吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (1): 70-86.doi: 10.13278/j.cnki.jjuese.20160258

• 地质与资源 • 上一篇    下一篇

西藏班公湖—怒江成矿带南侧矽卡岩型铜多金属矿床S、Pb同位素组成及成矿物质来源

伍登浩1,2, 高顺宝1, 郑有业1,3, 田坎3, 张永超1, 姜军胜3, 余泽章3, 黄鹏程3   

  1. 1. 中国地质大学地质调查研究院, 武汉 430074;
    2. 贵州能矿地热投资股份有限公司, 贵阳 550007;
    3. 中国地质大学资源学院, 武汉 430074
  • 收稿日期:2017-05-24 出版日期:2018-01-26 发布日期:2018-01-26
  • 通讯作者: 高顺宝(1980-),男,助理研究员,主要从事青藏高原区域成矿作用及找矿评价方面的研究,E-mail:gaoshunbao2002@163.com E-mail:gaoshunbao2002@163.com
  • 作者简介:伍登浩(1990-),男,硕士,主要从事成矿规律与成矿预测方面的研究,E-mail:wudenghao@126.com
  • 基金资助:
    国家重点研发计划项目（2016YFC0600300）；教育部长江学者和创新团队发展计划（IRT14R54）

Sulfur and Lead Isotopic Composition and Their Ore-Forming Material Source of Skarn Copper Polymetallic Deposits in Southern Tibet Bangonghu-Nujiang Metallogenic Belt

Wu Denghao1,2, Gao Shunbao1, Zheng Youye1,3, Tian Kan3, Zhang Yongchao1, Jiang Junsheng3, Yu Zezhang3, Huang Pengcheng3   

  1. 1. Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China;
    2. Guizhou Mineral Geothermal Investment Co., Ltd, Guiyang 550007, China;
    3. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
  • Received:2017-05-24 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Key R&D Plan(2016YFC0600300) and Programme for Changjiang Scholars and Innovative Research Team in University (IRT14R54)

PDF (PC)

261

摘要： 班公湖—怒江成矿带南侧分布着多个与班公湖—怒江洋南向俯冲、碰撞、后碰撞伸展各阶段有关的矽卡岩型铜多金属矿床，目前对单个矿床的研究较多，而对形成于不同环境下的矿床之间的对比研究较少。本文通过对该成矿带南侧典型矽卡岩型铜多金属矿床的S、Pb同位素特征进行较为系统的总结，并结合前人对辉钼矿Re同位素、成矿岩体地球化学特征、成岩成矿时代及区域构造演化等研究的成果，对不同构造背景下所形成的4个矿床的成矿物质来源进行对比研究。研究表明：舍索矿床的S同位素具有明显的双峰式分布，为壳幔混合来源，而区内典型矿床的S同位素显示从班公湖—怒江洋南向俯冲（舍索）→碰撞（嘎拉勒、尕尔穷）→后碰撞（班戈日阿）逐渐富集重硫的特征；Pb同位素显示舍索较其他矿床更富集放射成因Pb，舍索、班戈日阿矿床成矿物质主要来源于念青唐古拉群结晶基底，而同碰撞期形成的嘎拉勒、尕尔穷矿床则显示了明显的壳幔混合来源的特征，念青唐古拉群结晶基底对尕尔穷矿床的成矿物质有少量贡献。此外，斑岩-矽卡岩复合型矿床的成矿物质来源具有壳幔混源的特征，而单一的矽卡岩型矿床以上地壳来源为主。

关键词: S、Pb同位素, 成矿物质来源, 班公湖—怒江成矿带, 矽卡岩铜多金属矿床, 成矿环境

Abstract: Numerous skarn Cu polymetallic deposits are discovered in the southern Bangonghu-Nujiang suture zone (BNSZ), which are related to the Bangonghu-Nujiang Middle Tethys Ocean southward subduction, collision, and post-collision. There are a lot of researches on a single deposit, but not on the contrast between two deposits. The authors systematically summarized the characteristics of S and Pb isotope of these deposits in combination with the previous researches on the Re isotope, the geochemical characteristics of metallogenic rock body, rock-forming and ore-forming age, and regional tectonic evolution, and took the contrasts between deposits into the study on the ore-forming materials of these deposits formed under different tectonic backgrounds. The results show that the δ34S values of Shesuo deposit present a notable bimodel distribution,which can be explained by the mixing of stratum and mantle. In summary, the 34S values were gradually enriched from the oceanic crust subduction stage (Shesuo), through the plate collision stage (Galale and Gaerqiong), to the post-collisional stage (Bangeria). The composition of Pb isotope indicates that the Shesuo deposit is enriched in radiogenic lead than the other deposits, and the ore forming material of Shesuo and Bangeria deposits were mainly sourced from the Nyainqentanglha group crystalline basement,while Galale and Gaerqiong deposits were from a mixture of crust-mantle materials, and the basement has a small contribution to the Gaerqiong deposit. In addition, the ore forming material of porphyry-skarn deposits has the characteristics of the mixture of crust-mantle materials, while the material of a skarn deposit mainly came from the upper crust.

Key words: S and Pb isotope, ore-forming materials sources, Bangonghu-Nujiang metallogenic belt, skarn copper polymetallic deposits, metallogenic environment

中图分类号: 

  • P618.4
[1] 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. Li Guangming, Li Jinxiang,Qin Kezhang, 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.
[2] 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. Zhu Xiangping, Chen Huaan, Ma Dongfang, et al. Re-Os Dating for the Molybdenite from Bolong Porphyry Copper-Gold Deposit in Tibet, China and Its Geological Significance[J]. Acta Petrologica Sinica, 2011, 27(7):2159-2164.
[3] 吕立娜,赵元艺,宋亮,等.西藏班公湖-怒江成矿带西段富铁矿与铜(金)矿C、Si、O、S和Pb同位素特征及地质意义[J]. 地质学报,2011,85(8):1291-1304. Lǚ Lina, Zhao Yuanyi, Song Liang, et al. Characteristics of C, Si, O, S and Pb Isotopes of the Fe-Rich and Cu (Au)Deposits in the Western Bangong-Nujiang Metallogenic Belt, Tibet, and Their Geological Significance[J]. Acta Geologica Sinica, 2011,85(8):1291-1304.
[4] 邓世林.西藏革吉县尕尔穷铜金矿矿床地球化学特征[D].成都:成都理工大学,2011. Deng Shilin. Geochemistry Character of Gaerqiong Copper-Gold Deposit, Geji County, Tibet[D]. Chengdu: Chengdu University of Technology, 2011.
[5] 赵元艺, 宋亮, 樊兴涛, 等. 西藏申扎县舍索铜多金属矿床辉钼矿Re-Os年代学及地质意义[J]. 地质学报,2009,83(8): 1150-1158. Zhao Yuanyi, Song Liang, Fan Xingtao, et al. Re-Os Dating of Molybdenite from the Shesuo Copper Polymetallic Ore in Shenzha County, Tibet and Its Geological Significance[J]. Acta Geologica Sinica, 2009,83(8): 1150-1158.
[6] 赵元艺,崔玉斌,吕立娜,等. 西藏舍索矽卡岩型铜多金属矿床年代学与地球化学特征及意义[J]. 岩石学报,2011,27(7): 2132-2142. Zhao Yuanyi, Cui Yubin, Lü Lina, et al. Chronology, Geochemical Characteristics and the Significance of Shesuo Copper Polymetallic Deposit, Tibet[J]. Acta Petrologica Sinica, 2011,27(7):2132-2142.
[7] 黄瀚霄,李光明,刘波,等. 西藏仲巴县天宫尼勒矽卡岩型铜金矿床锆石U-Pb年代学和岩石地球化学特征:对成因及其成矿构造背景的指示[J]. 地球学报, 2012,33(4): 424-434. Huang Hanxiao, Li Guangming, Liu Bo,et al. Zircon U-Pb Geochronology and Geochemistry of the Tiangongnile Skarn-Type Cu-Au Deposit in Zhongba County, Tibet: Their Genetic and Tectonic Setting Significance[J]. Acta Geoscientica Sinica, 2012, 33(4): 424-434.
[8] 高顺宝, 郑有业, 王进寿, 等.西藏班戈地区侵入岩年代学和地球化学对班公湖怒江洋盆演化时限的制约[J]. 岩石学报,2011,27(7):1973-1982. Gao Shunbao, Zheng Youye, Wang Jinshou, et al. The Geochronology and Geochemistry of Intrusive Rocks in Bage Area: Constraints on the Evolution Time of the Bangong Lake-Nujiang Ocean Basin[J]. Acta Petrologica Sinica, 2011, 27(7):1973-1982.
[9] 高顺宝. 西藏冈底斯西段铜铁多金属成矿作用与找矿方向[D]. 武汉:中国地质大学,2015. Gao Shunbao. Copper-Iron Polymetal Metallogenesis and Exploration Direction in the Western of Gangdise Metallogenic Belt, Tibet[D]. Wuhan: China University of Geosciences, 2015.
[10] 曲晓明,范淑芳,马旭东,等. 西藏班公湖-怒江成矿带上的碰撞后铜矿床[J]. 矿床地质,2015,34(3): 431-448. Qu Xiaoming, Fan Shufang, Ma Xudong, et al. Post-Collisional Copper Ore Deposits Along Bangong Co-Nujiang Metallogenic Belt, Tibetan Plateau[J]. Mineral Deposits, 2015, 34(3): 431-448.
[11] 李金祥, 李光明, 秦克章, 等.班公湖带多不杂富金斑岩铜矿床斑岩-火山岩的地球化学特征与时代:对成矿构造背景的制约[J].岩石学报,2008,24(3):531-543. Li Jinxiang, Li Guangming, Qin Kezhang, et al. Geochemistry of Porphyries and Volcanic Rocks and Ore-Forming Geochronology of Duobuza Gold-Rich Porphyry Copper Deposit in Bangonghu Belt, Tibet: Constraints on Metallogenic Tectonic Settings[J]. Acta Petrologica Sinica, 2008, 24(3): 531-543.
[12] 黄瀚霄,李光明,陈华安,等. 西藏色布塔铜钼矿床中辉钼矿Re-Os定年及其成矿意义[J]. 地质学报,2013,87(2): 240-244. Huang Hanxiao, Li Guangming, Chen Huaan,et al. Molybdenite Re-Os Isotope Age and Metallogenic Significance of Sebuta Copper Molybdenum Deposit in Tibet[J]. Acta Geologica Sinica, 2013, 87(2): 240-244.
[13] 李志军,唐菊兴,姚晓峰,等.班公湖-怒江成矿带西段尕尔穷铜金矿床辉钼矿Re-Os年龄及其地质意义[J]. 成都理工大学学报(自然科学版),2011, 38(6):678-683. Li Zhijun, Tang Juxing, Yao Xiaofeng, et al. Re-Os Isotope Age and Geological Significance of Molybdenite in the Gaerqiong Cu-Au Deposit of Geji, Tibet, China[J]. Journal of Chengdu University of Technology (Science of Technology Edition), 2011, 38(6):678-683.
[14] 姚晓峰, 唐菊兴, 李志军, 等.西藏尕尔穷铜金矿床S、Pb同位素地球化学特征:成矿物质来源示踪[J]. 地球学报, 2012,33(4): 528-536. Yao Xiaofeng, Tang Juxing, Li Zhijun, et al. S, Pb Isotope Characteristics of the Ga'erqiong Gold-Copper Deposit in Tibet: Tracing the Source of Ore-forming Materials[J]. Acta Geoscientica Sinica,2012,33(4): 528-536.
[15] 宋扬, 唐菊兴, 曲晓明, 等. 西藏班公湖怒江成矿带研究进展及一些新认识[J]. 地球科学进展, 2014,29(7): 795-809. Song Yang, Tang Juxing, Qu Xiaoming, et al. Progress in the Study of Mineralization in the Bangongcuo-Nujiang Metallogenic Belt and Some New Recognition[J]. Advances in Earth Science, 2014, 29(7): 795-809.
[16] Qu Xiaoming, Wang Ruijiang, Xin Hongbo, et al. Age and Petrogenesis of A-Type Granites in the Middle Segment of Bangonghu-Nujiang Suture, Tibetan Plateau[J]. Lithos, 2012,146/147(8):264-275
[17] 罗梅, 潘凤雏, 李巨初, 等. 西藏大冈底斯北部金属矿床成矿系列研究[J]. 地质学报, 2015,89(4): 715-730. Luo Mei, Pan Fengchu, Li Juchu, et al. Greatgangdise Northern Tibet Metallogenic Series Study of Ore Deposits[J]. Acta Geologica Sinica, 2015, 89(4): 715-730.
[18] Pan Guitang, Wang Liquan, Li Rongshe, et al. Tec-tonic Evolution of the Qinghai-Tibet Plateau[J]. Journal of Asian Earth Sciences, 2012, 53(2):3-14.
[19] Metcalfe I. Gondwana Dispersion and Asian Accre-tion: Tectonic and Palaeogeographic Evolution of Eastern Tethys[J]. Journal of Asian Earth Sciences, 2013, 66: 1-33.
[20] Zhang Kaijun, Zhang Yuxiu, Tang Xianchun, et al. Late Mesozoic Tectonic Evolution and Growth of the Tibetan Plateau Prior to the Indo-Asian Collision[J]. Earth Science Reviews, 2012,114(3/4):236-249.
[21] 康志强,许继峰,王保弟,等. 拉萨地块北部去申拉组火山岩:班公湖-怒江特提斯洋南向俯冲的产物?[J]. 岩石学报,2010,26(10):3106-3116. Kang Zhiqiang, Xu Jifeng, Wang Baodi, et al.Qushenla Formatlion Volcanic Rocks in North Lhasa Block: Products of Bangong Co-Nujiang Tethys Southward Subduction[J]. Acta Petrologica Sinica, 2010,26(10):3106-3116.
[22] 张亮亮, 朱弟成, 赵志丹,等. 西藏申扎早白垩世花岗岩类:板片断离的证据[J]. 岩石学报, 2011, 27(7): 1938-1948. Zhang Liangliang, Zhu Dicheng, Zhao Zhidan, et al. Early Cretaceous Granitoids in Xizang, Tibet: Evidence of Slab Break-Off[J]. Acta Petrologica Sinica, 2011, 27(7):1938-1948.
[23] 姚晓峰,唐菊兴,李志军,等.班公湖-怒江带西段尕尔穷矽卡岩型铜金矿含矿母岩成岩时代的重新厘定及其地质意义[J].地质论评,2013,59(1):193-200. Yao Xiaofeng, Tang Juxing, Li Zhijun, et al. The Redefinition of the Ore-forming Porphyry's Age in Gaerqiong Skarn-type Gold-Copper Deposit, Western Bangong Lake-Nujiang River Metallogenic Belt, Xizang(Tibet)[J]. Geological Review, 2013, 59(1):193-200.
[24] 张志, 陈毓川, 唐菊兴, 等.西藏尕尔穷-嘎拉勒铜金矿集区火山岩年代学及地球化学[J]. 地球科学:中国地质大学学报, 2015,40(1): 77-97. Zhang Zhi, Chen Yuchuan, Tang Juxing, et al. Zircon U-Pb Age and Geochemical Characteristics of Volcanic Rocks in Gaerqiong-Galale Cu-Au Ore District, Tibet[J]. Earth Science:Journal of China University of Geosciences, 2015, 40(1): 77-97.
[25] 白云,张志,陈毓川,等. 尕尔穷-嘎拉勒铜金矿集区S、Pb同位素地球化学特征[J]. 金属矿山, 2015,44(9): 100-104. Bai Yun, Zhang Zhi, Chen Yuchuan, et al. S, Pb Isotope Geochemical Characteristics of the Gaerqiong-Galale Gold-Copper Ore-Concentrated Area[J]. Metal Mine, 2015, 44(9): 100-104.
[26] Zhang Zhi, Yao Xiaofeng, Tang Juxing, et al. Litho-geochemical, Re-Os and U-Pb Geochronological, Hf-Lu and S-Pb Isotope Date of the Ga'erqiong-Galale Cu-Au Ore-Concentrated Area: Evidence for the Late Cretaceous Magmatism and Metallogenic Event in the Bangong-Nujiang Suture Zone, Northwestern Tibet, China[J]. Resource Geology, 2015, 65(2):76-102.
[27] 李运,赵元艺. 西藏北部舍索与拉屋铜矿床硫化物铅同位素特征[J]. 沉积与特提斯地质, 2014,34(3): 96-105. Li Yun, Zhao Yuanyi. Lead Isotopes in the Sulfide Ores from the Shesuo and Lawu Copper Deposits, Northern Xizang[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(3): 96-105.
[28] 陈国荣, 刘鸿飞, 蒋光武, 等.西藏班公湖-怒江结合带中段沙木罗组的发现[J]. 地质通报,2004,23(2):193-194. Chen Guorong, Liu Hongfei, Jiang Guangwu, et al. Discovery of the Shamuluo Formation in the Central Segment of the Bangong Co-Nujiang River Suture Zone, Tibet[J]. Geological Bulletin of China, 2004, 23(2):193-194.
[29] 曲晓明,辛洪波,杜德道,等.西藏班公湖怒江缝合带中段碰撞后A型花岗岩的时代及其对洋盆闭合时间的约束[J]. 地球化学,2012,41(1): 1-14. Qu Xiaoming, Xin Hongbo, Du Dedao, et al. Ages of Post-Collisional A-Type Granite and Constraints on the Closure of the Oceanic Basin in the Middle Segment of the Bangonghu-Nujiang Suture, the Tibetan Plateau[J]. Geochimica, 2012, 41(1): 1-14.
[30] Kapp P, DeCelles P G, Gehrels G E,et al. Geological Records of the Lhasa-Qiangtang and Indo-Asian Collisions in the Nima Area of Central Tibet[J]. Geological Society of America Bulletin, 2007, 119(7/8): 917-933.
[31] 董磊,李光明,黄瀚霄,等. 西藏班戈县拉青铜多金属矿床地球化学特征和年龄[J]. 地质通报, 2013,32(5): 767-773. Dong Lei, Li Guangming, Huang Hanxiao, et al. Geochemical Characteristics, Chronology and the Significance of Laqing Copper Polymetallic Skarn Deposit, Bange County, Tibet[J].Geological Bulletin of China, 2013,32(5):767-773.
[32] Liu Deliang, Huang Qishuai, Fan Shuaiquan, et al. Subduction of the Bangong-Nujiang Ocean: Constraints from Granites in the Bangong Co area, Tibet[J]. Geological Journal, 2014, 49(2):188-206.
[33] 范建军, 李才, 胡培远, 等.西藏改则地区仲岗洋岛的特征:兼论班公湖-怒江缝合带的闭合时限[M].广州:中山大学出版社,2013. Fan Jianjun, Li Cai, Hu Peiyuan, et al. The Characteristics of Zhonggang Ocean Island in Gaize Area, Tibet: Evidence on the Closure of the Bangong-Nujiang Suture Zone[M]. Guangzhou: University of Zhongshan Press, 2013.
[34] 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. Qu Xiaoming, Xin Hongbo. 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.
[35] Rollison H R.Using Geochemical Data: Evaluation, Presentation, Interpretation[M]. London:Pearson Education Limited, 1993.
[36] 赵一鸣,林文蔚,毕承恩.中国矽卡岩矿床[M]. 北京: 地质出版社,1990:123-126. Zhao Yiming, Lin Wenwei, Bi Cheng'en. Skarn Deposits of China[M]. Beijing: Geology Publishing House, 1990:123-126.
[37] Gariépy C, Allègre C J, Xu R H. The Pb-Isotope Geochemistry of Granitoids from the Himalaya-Tibet Collision Zone Implication for Crustal Evolution[J]. Earth and Planetary Science Letters, 1985, 74(2/3): 220-234.
[38] Zartman R E, Doe B R. Plumbotectonics:The Model[J]. Tectonophysics, 1981, 75(1/2): 135-162.
[39] 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. Zhu Bingquan. The Theory and Practice of Isotope System in Geoscience: Concurrent Discussion of the Continental Crust and Mantle Evolvements in China[M]. Beijing: Science Press, 1998.
[40] Doe B R, Zartman R E. Plumbotectonics: The Phanerozoic[C]//Barnes H L. Geochemistry of Hydrothermal Ore Deposits. New York: John Wiley and Sons, 1979: 22-70.
[41] Kamona A F, Lévêque J, Friedrich G,et al. Lead Isotopes of the Carbonate-Hosted Kabwe, Tsumeb, and Kipushi Pb-Zn-Cu Sulphide Deposits in Relation to Pan African Orogenesis in the Damaran-Lufilian Fold Belt of Central Africa[J]. Mineralium Deposita, 1999, 34(3): 273-283.
[42] 毛景文,张招崇.北祁连山小柳沟钨矿床中辉钼矿Re-Os年龄测定及其意义[J]. 地质论评,1999,45( 4):412-417. Mao Jingwen, Zhang Zhaochong. Re-Os Age Dating Moylbdenites in the Xiaoliugou Tungsten Deposit in the Northern Qilian Mountains and Its Significance[J]. Geological Review, 1999, 45(4):412-417.
[43] Mao Jingwen, Zhang Zhaochong, Zhang Zuoheng, et al. Re-Os Isotopic Dating of Molybdenites in the Xiaoliugou W(Mo)Deposit in the Northern Qilian Mountains and its Geological Significance[J]. Geochim Cosmochim Acta, 1999,63(11/12):1815-1818.
[44] 李厚民, 叶会寿, 王登红, 等.豫西熊耳山寨凹钼矿床辉钼矿铼-锇年龄及其地质意义[J].矿床地质,2009,28(2):133-142. Li Houmin, Ye Huishou, Wang Denghong, et al. Re-Os Dating of Molybdenites from Zhaiwa Mo Deposit in Xiong'er Mountain, Western Henan Province, and its Geological Significance[J]. Mineral Deposits, 2009,28(2):133-142.
[45] 高合明. 斑岩铜矿床研究综述[J]. 地球科学进展,1995,10(1):40-46. Gao Heming. A Summary of Researches on Porphyry Copper Deposits[J]. Advances in Earth Science, 1995, 10(1):40-46.
[1] 谷团. 牛角塘伴生型镉矿床特殊的成矿环境[J]. 吉林大学学报(地球科学版), 2017, 47(2): 464-476.
[2] 叶霖, 杨玉龙, 高伟, 刘铁庚. 陕南铜厂铜矿床成矿物质来源探讨[J]. J4, 2012, 42(1): 92-103.
[3] 赵宏光,孙景贵，陈军强，赵俊康，姚凤良，段 展. 延边小西南岔富金斑岩铜矿床的含矿流体起源与演化——H，O，C，S，Pb同位素示踪[J]. J4, 2005, 35(05): 601-606.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发