Volume 22 Issue 2
Jun.  2016
Turn off MathJax
Article Contents
HUO Yan, LI Dan, 2016. STUDY ON THE FLUID INCLUSION PHYSICOCHEMICAL CONDITIONS OF BOLONG PORPHYRY COPPER-GOLD DEPOSIT IN TIBET. Journal of Geomechanics, 22 (2): 338-345.
Citation: HUO Yan, LI Dan, 2016. STUDY ON THE FLUID INCLUSION PHYSICOCHEMICAL CONDITIONS OF BOLONG PORPHYRY COPPER-GOLD DEPOSIT IN TIBET. Journal of Geomechanics, 22 (2): 338-345.

STUDY ON THE FLUID INCLUSION PHYSICOCHEMICAL CONDITIONS OF BOLONG PORPHYRY COPPER-GOLD DEPOSIT IN TIBET

More Information
  • Received: 2015-09-30
  • Published: 2016-06-01
  • Using Linkam THNSG600 dating and calculating by experience formulas, this paper discusses the fluid inclusion characteristics of Bolong porthyry copper-gold deposit in Tibet, which is beneficial to the migration of the main ore-forming element Cu, and the metallogenic process includes four periods: magma-advanced stage, magnetite-molybdenite period, chalcopyrite-pyrite period and anhydrite-pyrite period. It shows that the type of fluid inclusion is mainly the three-phases inclusion including NaCl and metal sulfide daughter minerals. The ore-forming fluid forms in high temperature (232~549 ℃) and low pressure (1.40×105~234.41×105 Pa), with high salinity (28.65~52.16wt% NaCl) and middle-high density (1.0683~1.1598 g/cm3). Along with the metallogenic process, the fluid fugacity and activity gradually reduce in each stages, while the values of pH and Eh increase. The element Cu mainly exits in the form of Cu(H2S)(HS)2-, which shows that Cu is easier to mineralization in high tempreture and acidic fluids.

     

  • loading
  • [1]
    曹圣华, 罗小川, 唐峰林, 等.班公湖—怒江结合带南侧弧-盆系时空结构与演化特征[J].中国地质, 2004, 31(1):51~56. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200401006.htm

    CAO Sheng-hua, LUO Xiao-chuan, TANG Feng-lin, et al. Time-space structure and evolution of the arc-basin system on the southern side of the Bangong Co-Nujiang junction zone [J]. Geology in China, 2004, 31(1):51~56. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200401006.htm
    [2]
    曲晓明, 辛洪波.藏西班公湖斑岩铜矿带的形成时代与成矿构造环境[J].地质通报, 2006, 25 (7):792~799. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200607005.htm

    Qu Xiao-ming, XIN Hong-bo. Ages and tectonic environment of the Bangong Co porphyry copper belt in western Tibet, China [J]. Geological Bulletin of China, 2006, 25 (7):792~799. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200607005.htm
    [3]
    李光明, 李金祥, 秦克章, 等.西藏班公湖带多不杂超大型富金斑岩铜矿的高温高盐高氧化成矿流体:流体包裹体证据[J].岩石学报, 2007, 23(5):935~952. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200705009.htm

    LI Guang-ming, LI Jin-xiang, QIN Ke-zhang, et al. High temperature, salinity and strong oxidation ore-forming fluid at Duobuza gold-rich porphyry copper deposit in the Bangonghu tectonic belt, Tibet: Evidence from fluid inclusions [J]. Acta Petrologica Sinica, 2007, 23(5):935~952. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200705009.htm
    [4]
    祝向平, 陈华安, 马东方, 等.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, 2011, 27(7):2159~2164. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201107024.htm

    ZHU Xiang-ping, CHEN Hua-an, MA Dong-fang, et al. Re-Os dating for the molybdenite from porphyry copper-gold deposit in Tibet, China and its geological significance [J]. Acta Petrologica Sinica, 2011, 27(7):2159~2164. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201107024.htm
    [5]
    祝向平, 陈华安, 马东方, 等.西藏波龙斑岩铜金矿床钾长石和绢云母40Ar/39Ar年龄及其地质意义[J].矿床地质, 2013, 32(5):954~962. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201305007.htm

    ZHU Xiang-ping, CHEN Hua-an, MA Dong-fang, et al. 40Ar/39Ar dating of hydrothermal K-feldspar and hydrothermal sericite from Bolong porphyry Cu-Au deposit in Tibet [J]. Mineral Deposits, 2013, 32(5):954~962. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201305007.htm
    [6]
    陈华安, 祝向平, 马东方, 等.西藏波龙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, 2013, 87(10):1593~1611. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201310009.htm

    CHEN Hua-an, ZHU Xiang-ping, MA Dong-fang, et al. Geochronology and geochemistry of the Bolong porphyry Cu-Au deposit, Tibet and tis mineralizing significance [J]. Acta Geologica Sinica, 2013, 87(10):1593~1611. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201310009.htm
    [7]
    周玉, 温春齐, 周雄, 等.西藏波龙铜矿区含矿斑岩主量元素特征及地质意义[J].矿物学报, 2011, 31(S1):444. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1225.htm

    ZHOU Yu, WEN Chun-qi, ZHOU Xiong, et al. The main elements characteristics and geological significance of ore-bearing porphyry in Bolong copper mining area, Tibet [J]. Acta Mineralogica Sinica, 2011, 31(S1):444. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1225.htm
    [8]
    周玉. 西藏波龙铜矿区含矿斑岩元素地球化学研究[D]. 成都: 成都理工大学, 2012.

    ZHOU Yu. Elements Geochemistry of Ore-bearing Porphyry in the Bolong Copper Mine District, Tibet [D]. Chengdu: Chengdu University Technology, 2012.
    [9]
    周玉, 多吉, 温春齐, 等.西藏波龙铜矿床S-Pb同位素地球化学特征[J].矿物岩石, 2013, 33(23):43~49. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS201302007.htm

    ZHOU Yu, DUO Ji, WEN Chun-qi, et al. Geochemical characteristics of Sulfur and Lead isotopes from the Bolong copper deposit, Tibet [J]. Journal of Mineralogy and Petrology, 2013, 33(23):43~49. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS201302007.htm
    [10]
    周玉, 多吉, 温春齐, 等.西藏波龙铜矿区变质岩特征及地质意义[J].矿物学报, 2013(S1):378~379. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2013S2213.htm

    ZHOU Yu, DUO Ji, WEN Chun-qi, et al. The metamorphic rocks' characteristics and geological significance of Bolong copper mining area, Tibet [J]. Acta Mineralogica Sinica, 2013(S1):378~379. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2013S2213.htm
    [11]
    倪曦, 刘志鹏, 杨蜜蜜.西藏波龙矿区含矿岩体地质特征[J].四川有色金属, 2016, 1:30~32. doi: 10.3969/j.issn.1006-4079.2016.01.008

    NI Xi, LIU Zhi-peng, YANG Mi-mi. Geological characteristics of ore-bearing rock mass in Bolong mining area, Tibet [J]. Sichuan Nonferrous Metals, 2016, 1:30~32. doi: 10.3969/j.issn.1006-4079.2016.01.008
    [12]
    李丹, 温春齐, 费光春, 等.西藏波龙铜矿床的砂岩成分与构造环境探讨[J].矿物学报, 2011, 31(S1):311~312. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1182.htm

    LI Dan, WEN Chun-qi, FEI Guang-chun, et al. The discussion of sandstone composition and tectonic environment in Bolong copper deposit, Tibet [J]. Acta Mineralogica Sinica, 2011, 31(S1):311~312. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1182.htm
    [13]
    周玉. 西藏波龙铜矿床成矿作用研究[D]. 成都: 成都理工大学, 2015.

    ZHOU Yu. Research on metallization of the Bolong copper deposit in Tibet, China [D]. Chengdu:Chengdu University of Technology, 2015.
    [14]
    李海宾. 西藏波龙铜(金)矿矿体地质要素特征研究[D]. 成都: 成都理工大学, 2015. http://epub.cqvip.com/articledetail.aspx?id=1000000246271

    LI Hai Bin. Study on the Characteristics of Geological Factors of Cooper and Gold Ore Deposit in Bolong, Tibet [D]. Chengdu:Chengdu University of Technology, 2015. http://epub.cqvip.com/articledetail.aspx?id=1000000246271
    [15]
    李丹. 西藏波龙铜矿床流体包裹体研究[D]. 成都: 成都理工大学, 2012.

    LI Dan. Study on the Fluid Inclusions of the Bolong Copper Deposit, Tibet [D]. Chengdu:Chengdu University of Technology, 2012.
    [16]
    周玉, 多吉, 温春齐, 等.西藏波龙铜矿区成矿流体来源示踪[J].中国矿业, 2015, 24(3):76~80. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGKA201503017.htm

    ZHOU Yu, DUO Ji, WEN Chun-qi, et al. The source of ore-forming fluids in the Bolong copper mine area, Tibet [J]. China Mining Magazine, 2015, 24(3):76~80. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGKA201503017.htm
    [17]
    邵洁涟.金矿找矿矿物学[M].北京:中国地质大学出版社. 1988.

    SHAO Jie-lian. Prospecting mineralogy of gold ore[M].Beijing:China University of Geosciences Press.1988.
    [18]
    Hall D L, Sterner S M, Bodnar R J. Freezing point depression of NaCl-KCl-H2O solutions[J]. Economic Geology, 1988, 83(1): 197~202. doi: 10.2113/gsecongeo.83.1.197
    [19]
    刘斌, 沈昆.流体包裹体热力学[M].北京:地质出版社, 1999.

    LIU Bin, SHEN Kun. Thermodynamics of fluid inclusions [M]. Beijing:Geological Publishing House, 1999.
    [20]
    徐文炘, 陈民扬, 喻铁阶, 等.矿物包裹体成分数据的热力学计算方法及应用[J].矿产与地质, 1985, 1:35~50. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD198501004.htm

    XU Wen-xi, CHEN Ming-yang, YU Tie-jie, et al. Thermodynamic calculation methods and applications of mineral inclusion composition data [J]. Mineral Resources and Geology, 1985, 1:35~50. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD198501004.htm
    [21]
    Crerar D A, Susak N J, Borcsik M, et al. Solubility of the buffer assemblage pyrite+pyrrhotite+magnetite in NaCl solutions from 200 to 350 degrees C [J]. Geochimica et Cosmochimica Acta, 1978, 42(9):1427~1438. doi: 10.1016/0016-7037(78)90048-0
    [22]
    李葆华, 蔡建明, 刘若兰.矿物包裹体学(下册)[M].成都:成都地质学院矿床教研室(内部教材), 1991.

    LI Bao-hua, CAI Jian-ming, LIU Ruo-lan. Mineral inclusion study(Part Ⅱ)[M]. Chengdu:Chengdu Institute of Geology and Mineral Deposits (internal teaching materials), 1991.
    [23]
    Helgeson H C. Thermodynamics of hydrothermal systems at elevated temperatures and pressures[J]. American Journal of Science, 1969, 267(7): 729~804. doi: 10.2475/ajs.267.7.729
    [24]
    Crerar D A, Barnes H L. Ore solution chemistry, V, Solubilities of chalcopyrite and chalcocite assemblages in hydrothermal solution at 200 degrees to 350 degrees C[J]. Economic Geology, 1976. 71(4): 772~794. doi: 10.2113/gsecongeo.71.4.772
    [25]
    金章东, 李福春.斑岩型铜矿床成矿过程中铜的迁移与沉淀机制研究新进展[J].矿产与地质, 1998, 12(2):73~78. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD802.000.htm

    JIN Zhang-dong, LI Fu-chun. New progress of copper mingation and precipitation mechanism during porphyry ore-forming process[J].Mineral Resources and Geology, 1998, 12(2):73~78. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD802.000.htm
    [26]
    李福春, 刘源, 金章东, 等.流体在金属成矿过程中的作用[J].矿产与地质, 1999, 13(3):129~134. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD903.000.htm

    LI Fu-chun, LIU Yuan, JIN Zhang-dong, et al. Role of fluid in the metal forming process of ore deposit [J]. Mineral Resources and Geology, 1999, 13(3):129~134. http://www.cnki.com.cn/Article/CJFDTOTAL-KCYD903.000.htm
  • 加载中

Catalog

    Figures(1)  / Tables(5)

    Article Metrics

    Article views (134) PDF downloads(9) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return