金川Ⅰ号岩体橄榄石Ni-MgO相互关系及其地质意义

陈列锰, 宋谢炎, Danyushevsky LV, 肖加飞, 李士彬, 官建祥. 金川Ⅰ号岩体橄榄石Ni-MgO相互关系及其地质意义[J]. 岩石学报, 2009, 25(12): 3369-3378.
引用本文: 陈列锰, 宋谢炎, Danyushevsky LV, 肖加飞, 李士彬, 官建祥. 金川Ⅰ号岩体橄榄石Ni-MgO相互关系及其地质意义[J]. 岩石学报, 2009, 25(12): 3369-3378.

金川Ⅰ号岩体橄榄石Ni-MgO相互关系及其地质意义

  • 加载中
  • [1]

    Arndt NT,Partitioning of nickel between olivine and ultrabesic and basic komatiite liquids,Carnegie Institution of Washington Yearbook,1977.

    [2]

    Asimow PD,Ghiorso MS,Algorithmic modifications extending MELTS to calculate subsolidus phase relations,American Mineralogist,1998(9-10).

    [3]

    Barnes SJ,Coats C,Naldrett A,Petrogenesis of a Proterozoic nickel-sulfide-komatiite association,the Katiniq Sill,Ungnva,Quebec,Economic Geology,1982(2).

    [4]

    Barnes SJ,The petrography and geochemistry of komatiite flows from the Abitibi Greenstone Belt and a model for their formation,Lithos,1985.

    [5]

    Barnes SJ,Naldrett AJ,Geochemistry of the J-M(Howland)Reef of the Stillwater Complex,Minneapolis Adit area; Ⅰ,Sulfide chemistry and sulfide-olivine equilibrium,Economic Geology,1985(3).

    [6]

    Barnes SJ,The effect of trapped liquid crystallization on cumulus mineral compositions in layered intrusions,Contributions to Mineralogy & Petrology,1986(4).

    [7]

    Barnes SJ,Maier WD,The fractionation of Ni,Cu and the noble metals in silicate and sulphide liquids,Geo.Assoc.of Canada,1999.

    [8]

    Beard JH,A procedure for calculating the equilibrium distribution of trace elements among the minerals of cumulate rocks,and the concentration of trace elements in the coexisting liquids,Chemical Geology,1994(1-4).

    [9]

    Brenan JM,Caciagli NC,Fe-Ni exchange between olivine and sulphide liquid:Implications for oxygen barometry in sulphidesaturated magmas,Geochim Casmochim Acta,2000(2).

    [10]

    Brenan JM,Effects of f_(o_2,)f_(s_2),temperature,and melt composition on Fe-Ni exchange between olivine and sulfide liquid:Implications for natural olivine-sulfide assemblages,Geochimica et Cosmochimica Acta,2003(14).

    [11]

    Campbell FE,Roeder PL,The solubility of olivine and pyroxene in the Ni-Mg-Si-O system,American Mineralogist,1968.

    [12]

    Chai G,Naldrett AJ,Characteristics of Ni-Cu-PGE mineralization and genesis of the Jinchuan deposit,Northwest China,Economic Geology,1992(6).

    [13]

    Chai G,Naldrett AJ,The Jinchuan ultramafic intrusion:Cumulate of a high-Mg basaltic magma,Journal of Petrology,1992(2).

    [14]

    Chen LM,Song XY,Nie XY,Zhou GF,Liu SR,Zheng WQ and Li SB,Mineral chemistry and geological significance of pyroxene from segment Ⅱ of the Jinchuan intrusion,Gansu J Miner Petrol,2008(1).

    [15]

    Chen LM,Song XY,Danyushevsky LV,Xiao JF Zhu D Zhou GF Guan JX Liu SR and Zheng WQ,Parental magma compositions of the Jinchuan intrusion,Gansu Province and MELTS thermodynamic modelling of fractional crystallization,Acta Geologica Sinica,2009(9).

    [16]

    De Waal SA,Xu ZG,Li CS,Mouri H,Emplacement of viscous mushes in the Jinchuan ultramafic intrusion,western China,Canadian Mineralogy,2004.

    [17]

    Dowling S,Hill R,The distribution of PGE in fractionated Archaean komatiites,Western and Central Ultramafic Units,Mt Keith region,Western Australia,Australian Journal of Earth Sciences,1992(3).

    [18]

    Ghiorso MS,Sack RO,Chemical transfer in magmatic processes Ⅳ:A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures,Mineralogy and Petrology,1995.

    [19]

    Lehmann J,Arndt N,Windley B,Zhou MF,Wang CY and Harris C,Field relationships and geochemical constraints on the emplacement of the Jinchuan intrusion and its Ni-Cu-PGE sulfide deposit,Gansu,China,Economic Geology,2007(1).

    [20]

    Li C,Naldrett AJ,Geology and petrology of the Voisey\'s Bay intrusion:Reaction of olivine with sulfide and silicate liquids,Lithns,1999(1-2).

    [21]

    Li C,Lightfoot PC,Amelin Y,Naldrett AJ,Contrasting petrological and geochemical relationships in the Voisey\'s Bay and Mushuau intrusions,Labrador,Canada:Implications for ore genesis,Econ Ceol,2000(4).

    [22]

    Li C,Ripley EM,Mathez EA,The effect of S on the partitioning of Ni between olivine and silicate melt in MORB,Chemical Geology,2003(3-4).

    [23]

    Li C,Ripley EM,Naldrett AJ,Compositional variations of olivine and sulfur isotopes in the Noril\'sk and Talnakh intrusions,Siberia:Implications for ore-forming processes in dynamic magma conduits,Economic Geology,2003(1).

    [24]

    Li C,Xu Z,Sybrand AW,Edward MR and Wolfgang DM,Compositional variations of olivine from the Jinchuan Ni-Cu sulfide deposit,western China:Implications for ore genesis,Mineral Deposits,2004(2).

    [25]

    Li C,Anthony J Nalddrett,Ripley EM,Controls on the Fo and Ni contents of olivine in sulfide-bearing mafic-ultramafic intrusions:Principles,models and examples hem Voisey\'s Bay,Earth Sciences Frontiers,2007(5).

    [26]

    Li SB,Song XY,Hu RZ,Chen LM and Nie XY,Lithological feature of the segment Ⅱ of the Jinchuan intrusion and discussion on fractional crystallization,Acta Petrologica Sinica,2007(10).

    [27]

    Li SB,Hu RZ,Song XY,Chen LM and Shen NP,Sulfide separation control in Ni content of olivine in bearing-ore intrusion of magma deposit:An example from Jinchuan intrusion,Bull Miner Petrol and Geochem,2008(2).

    [28]

    Li XH,Su L,Song B,Liu DY,SHRIMP U-Pb zircon age of the Jinchuan ultramafic intrusion and its geological significance,Chinese Science Bulletin,2004(4).

    [29]

    Li XH,Su L,Chung SL,Li ZX,Liu Y,Song B and Liu DY,Formation of the Jinchuan ultramafic intrusion and the world\'s third largest Ni-Cu sulfide deposit; associated with approximately 825 Ma south China mantle plume,Geochemistry Geophysics and Geosystems,2005(11).

    [30]

    Peach CL,Mathez EA,Sulfide melt-silicate melt distribution coefficients for nickel and iron and implications for the distribution of other chalcophile elements,Geochimica et Cosmochimica Acta,1993(13).

    [31]

    Roeder PL,Emslie RE,Olivine-liquid equilibrium Contrib,Mineralogy and Petrology,1970(4).

    [32]

    Simkin T,Smith JV,Minor element distribution in olivine,Journal of Geology,1970(3).

    [33]

    Smith PM,Asimow PD,Adiabat_1 ph:A new public front-end to the MELTS,pMELTS,and pHMELTS models,Geochemistry Geophysics and Geosystems,2005(1).

    [34]

    Song XY,Li SB,Wang YS,Ba DH and Chen LM,Significance of conduit of sulfide-bearing magma for exploration of magmatic sulfide deposit,Bull Mineral Petrol and Geochem,2005(4).

    [35]

    Song XY,Zhou MF,Wang CY,Qi L and Zhang CJ,Role of crustal contamination in formation of the Jinchuan intrusion and its world-class Ni-Cu-(PGE)sulfide deposit,Northwest China,International Geology Review,2006(12).

    [36]

    Xie GH,Wang YL,Fan CY,Zhang CJ and Zheng R,Ultramafic intrusion and diagenetic-mineralizatian mechanism of ultralarge sulfide deposit in the Jinchuan,Science in China(Series D),1998(zk).

    [37]

    Tang ZL,Model of the Jinchuan Cu-Ni sulfide deposit,Geoscience,1990(4).

    [38]

    Tang ZL,Li WY,Genesis Model and Geological Contrast of the Jinchuan(Pt-bearing)Cu-Ni Sulfide Deposit,北京:地质出版社,1995.

    [39]

    Tang ZL,Bai YL,Geotectonic framework and metallogenic system in the southwest margin of North China Paleocontinent,Earth Sciences Frontiers,1999(2).

    [40]

    Wang RT,Mao JW,He H,He Y,Sumary of studying on metallogenesis of nickel-copper sulfide magatic ore deposits,Engineering Science,2003(3).

    [41]

    Yang G,Du AD,Lu JR,Qu WJ and Chen JF,Re-Os(ICP-MS)dating of the massive sulfide ores from the Jinchuan Ni-Cu-PGE deposit,Science in China(Series D),2005(3).

    [42]

    Yang S,Qu W,Tian Y,Chen J,Yang G and Du A,Origin of the inconsistent apparent Re-Os ages of the Jinchuan Ni-Cu sulfide ore deposit,China:Post-segregatian diffusion of Os,Chemical Geology,2008(3-4).

    [43]

    陈列锰.宋谢炎.聂晓勇.周国富.刘世荣.郑文勤.李士彬 甘肃金川Ⅱ号岩体辉石化学特征及其地质意义 [J].-矿物岩石2008(1)

    [44]

    陈列锰,宋谢炎,Danyushevsky LV,肖加飞,朱丹,周国富,官建样,刘世荣,郑文勤,金川岩体母岩浆成分及其分离结晶过程的熔浆热力学模拟,地质学报,2009(9).

    [45]

    李士彬.宋谢炎.胡瑞忠.陈列锰.聂晓勇 甘肃金川Ⅱ号岩体岩相学特征及分离结晶过程探讨 [J].-岩石学报2007(10)

    [46]

    李士彬.胡瑞忠.宋谢炎.陈烈锰.沈能平 硫化物熔离对岩浆硫化物含矿岩体中橄榄石Ni含量的影响--以金川岩体为例 [J].-矿物岩石地球化学通报2008(2)

    [47]

    李献华.苏犁.宋彪.刘敦一 金川超镁铁侵入岩SHRIMP锆石U-Pb年龄及地质意义 [J].-科学通报2004(4)

    [48]

    宋谢炎.李士彬.王玉山.把多恒.陈烈锰 含矿岩浆通道对于岩浆铜镍硫化物矿床找矿工作的意义[J].矿物岩石地球化学通报2005(4)

    [49]

    汤中立 金川硫化铜镍矿床成矿模式 [J].-现代地质1990(4)

    [50]

    汤中立,李文渊,金川铜镍硫化物(含铂)矿床成矿模式及地质对比,北京:地质出版社,1995.

    [51]

    汤中立.白云来 华北古大陆西南边缘构造格架与成矿系统 [J].-地学前缘1999(2)

    [52]

    王瑞廷.毛景文.任小华.王民良.赫英 煎茶岭与金川硫化镍矿床的铂族元素地球化学特征对比及其意义 [J].-矿床地质2005(4)

    [53]

    解广轰,汪云亮,范彩云,金川超镁铁岩侵入体及超大型硫化物矿的成岩成矿机制,中国科学d辑,1998(zk).

    [54]

    杨刚.杜安道.卢记仁.屈文俊.陈江峰 金川镍-铜-铂矿床块状硫化物矿石的Re-Os(ICP-MS)定年 [J].-中国科学D辑2005(3)

    [55]

    甘肃省地矿局第六地质队,甘肃省永昌县自家咀子铜镍矿第一矿区地质勘探补充报告,1964.

  • 加载中
计量
  • 文章访问数:  6631
  • PDF下载数:  6282
  • 施引文献:  0
出版历程
刊出日期:  2009-12-31

目录