CSCD来源期刊

北大中文核心期刊

中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

世界期刊影响力指数报告Q1区（2023）

Volume 39 Issue 3
May  2020
Turn off MathJax
Article Contents
Article Navigation >  Bulletin of Geological Science and Technology  > 2020  >  39(3): 170-178
Zhang Haikun, Hu Peng, Cao Liang, Cheng Xiang, Zhan Mingguo, Pan Luozhong, Dai Yu, Pan Beihong. Characteristics of mineralization fluids and mineralization material sources of the Sedex-type Dairi Pb-Zn ore concentration area in Indonesia: Evidence from fluid inclusions and isotopic geochemistry[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 170-178. doi: 10.19509/j.cnki.dzkq.2020.0318
Citation: Zhang Haikun, Hu Peng, Cao Liang, Cheng Xiang, Zhan Mingguo, Pan Luozhong, Dai Yu, Pan Beihong. Characteristics of mineralization fluids and mineralization material sources of the Sedex-type Dairi Pb-Zn ore concentration area in Indonesia: Evidence from fluid inclusions and isotopic geochemistry[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 170-178. doi: 10.19509/j.cnki.dzkq.2020.0318
shu

Characteristics of mineralization fluids and mineralization material sources of the Sedex-type Dairi Pb-Zn ore concentration area in Indonesia: Evidence from fluid inclusions and isotopic geochemistry

doi: 10.19509/j.cnki.dzkq.2020.0318
  • Received Date: 27 Jan 2019
    Abstract
  • The Dairi Pb-Zn ore concentration area, hosted by shale and displaying Sedex-type Pb-Zn mineralization of giant scale, is located in northwestern Sumatra, Indonesia.Systematic analysis of fluid inclusions and H, O, S and Pb isotopes was performed to probe its genesis.The results show that (1) the homogenization temperatures range from 189 to 315℃, with a peak at 220-240℃, indicating medium temperature for mineralization; (2)values of δ18OV-SMOW vary from +5.9‰ to +19.5‰, with an average of +16.6‰, implying a magma water-dominated mineralization fluid with minor addition of shallow water; (3)pyrites have positive δ34SCDT values from +25.49‰ to +26.36‰; (4)lead isotopes possess high μ values of 9.92-10.17(averaging 10.04) and ω values of 38.06-40.51 (averaging 39.26).It is indicated that the ores from Dairi formed at medium temperatures, having a fluid source dominated by magma water with minor addition of shallow water, a sulfur source comparable to ocean water and a single lead source from the crust.

     

    • FullText(HTML)
  • loading
    • References(34)
  • [1]
    刘继顺.印尼Dairi巨型铅锌富矿发现与勘探历程[EB/OL].(2017-6-28)http://blog.sina.com.cn/s/blog_4931d5820102wxy6.html.
    [2]
    Hall R.Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific:Computer-based reconstructions, model and animations[J].Journal of Asian Earth Sciences, 2002, 20(4):353-431. doi: 10.1016/S1367-9120(01)00069-4
    [3]
    Metcalfe I.Tectonic framework and Phanerozoic evolution of Sundaland[J].Gondwana Research, 2011, 19(1):3-21. doi: 10.1016/j.gr.2010.02.016
    [4]
    Yin A.Cenozoic tectonic evolution of Asia:A preliminary synthesis[J].Tectonophysics, 2010, 488(1/4):293-325. http://www.sciencedirect.com/science/article/pii/S0040195109003217
    [5]
    Whittaker J M, Müller R D, Sdrolias M, et al.Sunda-Java trench kinematics, slab window formation and overriding plate deformation since the Cretaceous[J].Earth and Planetary Science Letters, 2007, 255(3/4):445-457. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=2b527c9c39ca40ffad7ab8655c86aa44
    [6]
    Barber A J.The origin of the Woyla Terranes in Sumatra and the Late Mesozoic evolution of the Sundaland margin[J].Asian Earth Sciences, 2000, 18(6):713-738. doi: 10.1016/S1367-9120(00)00024-9
    [7]
    Baber A J, Crow M J.Structure of Sumatra and its implications for the tectonic assembly of Southeast Asia and the destruction of Paleotethys[J].Island Arc, 2009, 18(1):3-20. doi: 10.1111/j.1440-1738.2008.00631.x
    [8]
    Metcalfe I.Gondwana dispersion and Asian accretion:Tectonic and palaeogeographic evolution of eastern Tethys[J].Journal of Asian Earth Sciences, 2013, 66:1-33. doi: 10.1016/j.jseaes.2012.12.020
    [9]
    Ueno K.The Permian fusulinoidean faunas of the Sibumasu and Baoshan blocks:Their implications for the paleogeographic and paleoclimatologic reconstruction of the Cimmerian Continent[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 193(1):1-24. doi: 10.1016/S0031-0182(02)00708-3
    [10]
    Hutchison C S.Gondwana and Cathaysian blocks, Palaeotethys suture and Cenozoic tectonics in South-East Asia[J].Geoloische Rundshau, 1994, 82:388-405. doi: 10.1007/BF00210553
    [11]
    McCarroll R J, Graham I T, Fountain R, et al.The Ojolali region, Sumatra, Indonesia:Epithermal gold-silver mineralisation within the Sunda Arc[J].Gondwana Research, 2014, 26(1):218-240. doi: 10.1016/j.gr.2013.08.013
    [12]
    Hall R.Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean[J].Tectonophysics, 2012, 570/571:1-41. doi: 10.1016/j.tecto.2012.04.021
    [13]
    Fernández-Blanco D, Philippon M, von Hagke C.Structure and kinematics of the Sumatran Fault System in North Sumatra (Indonesia)[J].Tectonophysics, 2016, 693:453-464. doi: 10.1016/j.tecto.2016.04.050
    [14]
    Clayton R N, Rex R W, Syers J K, et al.Oxygen isotope abundance in quartz from Pacific pelagic sediments.Journal of Geophysical Research, 1972, 77(21):3907-3915. doi: 10.1029/JC077i021p03907
    [15]
    张理刚.稳定同位素在地质科学中的应用[M].西安:陕西科学技术出版社, 1985.
    [16]
    Samson I M, Russell M J.Genesis of the Silvermines zinc-lead-barite deposit, Ireland:Fluid inclusion and stable isotope evidence[J].Economic Geology, 1987, 82:371-394. doi: 10.2113/gsecongeo.82.2.371
    [17]
    Greig J A, Baadsgaard H, Cumming G L, et al.Fluid inclusion data from carbonate hosted Irish base metal deposits (abstract)[M].Manchester:Mineral Deposits Studies Group Mtg, 1983.
    [18]
    王莉娟, 祝新友, 王京斌, 等.青海锡铁山铅锌矿床喷流沉积系统(SEDEX)成矿流体研究[J].岩石学报, 2008, 24(10):2433-2440. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200810024
    [19]
    韩发, 孙海田.Sedex型矿床成矿系统[J].地学前缘, 1999, 6(1):139-162. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy199901012
    [20]
    卢焕章, 范宏瑞, 倪培, 等.流体包裹体[M].北京:科学出版社, 2004.
    [21]
    张德会.矿物流体包裹体液相成分特征及其矿床成因意义[J].地球科学:中国地质大学学报, 1992, 17(6):677-688.
    [22]
    于皓丞, 邱昆峰, 孙志佳, 等.新疆阿合奇地区色帕巴衣铅矿床成因:地质、地球化学研究的启示[J].地质科技情报, 2017, 36(2):20-28. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201702003
    [23]
    杨钻云, 邱仁轩, 秦术凯, 等.川西龙门山地区元古代VMS铜矿床:硫化物微量元素和硫同位素证据[J].地质科技情报, 2009, 28(4):59-64. http://d.wanfangdata.com.cn/Periodical/dzkjqb200904010
    [24]
    郎兴海, 邓煜霖, 王旭辉, 等.西藏雄村矿区Ⅲ号矿体硫、铅同位素特征及成矿物质来源[J].地质科技情报, 2018, 37(4):1-9. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201804001
    [25]
    徐书奎.豫西寺家沟金矿床氢氧硫同位素特征及地质意义[J].地质科技情报, 2017, 36(5):143-147. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201705019
    [26]
    李振红, 赵亚辉, 周厚祥.硫同位素地质特征及其在湖南省铜矿床成矿物质来源示踪中的应用[J].华南地质与矿产, 2018, 34(1):72-77. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hndzykc201801008
    [27]
    Ohmoto H, Rye R D.Isotopes of sulfur and carbon[C]//Barnes H L.Geochemistry of hydrothermal ore deposits.New York: Wiley, 1979.
    [28]
    朱炳泉.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, 1998.
    [29]
    Chang X Y, Zhu B Q, Yu S Y, et al.Application of lead isotopes to geochemical exploration of gold deposits in Baoban, Hainan Province, China[J].Chinese Journal of Geochemistry, 2003, 22(3):244-252. doi: 10.1007/BF02842868
    [30]
    李红梅.河南桐柏围山城金银成矿带成矿物质来源:铅同位素证据[J].地质与勘探, 2009, 45(4):374-384. http://www.cnki.com.cn/Article/CJFDTotal-DZKT200904006.htm
    [31]
    马圣钞.青海虎头崖铜铅锌多金属矿床硫、铅同位素组成及成因意义[J].地质与勘探, 2012, 48(2):321-331. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt201202014
    [32]
    谭洪旗.四川乌依铅矿床成矿物质来源:硫、铅同位素和方铅矿稀土元素地球化学制约[J].地质与勘探, 2017, 53(6):1051-1060. http://www.cqvip.com/QK/93079X/20176/673781510.html
    [33]
    Zartman R E, Doe B R.Plumbotectonics-the model[J].Tectonophysic, 1981, 75(12):135-162. http://www.sciencedirect.com/science/article/pii/0040195181902134
    [34]
    吴开兴, 胡瑞忠, 毕献武, 等.矿石铅同位素示踪成矿物质来源综述[J].地质地球化学, 2002, 30(2):73-81. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzdqhx200203013
    • 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(587) PDF Downloads(455) Cited by()
    Proportional views
    Related

    Copyright © 2010Editorial Department of Bulletin of Geological Science and Technology    

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

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return