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REN Peng, LIANG Ting, LIU Kuo-long, NIU Liang, LU Lin, ZHANG Wen-jing. Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains[J]. Northwestern Geology, 2014, 47(1): 137-149.
Citation: REN Peng, LIANG Ting, LIU Kuo-long, NIU Liang, LU Lin, ZHANG Wen-jing. Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains[J]. Northwestern Geology, 2014, 47(1): 137-149.
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Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains

  • 1.

    Beijing SHRIMP Center of Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, China

  • 2.

    School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, China

  • 3.

    Institute of Areal Geology and Mineral Resources of Shaanxi Province, Xianyang 712000, China

Received Date:  05 January 2014
Revised Date:  23 February 2014
Publish Date:  15 March 2014
    Abstract
  • Fengtai mineral cluster region is located in the middle of Qinling Devonian lead and zinc polymetallic metallogenic belt. Lead-zinc deposits are mainly located in the siliceous rocks between Gudaoling group of the Upper Devonian and Xinghongpu group of the Middle Devonian. The analysis of S and Pb isotopic compositions of ore minerals in three typical ore deposits indicates that δ34S values of metal sulfide range no more than 10‰ in Qiandongshan, Bafangshan and Yinmusi lead-zinc deposits. The δ34S values of sulfides in the region range from 4.3‰ to 13.2‰, indicating that sulfur mainly came from seawater sulfate reduction. Among the lead isotope of three deposits, 206Pb/204Pb varies from 17.775 to 18.180, 207Pb/204Pb varies from 15.457 to 15.805, and 208Pb/204Pb varies from 37.977 to 38.670. Pb isotopic compositions have a large overlap, suggesting that the three lead-zinc deposits have similar sources of lead. The analysis of structure model diagram and Δβ-Δγ diagram of Pb isotope shows that lead came from the process that Yangtze plate subducted to North China plate in the middle of Early Paleozoic and Qinling microplate subducted to North China plate in the late Paleozoic.
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    • References
  • 祁思敬, 李英. 秦岭泥盆系铅锌成矿带[M]. 北京:地质出版社, 1993.

    Google Scholar

    Qi Sijing, Li Ying. Lead-Zinc Metallogenic Belt of Deronian System in Qinling Mountains[M]. Geological Publishing House, Beijing, 1993.

    Google Scholar

    王集磊, 何伯墀, 李健中, 等. 中国秦岭型铅锌矿床[M]. 北京:地质出版社, 1996.

    Google Scholar

    Wang Jilei, He Bochi, Li Jianzhong, et al. Qinling-Type Lead-Zinc Deposits in China[M]. Geological Publishing House, Beijing, 1996.

    Google Scholar

    吕仁生, 隗合明. 八方山层控多金属矿床地质特征及成因探讨[J]. 西安地质学院学报, 1990, 12(4):10-17.

    Google Scholar

    LV Rensheng, Wei Heming. The Geological Characteristics and Genetic Investigation of Bafangshan Stratabound Polymetallic Ores in Shaanxi Province[J]. Journal of Xi'an College of Geology, 1990, 12(4):10-17.

    Google Scholar

    王俊发, 张复新, 炎金才, 等. 秦岭泥盆系层控金属矿床[M]. 西安:陕西科学技术出版社, 1991.

    Google Scholar

    Wang Junfa, Zhang Fuxin, Yan Jincai, et al. Stratabound Ore Deposits of Deronian System in Qinling Mountains[M]. Shaanxi Science and Technology Publishing House, Xi'an, 1991.

    Google Scholar

    方维萱. 陕西凤县铅硐山大型铅锌矿床矿物地球化学研究[J]. 矿物学报, 1999, 19(2):198-205.

    Google Scholar

    Fang Weixuan. Research on Mineral Geochemistry of Qiandongshan Lead-Zinc Deposit, a Large-Sized Deposit in Fengxian County, Shaanxi[J]. Acta Mineralogica Sinica, 1999, 19(2):198-205.

    Google Scholar

    李徽. 凤县铅洞山铅锌矿床硫化矿物标型特征及其成因探讨[J]. 地质与勘探, 1986, 22(12):36-41.

    Google Scholar

    Li Hui. The Typomorphic Feature and Genesis of Sulfide in Qiandongshan Lead-Zinc Deposit of Fengxian County[J]. Geology and Prospecting, 1986, 22(12):36-41.

    Google Scholar

    杨兴科, 宫同伦. 铅硐山铅锌矿床动力热液成矿特征[J]. 西安地质学院学报, 1992, 14(1):35-41.

    Google Scholar

    Yang Xingke, Gong Tonglun. The Features of Dynamo-Hydrothermal Metallogenesis of the Qiandongshan Lead-Zinc Deposits[J]. Journal of Xi'an College of Geology, 1992, 14(1):35-41.

    Google Scholar

    祁思敬, 李英, 曾章仁, 等. 秦岭热水沉积型铅锌(铜)矿床[M]. 北京:地质出版社, 1993.

    Google Scholar

    Qi Sijing, Li Ying, Zeng Zhangren, et al. Lead-Zinc(copper) Deposits of Sedex Type in Qinling Mountains[M]. Geological Publishing House, Beijing, 1993.

    Google Scholar

    任鹏, 梁婷, 牛亮, 等. 陕西秦岭铅锌矿床的地质特征及成矿动力学过程[J]. 地球科学与环境学报, 2013, 35(1):34-47.

    Google Scholar

    Ren Peng, Liang Ting, Niu Liang, et al. Geological Characteristics and Geodynamic Process from Pb-Zn Deposits of Qinling Mountains, Shaanxi Province[J]. Journal of Earth Sciences and Environment, 2013, 35(1):34-47.

    Google Scholar

    张海, 何明友, 李方林, 等. 陕西凤县二里河喷流沉积型铅锌矿床的地质地球化学证据[J]. 地球科学与环境学报, 2011, 33(1):64-69. Zhang Hai, He Mingyou, Li Fanglin, et al. Geological and Geochemical Evidence of the Erlihe SEDEX Pb-Zn Deposit in Fengxian, Shaanxi[J]. Journal of Earth Sciences and Environment, 2011, 33(1):64-69. 罗静兰. 银母寺层控铅锌(铜)矿床的硫、铅同位素与矿床成因[J]. 西北地质, 1994, 15(1):19-24. Luo Jinglan. S、Pb Isotope and Genesis of Yinmusi Stratabound Pb-Zn Deposit[J]. Northwestern Geology, 1994, 15(1):19-24.

    Google Scholar

    周志贤, 王向阳, 师学安. 银母寺铅锌矿床成因研究[J]. 西安矿业学院学报, 1996, 16(4):334-338. Zhou Zhixian, Wang Xiangyang, Shi Xuean. Research on Genesis of Lead-Zinc Deposit in Yinmusi[J]. Journal of Xi'an Mining Institute, 1996, 16(4):334-338.

    Google Scholar

    隗合明. 秦岭凤太铅-锌矿田的海底喷气成矿类型及其空间分布规律[J]. 地质论评, 1990, 36(5):394-403. Wei Heming. The Submarine Exhalative Mineralization Types and Their Spatial Distribution in the Fengtai Pb-Zn Ore Field in the Qinling Mountains[J]. Geological Review, 1990, 36(5):394-403. 方维萱, 刘方杰, 胡瑞忠. 凤太泥盆纪拉分盆地中硅质铁白云岩-硅质岩特征及成岩成矿方式[J]. 岩石学报, 2000, 16(4):700-710.

    Google Scholar

    Fang Weixuan, Liu Fangjie, Hu Ruizhong. The Characteristics and Diagenetic-Metallogenic Pattern for Cherts and Siliceous Ferrodolomitites from Fengtai Apart-Pull Basin, Qinling Orogen[J]. Acta Petrologica Sinica, 2000, 16(4):700-710.

    Google Scholar

    贾润幸, 郭键, 赫英, 等. 秦岭凤太成矿区金多金属矿床成矿流体地球化学研究[J]. 中国地质, 2004, 31(2):192-198.

    Google Scholar

    Jia Runxing, Guo Jian, Hao Ying, et al. Ore Fluid Geochemistry of Gold Polymetallic Deposits in the Fengtai Ore District, Qinling Mountains[J]. Geology in China, 2004, 31(2):192-198.

    Google Scholar

    唐敏杰. 铅硐山铅锌矿床成矿模式及凤太矿田找矿潜力分析[J]. 有色金属(矿山部分), 2013, 65(6):23-28.

    Google Scholar

    Tang Minjie. Metallogenic Model of Qiandongshan Lead-Zinc Mine and Analysis on Prospecting Potential in Fengtai Ore Field[J]. Nonferrous Metals(Mining Section), 2013, 65(6):23-28.

    Google Scholar

    王瑞廷, 李芳林, 陈二虎, 等. 陕西凤县八方山-二里河大型铅锌矿床地球化学特征及找矿预测[J]. 岩石学报, 2011, 27(3):779-793.

    Google Scholar

    Wang Ruiting, Li Fanglin, Chen Erhu, et al. Geochemical Characteristics and Prospecting Prediction of the Bafangshan-Erlihe Large Lead-Zinc Ore Deposit, Feng County, Shaanxi Province, China[J]. Aata Petrologica Sinica, 2011, 27(3):779-793.

    Google Scholar

    邢宪龙, 胡仰军, 王嘉伟, 等. 凤太矿田尖端山铅锌矿床与八方山铜-铅锌矿床成矿特征对比研究[J]. 陕西地质, 2012, 30(2):19-26.

    Google Scholar

    Xing Xianlong, Hu Yangjun, Wang Jiawei, et al. Comparision of Mineralization Features between the Jianduanshan Lead-Zinc Deposit and Bafangshan Copper-Lead-Zinc Deposit in Fengxian-Taibai Area and the Ore-Prospecting Trend[J]. Geology of Shaanxi, 2012, 30(2):19-26.

    Google Scholar

    杨映堂. 秦岭银母寺铅锌矿床含矿地层沉积环境探讨[J]. 岩相古地理, 1996, 16(4):50-55.

    Google Scholar

    Yang Yingtang. Sedimentary Environments of the Ore-Bearing Strata within the Yingmusi Lead-Zinc Deposit in the Qinling Mountain Area[J]. Sedimentary Facies and Palaeogeography, 1996, 16(4):50-55.

    Google Scholar

    王向阳. 陕西凤县银母寺铅锌矿矿体定位预测研究[D]. 西安建筑科技大学, 2008 Wang Xiangyang. Prediction of Orebody in Yinmusi Lead Zinc Mine of Fengxian Shaanxi[D]. Xi'an University of Architecture and Technology, 2008.

    Google Scholar

    隗合明, 吕仁生. 凤太矿田层控铅锌(铜)矿床的成矿物质来源探讨[J]. 西安地质学院学报, 1990, 12(1):28-39.

    Google Scholar

    Wei Heming, LV Rensheng. An Exploratory Study of the Source of Mineralized Materials in the Stratabound Pb-Zn(Cu) Ore Deposits of the Fengtai Ore Field in the Qinling Mountains[J]. Journal of Xi'an College of Geology, 1990, 12(1):28-39.

    Google Scholar

    隗合明. 秦岭凤太矿田层控铅锌(铜)矿床的主要成矿特征及成矿模式[J]. 地质科学, 1992, (3):224-236.

    Google Scholar

    Wei Heming. Main Metallogenic Characteristics and Ore-Formation Model of Stratabound Lead-Zinc(copper) Ore Deposits of the Fengtai Ore Field, Qinling[J]. Scientia Geologica Sinica, 1992, (3):224-236.

    Google Scholar

    张国伟. 秦岭造山带的形成及其演化[M]. 西安:西北大学出版社, 1988. Google Scholar

    Sangster D.F. Sulphur and Lead Isotopes in Strata-Bound Deposits[A]. Wolf K.H. Handb遯汯顫 o陦氠屓tr穡孴呡伭終坯瑵卮孤 and 卓乴r祡孴兩牦祯rm Ore Deposits[C]. Amsterdam:Elsevier, 1976, 2:219-266.

    Google Scholar

    Orr W L. Rate and Mechanism of Non Microbial Su獬瑦幡te礠屒遥層幵陣襴歩乯襮睛降卝儮圠酇履睯幬扯睧橩彣呡扬眠顓浯硣穩ety o卦堠呁祭硥扲呩ca匬丠B乯噵坬赤奥孲, 1982.

    Google Scholar

    Ohmoto H. Systematics of Sulfur and Carbon Isotopes in Hydrothermal Ore Deposit[J]. Econ. Geol., 1972, 67:551-579.

    Google Scholar

    Hoefs J. Stable isotope geochemistry[M]. Springer-Verlag, Berlin Heidelberg, 1980.

    Google Scholar

    Pinckney D.m., Rafter T.A., Frac陴艩奯na啴汩o汮礠睯幦瘠坓赵呬坦瑵卲嬠牉彳otope丠噤杵色酩屮嵧丠恏兲卥圭资剥杰息屳it啩汯n氠祩睮帠扴睨佥甠硕穰獰牥乲輠屍issis即乩p坰赩儠牖祡lley Zinc-Lead District[J]. Econ. Geol., 1972, 67:315-328.

    Google Scholar

    Doe B.R., Zartman R.E. Plumb Tectonic, the Phanerozoic[A]. Barnes H.L. Geochemistry of Hydrothermal Ore Deposits[C]. Wileg-Interscience, NewYork, 1979:22-70.ress of Exhalative-Sedimentary Deposits[C]. Geological Publishing House, Beijing, 1994:42-50.

    Google Scholar

    于金杰, 杨海明, 叶会寿. 霍各乞铜多金属矿床的地质一地球化学特征及矿质来源[J]. 矿床地质, 1993, 12(1):67-76.

    Google Scholar

    Yu Jinjie, Yang Haiming, Ye Huishou. Geological and Geochemical Characteristics and Material Sources of the Huogeqi Copper-Polymetallic Deposit, Inner Mongolia[J]. Mineral Deposits, 1993, 12(1):67-76.

    Google Scholar

    付超, 王建平, 彭润民. 内蒙古甲生盘铅锌硫矿床硫同位素特征及其成因意义[J]. 现代地质, 2010, 24(1):34-41.

    Google Scholar

    Fu Chao, Wang Jianping, Peng Runmin. Features of Sulfur Isotope of the Jiashengpan Lead-Zinc-Sulfur Deposit in Inner Mongolia and Its Genesis Significance[J]. Geoscience, 2010, 24(1):34-41.

    Google Scholar

    B.A.格里年科. 硫同位素地球化学[M]. 赵瑞译. 北京:科学出版社, 1980.

    Google Scholar

    B.A.Grinenko. Sulfur Isotopic Geochemistry[M]. Translated by Zhao Rui. Science Press, Beijing, 1980.

    Google Scholar

    侯增谦. 现代与古代海底热水成矿作用[M]. 北京:地质出版社, 2003.

    Google Scholar

    Hou Zengqian. Hydrothermal Systems and Metallogeny on the Modern and Ancient Sea-Floor[M]. Geological Publishing House, Beijing, 2003.

    Google Scholar

    曾庆栋, 刘建明, 贾长顺, 等. 内蒙古赤峰市白音诺尔铅锌矿沉积喷流成因:地质和硫同位素证据[J]. 吉林大学学报(地球科学版), 2007, 37(4):659-667.

    Google Scholar

    Zeng Qingdong, Liu Jianming, Jia Changshun, et al. Sedimentary Exhalative Origin of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia:Geological and Sulfur Isotope Evidence[J]. Journal of Jilin University(Earth Science Edition), 2007, 37(4):659-667.

    Google Scholar

    马圣钞, 丰成友, 李国臣, 等. 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.

    Google Scholar

    Ma Shenchao, Feng Chengyou, Li Guochen, et al. Sulphur and Lead Isotope Compositions of the Hutouya Copper-Lead-Zinc Polymetallic Deposit in Qinghai Province and Their Genetic Sigifinance[J]. Geology and Exploration, 2012, 48(2):321-331.

    Google Scholar

    刘婷婷, 唐菊兴, 刘鸿飞, 等. 西藏墨竹工卡县洞中拉铅锌矿床S、Pb同位素组成及成矿物质来源[J]. 现代地质, 2011, 25(5):869-876.

    Google Scholar

    Liu Tingting, Tang Juxing, Liu Hongfei, et al. Sulphur and Lead Isotope Composition and Tracing for Sources of Ore-Forming Materials in The Dongzhongla Pb-Zn Deposits in Mozhugongka County, Tibet[J]. Geoscience, 2011, 25(5):869-876.

    Google Scholar

    沈渭洲, 丁悌平, 张宗清. 稳定同位素地质[M]. 北京:原子能出版社, 1987.

    Google Scholar

    Shen Weizhou, Ding Tiping, Zhang Zongqing. Stable Isotope Geology[M]. Atomic Press, Beijing, 1987.

    Google Scholar

    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(3):73-81.

    Google Scholar

    Wu Kaixing, Hu Ruizhong, Bi Xianwu, et al. Ore Lead Isotopes as a Tracer for Ore-Forming Material Sources: Areview[J]. Geology-Geochemistry, 2002, 30(3):73-81.

    Google Scholar

    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.

    Google Scholar

    Zhu Bingquan. Theory and Application of the Isotope Systems in Earth Science and the Evolution of the Crust and the Mantle[M]. Science Press, Beijing, 1998.

    Google Scholar

    张国伟, 董云鹏, 姚安平. 秦岭造山带基本组成与结构及其构造演化[J]. 陕西地质, 1997, 15(2):1-14.

    Google Scholar

    Zhang Guowei, Dong Yunpeng, Yao Anping. The Crustal Compositions, Structures and Tectonic Evolution of the Qinling Orogenic Belt[J]. Geology of Shaanxi, 1997, 15(2):1-14.

    Google Scholar

    Bruce E. Taylor. Biogenic and Thermogenic Sulfate Reduction in the Sullivan Pb-Zn-Ag Deposit, British Columbia (Canada):Evidence Frommicro-Isotopic Analysis of Carbonate and Sulfide in Bedded Ores[J]. Chemical Geology, 2004, 204:215-236.

    Google Scholar

    ElswickER, Morton J, WarnerMC, et al. Sulfur and Strontium Isotopic Composition of Massive Barites at Red Dog Alaska[J]. In Geological Society of America, 2000 Annual Meeting Abstracts with Programs-G

    Google Scholar

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