Chengdu Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2023 Vol. 43, No. 1
Article Contents
Article navigation > Sedimentary Geology and Tethyan Geology > 2023 > 43(1): 145-155
Next Article Previous Article

GAO Ke, SONG Yang, LIU Zhibo, YANG Huanhuan, WANG Yiyun. 2023. Sulfur and lead isotope composition and tracing for sources of ore-forming materials in the Naruo Cu(Au) deposit, in Tibet. Sedimentary Geology and Tethyan Geology, 43(1): 145-155. doi: 10.19826/j.cnki.1009-3850.2021.05002
Citation: GAO Ke, SONG Yang, LIU Zhibo, YANG Huanhuan, WANG Yiyun. 2023. Sulfur and lead isotope composition and tracing for sources of ore-forming materials in the Naruo Cu(Au) deposit, in Tibet. Sedimentary Geology and Tethyan Geology, 43(1): 145-155. doi: 10.19826/j.cnki.1009-3850.2021.05002
shu

Sulfur and lead isotope composition and tracing for sources of ore-forming materials in the Naruo Cu(Au) deposit, in Tibet

  • 1. Chengdu Center, China Geological Survey, Chengdu 610081, China;

  • 2. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date:  21 October 2020
Revised Date:  14 April 2021
    Abstract
  • On the basis of detailed field geological survey and mineralogical research, in order to discuss the source of ore-forming materials from the Naruo copper (gold) deposit in the Duolong ore-concentrated area and study the metallogenic mechanism, we analyzed the sulfur and lead isotope from the orebody, discussed the significance. The results show that the δ34S values of the seventeen metal sulfides vary from -2.3‰ to 2.3‰, with an average of 0.13‰. The δ34S values of thirteen pieces of pyrite vary from -2.3‰ to 2.3‰, with an average of 0.17‰. δ34S values of four pieces of chalcopyrite vary from -1.5‰ to 0.8‰, with an average of -1.1‰. The δ34S histogram is distributed approximately in a tower shape, with an average nearly zero, which indicates a mantle source. 208Pb/204Pb, 207Pb/204Pb, 206Pb/204Pb isotopic composition of metal sulfides respectively are 38.209~38.854, 15.541~15.665 and 17.942~18.58, with average of 38.635, 15.605 and 18.641. These data show the normal lead characteristics. Lead isotope μ values range from 9.40 to 9.57, less than 9.58. The feature shows that lead mainly comes from mantle material. Sulfur and lead isotopic characteristics of theNaruo deposit are identical with those of other porphyry deposits in the Duolong ore-concentrated area. The ore-forming materials of theNaruo deposit was mainly derived from mantle materials in an island arc environment, and there may be a mix of shell-derived materials.
    • FullText(HTML)
  • 加载中
    • References
  • Chaussidon M，Albarede F，Sheppard S M F，1989. Sulphur isotope variations in the mantle from ion microprobe analyses of micro-sulphide inclusions[J]. Earth and Planetary Science Letters，92（2）：144-156.

    Google Scholar

    Chinnasamy SS，Mishra B，2013. Greenstone metamorphism，hydrothermal alteration，and gold mineralization in the genetic context of the granodiorite-hosted gold deposit at Jonnagiri，Eastern Dharwar Craton，India[J]. Economic Geology，108（5）：1015-1036.

    Google Scholar

    Doe B R，Zartman R E，1979. Plumbotectoics，the Phanerozoic，In Barnes，H. L. ，ed. ，Geochemistryof hydrothermal ore deposits-second edition[C]. New York，John Wiley，22-70.

    Google Scholar

    Donoghue KA，Ripley EM，Li CS，2014. Sulfur isotope and mineralogical studies of Ni-Cu sulfide mineralization in the bovine igneous complex intrusion，Baraga，Northern Michigan[J]. Economic Geology，109（2）：325-341.

    Google Scholar

    Lin B，Tang J X，Chen Y C，et al. ，2017. Geochronology and genesis of the tiegelongnan porphyry cu（au） deposit in tibet：evidence from U–Pb，Re–Os dating and Hf，S，and H–O isotopes[J]. Resource Geology，67（1）：1-21.

    Google Scholar

    Ohmoto H，Rye R O，1979. Isotopes of sulfur and carbon [J]. Geochemistry of Hydrothermal Ore Deposits，509 - 567.

    Google Scholar

    Stacey J S，Hedlund D C，1983. Lead-isotopic compositions of diverse igneous rocks and ore deposits from southwestern New Mexico and their implications for early Proterozoic crustal evolution in the western United States[J]. Geological Society of America Bulletin，94（1）：1558-1567.

    Google Scholar

    Xu Z Q，Dilek K，Cao H，et al. ，2015. Paleo-Tethyan evolution of Tibet as recorded in the East Cimmerides and West Cathaysides[J]. Journal of Asian Earth Sciences，105：320–337.

    Google Scholar

    Zartman R E，Doe B R，1981. Plumbotetonics-the model （in evolution of the upper mantle）[J]. Tectonophysics，75：135-162.

    Google Scholar

    Zhang J，Chen Y J，Yang Y，et al. ，2011. Lead isotope systematics of the Weishancheng Au−Ag belt，Tongbai Mountains，central China：Implication for ore genesis[J] International Geology Review，53（5−6）：656−676.

    Google Scholar

    Zheng Y F，1991. Sulphur isotopic fractionation between sulphate and sulphide in hydrothermal ore deposits：disequilibrium vs equilibrium processes[J]. Terra Nova，3（5）：510-516.

    Google Scholar

    陈俊，王鹤年，2005. 地球化学[M]. 北京：科学出版社，129−135

    Google Scholar

    Chen J，Wang H N，2004. Geochemistry. Beijing：Science Press，129-135（in Chinese）.

    Google Scholar

    丁帅，2014. 西藏改则县拿若铜（金）矿地质特征研究[D]. 成都：成都理工大学.

    Google Scholar

    Ding S，2014. The Study of Geological characteristics of Naruo copper（gold）deposit in Gaize，Tibet[D]. Chengdu ：Chengdu University of Tecnology（in Chinese）.

    Google Scholar

    高轲，唐菊兴，宋扬，等，2016a. 西藏拿若铜（金）矿床隐爆角砾岩流体包裹体研究[J]. 地质与勘探，52（5）：815-825.

    Google Scholar

    Gao K，Tang J X，Song Y，et al.，2016a. Fluid inclusion study of the cryptoexplosive breccias of the Naruo deposit in Tibet[J]. Geology and Exploration，52，815-825(in Chinese with English abstract).

    Google Scholar

    高轲，多吉，唐菊兴，等，2016b. 西藏多龙矿集区拿若铜（金）矿床蚀变特征[J]. 矿物岩石地球化学通报，35（6）：1226-1237.

    Google Scholar

    Gao K，Duo J，Tang J X，et al.，2016b. Alteration of Naruo Porphyry Cu （Au）Deposit in the Duolong Ore-concentration Area，Tibet[J]. Bulletion of Mineralogy，Petrology and Geochemist，35（6）：1206-1217(in Chinese with English abstract).

    Google Scholar

    郭硕，2013. 西藏改则县多龙矿集区矿床模型与应用[D]. 北京：中国地质大学（北京）.

    Google Scholar

    Guo S， 2013. Mineral deposit model of the Duolong deposit cluster in Gaize County，Tibet and its application[D]. Beijing: China University of Geosciences（Beijing）(in Chinese).

    Google Scholar

    何阳阳，温春齐，刘显凡，等，2013. 多不杂铜矿区铅同位素地球化学特征[J]. 金属矿山，440（2）：101-104

    Google Scholar

    He Y Y，Wen C Q，Liu X F，et al. ，2013. Geochemical Characteristics of Pb Isotopes in Duobuza Copper Deposit[J]. Metal Mine，440（2）：101-104.

    Google Scholar

    李丹，2012. 西藏波龙铜矿床流体包裹体研究[D]. 成都：成都理工大学.

    Google Scholar

    Li D，2012. Study on the Fluid Inclusions of the Bolong Copper Deposit，Tibet[D]. Chengdu：Chengdu University of Technology（in Chinese）.

    Google Scholar

    李金祥，2008. 班公湖带多不杂超大型富金斑岩铜矿床的成岩成矿年代学、岩石学及高氧化岩浆−流体−成矿作用[D]. 北京：中国科学院地质与地球物理研究所.

    Google Scholar

    Li J X，2008. Geochronology，petrology and metallogeneses of high oxidized magma-hydrothermal fluid of Duobuza gold-rich porphyry copper deposit in Bangonghu belt，Northern Tibet[D]. Institute of Geology and Geophysics，Graduate University of Chinese Academy of Sciences（in Chinese）.

    Google Scholar

    李胜荣，肖润，周肃，等，2005. 西藏改则地区金成矿作用[J]. 矿床地质，24（1）：1-14

    Google Scholar

    Li R S，Xiao R，Zhou S，et al. ，2005. Gold mineralization in Gaize area，Tibet[J]. MINERAL DEPOSITS，24（1）：1-14.

    Google Scholar

    李玉彬，钟婉婷，郭建慈，等，2019. 西藏班公湖-怒江成矿带西段拿厅斑岩Cu（Au）矿床的火成岩岩石成因与成矿物质来源[J]. 岩石学报，35（6）：1717-1737

    Google Scholar

    Li Y B，Zhong W T，Guo J C，et al. ，2019. Petrogenesis of igneous rocks and ore-forming material source of the Nating porphyry Cu （Au） deposit in the western section of the Bangong Co-Nujiang metallogenic belt，Tibet[J]. Acta Petrologica Sinica，35（6）：1717-1737.

    Google Scholar

    吕丽娜，2012. 西藏班公湖−怒江成矿带西段富铁与铜（金）矿床模型[D]. 北京：中国地质科学院.

    Google Scholar

    Lü L N，2012. Metallogenic model of rich iron and copper（gold） deposits in Western Part of Bangong Co-Nujiang metallogenic belt，Tibet[D]. Beijing：Chinese Academy of Geological Sciences（in Chinese）.

    Google Scholar

    潘桂棠，王立全，耿全如，等，2020. 班公湖-双湖-怒江-昌宁-孟连对接带时空结构——特提斯大洋地质及演化问题[J]. 沉积与特提斯地质，40（3）：1-19

    Google Scholar

    Pan G T，Wang L Q，Geng Q R，et al. ，2020. Space-time structure of the Bangonghu-Shuanghu-Nujiang-Changning-Menglian Mega-suture zone：A discussion on geology and evolution of the Tethys Ocean[J]. Sedimentary Geology and Tethyan Geology，40（3）：1-19.

    Google Scholar

    佘宏全，李进文，马东方，等，2009. 西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP 测年及地质意义[J]. 矿床地质，28（6）：737-746

    Google Scholar

    She H Q，Li J W，Ma D F，et al. ，2009. Molybdenite Re-Os and SHRIMP zircon U-Pb dating of Duobuza porphyry copper deposit in Tibet and its geological implications[J]. MINERAL DEPOSITS，28（6）：737-746.

    Google Scholar

    沈渭洲，黄耀生，1987. 稳定同位素地质[M]. 北京：原子能出版社，1−495.

    Google Scholar

    Shen W Z，Huang Y S，1987. Stable isotope geology[M]. Beijing：Atomic Energy Press，1-1495（in Chinese）.

    Google Scholar

    孙振明，2015. 西藏班—怒成矿带西段多龙矿集区铜金成矿作用与成矿规律[D]. 吉林：吉林大学.

    Google Scholar

    Sun Z M，2015. Copper-Gold Mineralization and Metallogenic Regularity of Duolong Mineralization Area in Western Bangongco-Nujiang[D]. Jilin：Jilin University（in Chinese）.

    Google Scholar

    王松，赵元艺，汪傲，等，2017. 西藏拿顿铜（金）矿床岩矿相学、流体包裹体和地球化学特征与成矿作用研究[J]. 地质学报，91（7）：1565-1588

    Google Scholar

    Wang S，Zhao Y Y，Wang A，et al. ，2017. The Study of Facieology-Mineragraphy，Fluid Inclusions，and Geochemical Characteristics and Mineralization in Nadun Cu （Au） Deposit，Tibet[J]. Acta Geologica Sinica，91（7）：1565-1588.

    Google Scholar

    王艺云，2018. 西藏铁格隆南超大型铜（金、银）矿床成因——矿物学、蚀变与成矿[D]. 成都：成都理工大学.

    Google Scholar

    Wang Y Y，2018. Genesis of Tiegelongnan super-large copper（gold and silver） deposit in Tibet，China——mineralogy，alteration and mineralization[D]. Chengdu：Chengdu University of Technology（in Chinese）.

    Google Scholar

    王艺云，唐菊兴，宋扬，等，2017. 西藏铁格隆南超大型Cu（Au、Ag）矿床S、Pb同位素地球化学研究[J]. 地球学报，38（5）：627-637

    Google Scholar

    Wang Y Y，Tang J X，Song Y，et al. ，2017. Geochemical Characteristics of Sulfur and Lead Isotopes from the Superlarge Tiegelongnan Copper （Gold-silver） Deposit，Tibet[J]. Acta Geoscientia Sinica，38（5）：627-637.

    Google Scholar

    肖剑波，2012. 班怒西段多不杂铜矿床成因浅析[D]. 成都：成都理工大学.

    Google Scholar

    Xiao J B，2012. Genesis of the Duobuza copper deposit in the western Bangong Co-Nujiang Metallogenic belt，Tibet[D]. Chengdu University of Technology（in Chinese）.

    Google Scholar

    辛洪波，曲晓明，王瑞江，等，2009. 藏西班公湖斑岩铜矿带成矿斑岩地球化学及Pb、Sr、Nd同位素特征[J]. 矿床地质，28（6）：785-792

    Google Scholar

    Xin H B，Qu X M，Wang R J，et al. ，2009. Geochemistry and Pb，Sr，Nd isotopic features of ore-bearing porphyries in Bangong Lake porphyry copper belt，western Tibet[J]. MINERAL DEPOSITS，28（6）：785-792.

    Google Scholar

    杨超，唐菊兴，王艺云，等，2014. 西藏铁格隆南浅成低温热液型-斑岩型Cu-Au矿床流体及地质特征研究[J]. 矿床地质，33（6）：1287-1305

    Google Scholar

    Yang C，Tang J X，Wang Y Y，et al. ，2014. Fluid and geological characteristics researches of Southern Tiegelong epithermal porphyry Cu-Au deposit in Tibet[J]. Mineral deposits，33：1287-1305.

    Google Scholar

    杨竞红，孙延绵，董毅，1992. 硫同位素组成特征、成因分类及在找矿评价中的应用——以中国北东部铜铅锌多金属矿床为例[J]. 有色金属矿产与勘查，1（2）：117-125

    Google Scholar

    Yang J H，Sun Y M，Dong Y，1992. Sulfur isotopic composition，genetic classification and its application in prospecting evaluation：A case study of the copper，lead and zinc polymetallic deposits in North eastern China[J]. Non-ferrous mineral resources and exploration，1（2）：117-125.

    Google Scholar

    张静，杨艳，胡海珠，等，2009. 河南银洞沟造山型银矿床碳硫铅同位素地球化学[J]. 岩石学报，25（11）：2833-2842.

    Google Scholar

    Zhang J，Yang Y，Hu H Z，et al.，2009. C-S-Pb isotope geochemistry of the Yindonggou orogenic type silver deposit in Henan province[J]. Acta Petrologica Sinica，25（11）：2833-2842(in Chinese with English abstract).

    Google Scholar

    张良，刘跃，李瑞红，等，2014. 胶东大尹格庄金矿床铅同位素地球化学[J]. 岩石学报，30（9）：2468-2480

    Google Scholar

    Zhang L，Liu Y，Li R H，et al. ，2014. Lead isotope geochemistry of Dayingezhuang gold deposit，Jiaodong Peninsula，China[J]. Acta Petrologica Sinica，30（9）：2468-2480.

    Google Scholar

    周玉，多吉，温春齐，等，2013. 西藏波龙铜矿床S，Pb同位素地球化学特征[J]. 矿物岩石，33（2）：43-49

    Google Scholar

    Zhou Y，Duo J，Wen C Q，et al. ，2013. Geochemical Characteristics of Sulfur and Lead Isotopes from the Bolong Copper Deposit，Tibet[J]. Journal of Mineralogy and Petrology，，33（2）：43-49.

    Google Scholar

    朱炳泉，1998. 地球科学中同位素体系理论与应用—兼论中国大陆壳幔演化[M]. 北京：科学出版社.

    Google Scholar

    Zhu B Q，1998. Theory and Application of isotope system in Earth Science，and on crust-mantle evolution in mainland China[M]. Beijing：Science Press（in Chinese）.

    Google Scholar

    祝向平，陈华安，刘鸿飞，等，2015. 西藏拿若斑岩铜金矿床成矿斑岩年代学、岩石化学特征及其成矿意义[J]. 地质学报，89（1）：109-128

    Google Scholar

    Zhu X P，Chen H A，Liu H F，et al. ，2015. Geochronology and geochemistry of porphyries from the Naruo porphyry copper deposit，Tibet and their metallogenic significance[J]. Acta Geologica Sinica，89：109-128.

    Google Scholar

    祝向平，陈华安，马东方，等，2011. 西藏波龙斑岩铜金矿床的Re-Os同位素年龄及其地质意义[J]. 岩石学报，27（7）：2159-2164

    Google Scholar

    Zhu X P，Chen H A，Ma D F，et al. ，2011. Re-Os dating for the molybdenite from Bolong porphyry copper-gold deposit in Tibet，China and its geological significance[J]. Acta Petrologica Sinica，27（7）：2159-2164.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
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
Export Citation
PDF
XML

Article Metrics

Article views(734) PDF downloads(239) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020