湖南芙蓉锡多金属矿床成矿流体地球化学

双燕, 毕献武, 胡瑞忠, 彭建堂, 苏文超, 朱长生. 湖南芙蓉锡多金属矿床成矿流体地球化学[J]. 岩石学报, 2009, 25(10): 2588-2600.
引用本文: 双燕, 毕献武, 胡瑞忠, 彭建堂, 苏文超, 朱长生. 湖南芙蓉锡多金属矿床成矿流体地球化学[J]. 岩石学报, 2009, 25(10): 2588-2600.

湖南芙蓉锡多金属矿床成矿流体地球化学

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  • [1]

    Bai DY,Chen JC,Ma TQ and Wang XH.2005. Geochemical characteristics and tectonic setting of Qitianling A-type granitic pluton in southeast Hunan.Acta Petrologica et Mineralogica,24(4):255-272(in Chinese with English abstract)

    [2]

    Bi CS,Shen XY,Xu QS.,Ming KH,Sun HL and Zhang CS.1993. Geological Characteristics of Stanniferous Granites in the Beilekuduk Tin Metallogenic Belt,Xinjiang.Acta Petrologica et Mineralogica,(3):213-223(in Chinese with English abstract)

    [3]

    Bi XW,Li HL,Shuang Y,Hu XY,Hu RZ and Peng JT.2008. Geochemical characteristics of fluid inclusions from Qitianling A-type granite,Hunan Province,China-tracing the source of ore forming fluid of the Furong superlarge tin\' deposit.Geological Journal of China Universities,14(4):539-548(in Chinese with English abstract)

    [4]

    Chen J,Wang RC,Zhou JP and Ji JF.2000. The geochemistry of Tin.Nanjing:Nanjing University Publication:1-320

    [5]

    Chen YJ and Li N.2009. Nature of ore-fluids of intracontinental intrusion-related hypothermal deposits and its difference from those in island arcs.Acta Petrologica Sinica,25(10):2477-2508

    [6]

    Chen YJ,Xiao WJ and Zhang JJ.2008. Ore-system as a geodynamic probe.Geology in China,35(6):1059-1073(in Chinese with English abstract)

    [7]

    Clayton RN,O\'Neil JR and Mayeda TK.1972. Oxygen Isotope Exchange between Quartz and Water.Journal of Geophysical Research,77:3057-3067

    [8]

    Craw D,Teagle DAH and Belocky R.1993. Fluid immiscibility in late-Alpine gold-bearing veins,Eastern and Northwestern European Alps.Mineralium Deposita,28(1):28-36

    [9]

    Evandro LK,Chris H,Christophe R,Andre G,Candido AVM and Kazuo F.2006. Fluid inclusion and stable isotope(O,H,C,and S)constraints on the genesis of the Serrinha gold deposit,Gurupi Belt,northern Brazil.Mineralium Deposita,V41(2):160-178

    [10]

    Fu JM,Ma CQ,Xie CF,Zhang YM and Peng SB.2004. Zircon SHRIMP dating of the Cailing granite on the eastern margin of the Qitianling granite,Hunan,South China,and its significance.Geology in China,31(1):96-100(in Chinese with English abstract)

    [11]

    Heinrich CA.1990. The chemistry of hydrothermal tin(-tungsten)ore deposition.Economic Geology,85(3):457-481

    [12]

    Huang GF,Gong SQ,Jiang XW,Tan SX,Li CB and Liu DH.2003. Exploration on the ore-forming regularities of tin deposits in Qitianling area,southern Hunan.Geological Bulletin of China,22(6):445-451(in Chinese with English abstract)

    [13]

    Huang GF,Zeng QW,Wei SL,Xu YM,Hou MS and Kang WQ.2001. Geological characteristics and ore-controlling factors of the Furong orefield,Qitianling,Hunan.Chinese Geology,28(10):30-34(in Chinese with English abstract)

    [14]

    Jiang SY,Zhao KD,Jiang YH,Ling HF and Ni P.2006. New type of tin mineralization related to granite in South China:Evidence from mineral chemistry,element and isotope geochemistry.Acta Petrologica Sinica,22(10):2509-2516(in Chinese with English abstract)

    [15]

    Li JD,Bai DY,Wu GY,Che QJ,Liu YR and Ma TQ.2005. Zircon SHRIMP dating of the Qitianling granite,Chenzhou,southern Hunan,and its geological significance.Geological Bulletin of China,24(5):411-414(in Chinese with English abstract)

    [16]

    Li ZL,Hu RZ,Peng JT,Bi XW and Li XM.2006. Helium isotope geochemistry of ore-forming fluids from Furong tin orefield in Hunan Province,China.Resource Geology,56(1):9-15

    [17]

    Li ZL,Hu RZ,Yang JS,Peng JT,Li XM and Bi XW.2007. He,Pb and S isotopic constraints on the relationship between the A-type Qitianling granite and the Furong tin deposit,Hunan Province,China.Lithos,In Press,Corrected Proof:331

    [18]

    Lu HZ,Fan HR,Ni P,Ou GX,Shen K and Zhang WH.2004. Fluid Inclusions.Beijing:Science Press,1-487(in Chinese)

    [19]

    Mao JW,Li XF,Bernd L,Chen W,Lan XM and Wei SL.2004.~(40)Ar-~(39)Ar dating of tin ores and related granite in Furong tin orefield,Hunan Province,and its geodynamic significance.Mineral Deposits,23(2):164-175(in Chinese with English abstract)

    [20]

    Mao JW,Wang ZL,Li HM,Wang CY and Chen YC.2003. Carbon and oxygen isotope components in the Permian Basalt-hosted copper deposit in Ludian Area,Yunnan:Implication for the mineralization process.Geological Review,49(6):610-615(in Chinese with English abstract)

    [21]

    Muller B,Frischknecht R,Seward T,Heinrich C and Gallegos WC.2001. A fluid inclusion reconnaissance study of the Huanuni tin deposit(Bolivia),using LA-ICP-MS micro-analysis.Mineralium Deposita,V36(7):680-688

    [22]

    Nilson BF and Márcia MA.1998. Granite-ore deposit relationships in Central Brazil.Journal of South American Earth Sciences,11(5):427-438

    [23]

    Ohmoto H.1972. Systematics of Sulfur and Carbon Isotopes in Hydrothermal Ore Deposits.Economic Geology,67(5):551-578

    [24]

    O\' Neil JR,Clayton RN and Mayeda TK.1969. Oxygen isotope fractionation in divalent metal carbonates.The Journal of Chemical Physics,51:5547-5558

    [25]

    Peng JT,Hu RZ,Bi XW,Dai TM,Li ZL,Li XM,Shuang Y,Yuan SD and Liu SR.2007.~(40)Ar/~(39)Ar isotopic dating of tin mineralization in Furong deposit of Hunan Province and its geological significance.Mineral Deposits,26(3):237-248(in Chinese with English abstract)

    [26]

    Peng JT and Hu RZ.2001. Carbon and oxygen isotope systematics in the Xikuangshan giant antimony deposit,Central Hunan.Geological Review,47(1):34-41(in Chinese with English abstract)

    [27]

    Peng JT,Zhou MF,Hu RZ,Shen NP,Yuan SD,Bi XW,Du AD and Qu WJ.2006. Precise molybdenite Re-Os and mica Ar-Ar dating of the Mesozoic Yaogangxian tungsten deposit,central Nanling district,South China.Miner Deposita,41:661-669

    [28]

    Qu XM,Hou ZQ,Zhou SG and Tang SH.2002. The age and tectonic setting of Lianlong Sn-bearing granite in Western Sichuan province.Acta Geoscientia Sinica,23(3):223-228(in Chinese with English abstract)

    [29]

    Ramboz C,Pichavant M and Weisbrod A.1982. Fluid immiscibility in natural processes:Use and misuse of fluid inclusion data:Ⅱ.Interpretation of fluid inclusion data in terms of immiscibility.Chemical Geology,37(1-2):29-48

    [30]

    Reilly CO,Jenkin GRT,Feely M,Alderton DHM and Fallick AE.1997. A fluid inclusion and stable isotope study of 200Ma of fluid evolution in the Galway Granite,Connemara,Ireland.Contributions to Mineralogy and Petrology,129(2):120-142

    [31]

    Schwartz MO.1989. Determining phase volumes of mixed CO_2-H_20 inclusions using microthermometric measurements.Mineralium Deposita,24(1):43-47

    [32]

    Shepherd TJ,Rankin AH and Alderton DHM.1985. A practical guide to fluid inclusion studies.Blackie:Distributed in the USA by Chapman and Hall,Glasgow,New York,xi,1-239

    [33]

    Shuang Y,Bi XW,Hu RZ,Peng JT,Li ZL,Li XM,Yuan SD and Qi YQ.2006. REE geochemistry of hydrothermal calcite from Furong tin polymetallic deposit and its indication of source of hydrothermal ore-forming fluid.J Mineral Petrol,26(2):57-65(in Chinese with English abstract)

    [34]

    Taylor HP.1974. The Application of Oxygen and Hydrogen Isotope Studies to Problems of Hydrothermal Alteration and Ore Deposition.Economic Geology,69(6):843-883

    [35]

    Wang XW,Wang XD,Liu JQ and Chang HL.2004. Relationship of Qitianling granite to Sn mineralization in Hunan province.Geological Science and Technology Information,23(2):1-12(in Chinese with English abstract)

    [36]

    Wei SL,Zeng QW,Xu YM,Lan XM,Kang WQ and Liao XY.2002. Characteristics and ore prospects of tin deposits in the Qitianling area,Hunan.Geology in China,29(1):67-75(in Chinese with English abstract)

    [37]

    Xu YM,Hou MS,Liao XY and Ao ZW.2000. Deposit types and prospect for prospecting of Sn deposits in Furong ore field,Chenzhou.Hunan Geology,19(2):95-100(in Chinese with English abstract)

    [38]

    Zhang LG.1985. The application of stable isotopes in geological sciences.Xi\'an:The Shangxi Scientifica publication,1-267

    [39]

    Zhao KD,Jiang SY,Jiang YH and Wang RC.2005. Mineral chemistry of the Qitianling granitoid and the Furong tin ore deposit in Hunan Province,South China:Implication for the genesis of granite and related tin mineralization.European Journal of Mineralogy,17(4):635-648

    [40]

    Zhao ZH,Bao ZW,Zhang BY and Xiong XL.2000. The crust-mantle interaction geodynamics setting of Shizhuyuan super-large W polymetallic deposit.Science in China(Series D),30(suppl.):161-168(in Chinese)

    [41]

    Zheng JJ and Jia BH.2001. Geological characteristics and related tinpolymetallic mineralization of the Qitianling granite complex in Southern Hunan Province.Geology and Mineral Resources of South China,(4):50-57(in Chinese with English abstract)

    [42]

    Zhu JC,Huang GF,Zhang PH,Li FC and Rao B.2003. On the emplacement age and material sources for the granites of Cailing Superunit,Qitianling pluton,South Hunan Province.Geological Review,49(3):245-252(in Chinese with English abstract)

    [43]

    Zhu JC,Zhang H,Xie CF,Zhang PH and Yang C.2005. Zircon SHRIMP U-Pb geochronology,petrology and geochemistry of the Zhujianshui Granite,Qitianling pluton,Southern Hunan Province.Geological Journal of China Universities,11(3):335-342(in Chinese with English abstract)

    [44]

    柏道远,陈建超,马铁球,王先辉.2005.湘东南骑田岭岩体A型花岗岩的地球化学特征及其构造环境.岩石矿物学杂志,24(4):255-272

    [45]

    毕承思,沈湘元,徐庆生,明奎海,孙惠礼,张春生.1993.新疆贝勒库都克锡矿带含锡花岗岩地质特征.岩石矿物学杂志,(3):213-223

    [46]

    毕献武,李鸿莉,双燕,胡晓燕,胡瑞忠,彭建堂.2008.骑田岭A型花岗岩流体包裹体地球化学特征-对芙蓉超大型锡矿成矿流体来源的指示.高校地质学报,14:539-548

    [47]

    陈骏,王汝成,周建平,季骏峰.2000.锡的地球化学.南京大学出版社,南京,1-320

    [48]

    陈衍景,李诺.2009.大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异.岩石学报,25(10):2477-2508

    [49]

    陈衍景,肖文交,张进江.2008.成矿系统:地球动力学的有效探针.中国地质,35(6):1059-1073

    [50]

    付建明,马昌前,谢才富,张业明,彭松柏.2004.湖南骑田岭岩体东缘菜岭岩体的锆石shrimp定年及其意义.中国地质,31(1):96-100

    [51]

    黄革非,龚述清,蒋希伟,谭双喜,黎传标.刘东红.2003.湘南骑田岭锡矿成矿规律探讨.地质通报,22(6):445-451

    [52]

    黄革非,曾钦旺,魏绍六,许以明,侯茂松,康卫清.2001.湖南骑田岭芙蓉矿田锡矿地质特征及控矿因素初步分析.中国地质,28(10):30-34

    [53]

    蒋少涌,赵葵东,姜耀辉,凌洪飞,倪培.2006.华南与花岗岩有关的一种新类型的锡成矿作用:矿物化学、元素和同位素地球化学证据.岩石学报,22(10):2509-2516

    [54]

    李金冬,柏道远,伍光英,车勤建,刘耀荣,马铁球.2005.湘南郴州地区骑田岭花岗岩锆石Shrimp定年及其地质意义.地质通报,24(5):411-414

    [55]

    卢焕章,范宏瑞,倪培,欧光习,沈昆,张文淮.2004.流体包裹体.北京:科学出版社,1-487

    [56]

    毛景文,李晓峰,Bemd Lehmann,陈文,蓝晓明,魏绍六.2004.湖南芙蓉锡矿床锡矿石和有关花岗岩的~(40)Ar-~(39)Ar年龄及其地球动力学意义.矿床地质,23(2):164-175

    [57]

    毛景文,王志良,李厚民,王成玉,陈毓川.2003.云南鲁甸地区二叠纪玄武岩中铜矿床的碳氧同位素对成矿过程的指示.地质论评,49(6):610-615

    [58]

    彭建堂,胡瑞忠,毕献武,戴植谟,李兆丽,李晓敏,双燕,袁顺达,刘世荣.2007.湖南芙蓉锡矿床~(40)Ar/~(39)Ar同位素年龄及地质意义.矿床地质,26(3):237-248

    [59]

    彭建堂,胡瑞忠.2001.湘中锡矿山超大型锑矿床的碳、氧同位素体系.地质论评,47(1):34-41

    [60]

    双燕,毕献武,胡瑞忠,彭建堂,李兆丽,李晓敏,袁顺达,齐有强.2006.芙蓉锡矿方解石稀土元素地球化学特征及其对成矿流体来源的指示.矿物岩石,26(2):57-65

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