933.

    Google Scholar

    Ye Y K, Zhou J Y, Zhou X. Zircon LA-ICP-MS U-Pb age and geochemical features of the Songlinkou Pluton, western Sichuan[J]. Rock and Mineral Analysis, 2020, 39(6): 921-933.

    Google Scholar

    [30] 胡志中, 王坤阳, 晏雄, 等. 锆石环氧树脂靶表面形貌特征及对LA-ICP-MS分析影响研究[J]. 岩矿测试, 2020, 39(6): 804-815.

    Google Scholar

    Hu Z Z, Wang K Y, Yan X, et al. Study on the morphology of zircon-bearing epoxy resin surface and its effect for LA-ICP-MS analysis[J]. Rock and Mineral Analysis, 2020, 39(6): 804-815.

    Google Scholar

    [31] 舒良树, 陈祥云, 楼法生. 华南前侏罗纪构造[J]. 地质学报, 2020, 94(2): 333-360. doi: 10.3969/j.issn.0001-5717.2020.02.001

    CrossRef Google Scholar

    Shu L S, Chen X Y, Lou F S. Pre-Jurassic tectonics of the South China[J]. Acta Geologica Sinica, 2020, 94(2): 333-360. doi: 10.3969/j.issn.0001-5717.2020.02.001

    CrossRef Google Scholar

    [32] Yao W H, Li Z X, Li W X, et al. Post-kinematic lithospheric delamination of the Wuyi—Yunkai Orogen in South China: Evidence from ca. 435Ma high-Mg basalts[J]. Lithos, 2012, 154: 115-129. doi: 10.1016/j.lithos.2012.06.033

    CrossRef Google Scholar

    [33] Zhang X S, Xu X S, Xia Y, et al. Early paleozoic intra-continental orogeny and post-orogenic extension in the South China Block: Insights from volcanic rocks[J]. Journal of Asian Earth Sciences, 2017, 141: 24-42. doi: 10.1016/j.jseaes.2016.07.016

    CrossRef Google Scholar

    [34] 贺振宇, 徐夕生, 王孝磊, 等. 赣南橄榄安粗质火山岩的年代学与地球化学[J]. 岩石学报, 2008, 24(11): 2524-2536.

    Google Scholar

    He Z Y, Xu X S, Wang X L, et al. Geochronology and geochemistry of shoshonitic colcanics in southern Jiangxi Province[J]. Acta Petrologica Sinica, 2008, 24(11): 2524-2536.

    Google Scholar

    [35] 项媛馨, 巫建华. 赣南龙南地区余田群玄武岩SHRIMP锆石U-Pb年龄及其地质意义[J]. 地质通报, 2012, 31(5): 716-725. doi: 10.3969/j.issn.1671-2552.2012.05.008

    CrossRef Google Scholar

    Xiang Y X, Wu J H. SHRIMP zircon U-Pb age of Yutian Group basalts in Longnan area of southern Jiangxi Province and its geological significance[J]. Geological Bulletin of China, 2012, 31(5): 716-725. doi: 10.3969/j.issn.1671-2552.2012.05.008

    CrossRef Google Scholar

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