新疆东天山黄山岩带镁铁—超镁铁质岩石成因及成矿作用
|
摘要
新疆北部康古尔-黄山韧性剪切带发育有一系列镁铁-超镁铁质岩体，其中土墩、香山、黄山、黄山东、葫芦和图拉尔根岩体产出有工业矿床，二红洼和黄山南岩体中均发现了不同程度的铜镍硫化物矿化。近年来，随着勘探深度和网度的加大，资源量得到了大幅增加，使得该带目前已成为我国第二个世界级的岩浆铜镍硫化物矿床成矿带。论文选择二红洼、香山、黄山南、黄山、黄山东、葫芦岩体为研究对象，紧扣岩浆硫化物矿床的关键岩石学问题：①岩浆源区的性质和原生岩浆的组成；②是否有同化混染作用，混染物的类型和混染程度，同化混染作用与硫化物分凝之间的关系；③分离结晶、岩浆演化过程。通过岩石学、矿物学、元素地球化学以及Nd、Sr、Pb同位素地球化学方法，就含矿岩体与弱矿化岩体、含硫化物矿床岩体与含氧化物矿床岩体进行系统研究，主要获得以下几方面的成果：
(1)含矿岩体岩相分带清楚，岩石蚀变较强；弱矿化岩体岩相分带较差，岩石新鲜，蚀变弱，岩石组合中橄榄岩相所占比例小。
(2)含矿岩体与弱矿化岩体稀土元素地球化学特征存在较大差异，含矿岩体稀土元素总量高于弱矿化岩体，其轻重稀土元素之间以及轻、重两组稀土元素内部分馏程度明显强于弱矿化岩体。
(3)含矿岩体均发生了不同程度陆壳物质的混染，黄山东和葫芦岩体分别遭受了约5%、5%-10%中-上陆壳物质的混染，黄山、香山岩体遭受了不同程度中-下地壳的混染，而弱矿化的黄山南岩体局部遭受较弱同化混染作用，二红洼岩体基本没有遭受陆壳混染。
(4)利用Mg~#以及液相线橄榄石Fo分子约束原生岩浆的MgO含量。除香山岩体原生岩浆MgO含量下限值稍低(5．0%)外，含矿岩体原生岩浆均为高镁拉斑玄武质岩浆。其中，黄山东岩体的原生岩浆MgO含量为11．6%，黄山岩体和葫芦岩体原生岩浆MgO含量下限值分别为9．2%，7．1%；而弱矿化的二红洼岩体原生岩浆MgO含量为7．1%，黄山南岩体原生岩浆MgO含量下限值为5．7%。
(5)含矿岩体地球化学特征表明，导致硫化物过饱和熔离的主要原因是岩浆结晶分异和同化混染作用过程中富Si组分的加入。
(6)香山中含铜镍矿岩体和香山西含钒钛磁铁矿岩体具有不同成矿专属性的岩石系列。香山中含铜镍矿岩体中无原生磁铁矿出现，岩石化学成分明显富MgO，贫FeO_T、TiO_2，具有较弱的正、负铕异常。含矿岩相m/f值(3．97-5．53)，为铁质超基性岩。香山西含钒钛磁铁矿岩体中有一定数量的原生磁铁矿，岩石富FeO_T、TiO_2、Al_2O_3，普遍具有显著的正铕异常。钛铁辉长岩的m/f值(0．68-0．90)，属于铁质基性岩。岩浆自身演化过程和流体的广泛参与，应该对形成CuNi-VTi复合型矿床起到了主要作用。
(7)Nd、Sr、Pb同位素及相关微量元素研究表明，岩体具有相似的岩浆源区。岩浆源区由被消减板片交代的地幔楔物质和软流圈地幔物质组成。岩石圈根部拆沉和软流圈地幔上涌过程中生成了黄山岩带的镁铁-超镁铁岩体。
A series of mafic-ultramafic intrusions occur in the Kangguer-Huangshan shear zone in northXinjiang,including Tudun,Xiangshan,Huangshan,Huangshandong and Tulargen economic mineralizedintrsions,Erhongwa and Huangshannan intrsions with variable degrees of copper-nickel sulphidemineralization.In recent years,with the increasing exploration depth and density,reserves has substantialincreased,Kangguer- Huangshan zone has now become the second world-class magmatic copper-nickelsulfide deposit metallogenic zone in China.Erhongwa,Xiangshan,Huangshannan,Huangshan,Huangshandong,Hulu intrusions were selected for detailed study,focusing on the key petrology issues ofmagmatic sulfide deposits:①the nature of magma source and the composition of primary magma;②whether the intrusion has underwent crustal contamination or not,the type of hybrids and the degree ofcrustal contamination,the relationship between crustal contamination and sulphide segregation;③fractional crystallization,magma evolution.Systematically comparison between economic mineralizedintrusions and uneconomic mineralized intrusions,oxides deposits and sulfide deposits respectively werecarried out based on petrology,mineralogy,element geochemistry,Nd,Sr,and Pb isotope geochemistry.The following are the main results:
(1) The economic mineralized intrusions have clear facies and highly altered,while the uneconomicmineralized intrusions are fresh.there are a few peridotite.
(2)Geochemistry characteristics of rare earth element has obvious difference between the economicmineralized intrusions and the uneconomic mineralized intrusions.The economic mineralized intrusionshave significantly higher content of the total rare earth elements than that of the uneconomic mineralizedintrsions,and the degree of the LREEs fractionation of the formers,as well as the HREEs,are also strongerthan that of the latters.
(3) The economic mineralized intrusions underwent crustal contamination to some extent.For example,Huangshandong and Hulu intrusion were subjected to comtaminated about 5%,5%～10% byupper-intermediate continental crust.Huangshan intrusion and Xiangshan intrusion contamination hascome from the intermediate-lower crust.In contrast,the uneconomic mineralized intrusions,such asHuangshannan intrusion,only experienced partially contamination,Erhongwa intrusion didnot have theimpact of crustal contamination.
(4) The Fo molecules of olivine and Mg~# are used to restrict the MgO content of the primary magma. Rearch proves that the MgO content of the economic mineralized intrusions are higher than that of theuneconomic mineralized intrusions,although the minimum MgO content of Xiangshan intrusion is 5.0%.Among the economic mineralized intrusions,the MgO content of primary magma of Huangshandonginstrusion is 11.6%;the minimum MgO content of primary magma of Huangshan instrusion and Huluintrusion is respectively 9.2%,7.1%,While among the uneconomic mineralized intrusions,the MgOcontent of primary magma of Erhongwa intrusion is 7.1%,and the minimum MgO content of primarymagma of Huangshannan instrusion is 5.7%.
(5) Magmatic crystallization and crustral contamination comeing from Si-rich component lead to sulfidesaturation in economic mineralized intrusions.
(6) Xiangshanzhong intrusion of Cu-Ni deposit and Xiangshanxi intrusion of V-Ti-Fe deposit have differentwith rock series.Xiangshanzhong intrusion have no primary magnetite,with rich in MgO,low in FeO_T,TiO_2 and positive/negative Eu anomalies.The m/f ratio of rock is 3.97-5.53 and belong to ferruginousultrabasic rocks.However Xiangshanxi intrusion have some primary magnetite,are rich in FeO_T,TiO_2 andhave obvious positive Eu anomalies.The m/f ratio of Fe-Ti gabbro is 0.68-0.90 and belong toferruginous basic rocks.Participating in fluid and magmatic evolution itself are the key to from theCuNi-VTi composite deposits.
(7) Nb、Sr、Pb isotope and trace element geochemistry characters indicate that magma source of theseintrusions were similar and composed of wedge matasomasised by subducting slab and aesethenospherecomponents.The mafic-ultramafic intrusions of Huangshan terrane are the result of the lithosphericdelamination at the root and the upwelling of asthenosphere components.
(1)含矿岩体岩相分带清楚，岩石蚀变较强；弱矿化岩体岩相分带较差，岩石新鲜，蚀变弱，岩石组合中橄榄岩相所占比例小。
(2)含矿岩体与弱矿化岩体稀土元素地球化学特征存在较大差异，含矿岩体稀土元素总量高于弱矿化岩体，其轻重稀土元素之间以及轻、重两组稀土元素内部分馏程度明显强于弱矿化岩体。
(3)含矿岩体均发生了不同程度陆壳物质的混染，黄山东和葫芦岩体分别遭受了约5%、5%-10%中-上陆壳物质的混染，黄山、香山岩体遭受了不同程度中-下地壳的混染，而弱矿化的黄山南岩体局部遭受较弱同化混染作用，二红洼岩体基本没有遭受陆壳混染。
(4)利用Mg~#以及液相线橄榄石Fo分子约束原生岩浆的MgO含量。除香山岩体原生岩浆MgO含量下限值稍低(5．0%)外，含矿岩体原生岩浆均为高镁拉斑玄武质岩浆。其中，黄山东岩体的原生岩浆MgO含量为11．6%，黄山岩体和葫芦岩体原生岩浆MgO含量下限值分别为9．2%，7．1%；而弱矿化的二红洼岩体原生岩浆MgO含量为7．1%，黄山南岩体原生岩浆MgO含量下限值为5．7%。
(5)含矿岩体地球化学特征表明，导致硫化物过饱和熔离的主要原因是岩浆结晶分异和同化混染作用过程中富Si组分的加入。
(6)香山中含铜镍矿岩体和香山西含钒钛磁铁矿岩体具有不同成矿专属性的岩石系列。香山中含铜镍矿岩体中无原生磁铁矿出现，岩石化学成分明显富MgO，贫FeO_T、TiO_2，具有较弱的正、负铕异常。含矿岩相m/f值(3．97-5．53)，为铁质超基性岩。香山西含钒钛磁铁矿岩体中有一定数量的原生磁铁矿，岩石富FeO_T、TiO_2、Al_2O_3，普遍具有显著的正铕异常。钛铁辉长岩的m/f值(0．68-0．90)，属于铁质基性岩。岩浆自身演化过程和流体的广泛参与，应该对形成CuNi-VTi复合型矿床起到了主要作用。
(7)Nd、Sr、Pb同位素及相关微量元素研究表明，岩体具有相似的岩浆源区。岩浆源区由被消减板片交代的地幔楔物质和软流圈地幔物质组成。岩石圈根部拆沉和软流圈地幔上涌过程中生成了黄山岩带的镁铁-超镁铁岩体。
A series of mafic-ultramafic intrusions occur in the Kangguer-Huangshan shear zone in northXinjiang,including Tudun,Xiangshan,Huangshan,Huangshandong and Tulargen economic mineralizedintrsions,Erhongwa and Huangshannan intrsions with variable degrees of copper-nickel sulphidemineralization.In recent years,with the increasing exploration depth and density,reserves has substantialincreased,Kangguer- Huangshan zone has now become the second world-class magmatic copper-nickelsulfide deposit metallogenic zone in China.Erhongwa,Xiangshan,Huangshannan,Huangshan,Huangshandong,Hulu intrusions were selected for detailed study,focusing on the key petrology issues ofmagmatic sulfide deposits:①the nature of magma source and the composition of primary magma;②whether the intrusion has underwent crustal contamination or not,the type of hybrids and the degree ofcrustal contamination,the relationship between crustal contamination and sulphide segregation;③fractional crystallization,magma evolution.Systematically comparison between economic mineralizedintrusions and uneconomic mineralized intrusions,oxides deposits and sulfide deposits respectively werecarried out based on petrology,mineralogy,element geochemistry,Nd,Sr,and Pb isotope geochemistry.The following are the main results:
(1) The economic mineralized intrusions have clear facies and highly altered,while the uneconomicmineralized intrusions are fresh.there are a few peridotite.
(2)Geochemistry characteristics of rare earth element has obvious difference between the economicmineralized intrusions and the uneconomic mineralized intrusions.The economic mineralized intrusionshave significantly higher content of the total rare earth elements than that of the uneconomic mineralizedintrsions,and the degree of the LREEs fractionation of the formers,as well as the HREEs,are also strongerthan that of the latters.
(3) The economic mineralized intrusions underwent crustal contamination to some extent.For example,Huangshandong and Hulu intrusion were subjected to comtaminated about 5%,5%～10% byupper-intermediate continental crust.Huangshan intrusion and Xiangshan intrusion contamination hascome from the intermediate-lower crust.In contrast,the uneconomic mineralized intrusions,such asHuangshannan intrusion,only experienced partially contamination,Erhongwa intrusion didnot have theimpact of crustal contamination.
(4) The Fo molecules of olivine and Mg~# are used to restrict the MgO content of the primary magma. Rearch proves that the MgO content of the economic mineralized intrusions are higher than that of theuneconomic mineralized intrusions,although the minimum MgO content of Xiangshan intrusion is 5.0%.Among the economic mineralized intrusions,the MgO content of primary magma of Huangshandonginstrusion is 11.6%;the minimum MgO content of primary magma of Huangshan instrusion and Huluintrusion is respectively 9.2%,7.1%,While among the uneconomic mineralized intrusions,the MgOcontent of primary magma of Erhongwa intrusion is 7.1%,and the minimum MgO content of primarymagma of Huangshannan instrusion is 5.7%.
(5) Magmatic crystallization and crustral contamination comeing from Si-rich component lead to sulfidesaturation in economic mineralized intrusions.
(6) Xiangshanzhong intrusion of Cu-Ni deposit and Xiangshanxi intrusion of V-Ti-Fe deposit have differentwith rock series.Xiangshanzhong intrusion have no primary magnetite,with rich in MgO,low in FeO_T,TiO_2 and positive/negative Eu anomalies.The m/f ratio of rock is 3.97-5.53 and belong to ferruginousultrabasic rocks.However Xiangshanxi intrusion have some primary magnetite,are rich in FeO_T,TiO_2 andhave obvious positive Eu anomalies.The m/f ratio of Fe-Ti gabbro is 0.68-0.90 and belong toferruginous basic rocks.Participating in fluid and magmatic evolution itself are the key to from theCuNi-VTi composite deposits.
(7) Nb、Sr、Pb isotope and trace element geochemistry characters indicate that magma source of theseintrusions were similar and composed of wedge matasomasised by subducting slab and aesethenospherecomponents.The mafic-ultramafic intrusions of Huangshan terrane are the result of the lithosphericdelamination at the root and the upwelling of asthenosphere components.
引文
1.Kepezhinskas P,McDermott F,Defant MJ et al.Trace element and Sr-Nd-Pb isotopic constraints on a three-component model of Kamchatka Arc petrogenesis[J].Geochimica et Cosmochimica Acta,1997,61(3):577-600
2.Kerr A.Nickeliferous gabbroic intrusions of the Pants Lake area,Labrador,Canada:implications for the development of magmatic sulfides in mafic systems[J].Am.J.Sci,2005,303:221-258
3.Meibom A,Sleep NH,Chamberlain CP et al.,Re-Os isotopic evidence for long-lived heterogeneity and equilibration processes in the Earth's upper mantle[J].Nature,2002,419:705-708.
4.Niu YL.Bulk-rock Major and Trace Element Compositions of Abyssal Peridotites:Implications for Mantle Melting,Melt Extraction and Post-melting Processes Beneath Mid-Ocean Ridges.Journal of Petrology,2004,45(12):2423-2458
5．金川公司信息中心．世界镍矿资源现状[R]．内部资料．2000
6．汤中立．中国的小岩体岩浆矿床[J]．中国工程科学，2002,4(6)：9-12．
7．毛景文，杨建民，屈文俊等．新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J]．矿床地质，2002，21(4)：323-330
8.Zhou MF,Leshen CM,Yang ZX et al.Geochemistry and petrogenesis of 270 Ma Ni-Cu-(PGE) sulfide-bearing mafic-ultramafic intrusions in Huangshan district,eastern Xinjiang,northwest China:implications for the tectonic evolution of the Central Asian orogenic belt[J].Chemical Geology,2004,209:233-257
9．韩宝福，季建清，宋彪等．新疆喀拉通克和黄山东含铜镍矿镁铁-超镁铁杂岩体的SHRIMP锆石U-Pb年龄及其地质意义[J]．科学通报，2004，49(22)：2324-2328
10.Zhang ZH,Mao JW,Du AD et al.Re-Os dating of two Cu-Ni sulfide deposits in northern Xinjiang,NW China and its geological significance[J].Journal of Asian Earth Sciences,2008,doi:10.1016/j.jseaes.2007.10.005
11．焦建刚．甘肃龙首山地区小岩体成大矿深部过程[D]．长安大学,2007,5
12.Naldrett AJ.IGCP.Projeet No.161 and a Proposed classification of Ni-Cu-PGE sulfide deposits[J].Canadian mineralogist,1979,17:143-145
13.Naldrett AJ.Niekel sulfides deposits:classification,composition,and genesis[J].Eeon.Geol.,1981,6:28-65
14.Naldrett AJ.Magma Sulfide Deposits Geology,Geochemistry And Exploration[M].Springer,2004,1-17
15.Ross JR,Travis GA.The niekel sulfide deposits in westem Australia in global Perspective[J].Economic Geology,1981,76(6):1291-1329
16．陈浩琉，吴水波，傅德彬等．镍矿床[M]．地质出版社，1993，22-57
17．汤中立．中国硫化镍矿床类型[J]．地质学报，1987,27(4)：350～369
18．汤中立S．J．Barnes，岩浆硫化物矿床成矿机制，北京：地质出版社，1998
19．汤中立，闫海卿，焦建刚等．中国岩浆硫化物矿床新分类与小岩体成矿作用[J]．矿床地质．2006．25(1)：1-8
20．汤中立．中国镁铁、超镁铁岩浆矿床成矿系列的聚集与演化[J]．地学前缘，2004，11(1)：113-119．
21.Naldrett A J,Duke JM,Lightfoot PC et al.Quantitative Modelling of the segregation of magrnatic sulfides:an exploration guide[J].Bull Can Inst Min Metall,1984,77:46-57
22.Naldrett AJ.Magmatic sulfide deposit[M]:New York,Oxford University Press,1989
23.Naldrett AJ.An overview of Ni-Cu mineralization with conclusions guide in exploration (Z).International Geological Correlation Programme 479 short course notes,2004,154-164
24.Lightfoot PC and Hawkesworth C J.Flood basalts and magmatic Ni,Cu and PGE sulphide mineralization:Comparative geochemistry of the Noril'sk (Siberian Trap) and West Greenland sequences[A].In:Mahoney JJ and Coffin MF,ed.Large igneous province[M].Washington D C:American Geophysical Union.1997.357-380.
25.Maclean WH.Liquid phase relations in the FeS-FeO-Fe2O3-SiO2 sysytems and their applications in geology[J].Economic Geology,1969,64:865-884
26.Shima H,Naldrett AJ.Solubility of sulfur in ultrmafic melt and the relevance of the system Fe-S-O[J].Economic Geology.1975,70:960-967
27.Holzheid A,Grove TL.Sulfur saturation limits in silicate melts and their implications for core formation scenarios for terrestrial planets[J].American Mineralogist,2002,87:227-237
28.Lorand J P.Are spinel iherzolite xenoliths representative of the sulfur content of the upper mantle[J].Geochim.Cosmochim.Acta,1990,54:1487-1492.
29.McDonough WF and Sun SS.The composition of the earth[J].Chem.Geol.,1995,120:233-253.
30.Keays RR.The role of komatiitic and picritic magrnatism and S saturation in the formation of ore deposits[J].Lithos,1995,34:1-18
31.Wendlandt RE Sulphide saturation of basalt and andesite melts at high pressures and temperature[J].American mineralogist,1982,67:877-885
32.Irvine TN.Crystallization sequences of the Muskox intrusion and other layered intrusion Ⅱ.Origin of chromitite layers and similar deposits of other magmatic ores[J].Geochimical et cosmchimica acta,1975,39:991-1020
33.Lambertt DD,Walker RJ,Morgan JW.Re-Os and Sm-Nd isotope geochemistry of the Stillwater Complex,montana:implications for the prteogenesis of the J-M Reef[J].Journal of petrology,1998,35:1717-1753
34.Naldrett AJ.Fedornko VA,Asif M et al.Controls on the compositions of Ni-Cu sulfide deposits as illustrated by those at Noril'sk,Siberia[J].Economic Geology,1996,91:751-773
35.Naldrett AJ.World-class Ni-Cu-PGE deposits:key factors in their genesis[J].Mineralium Deposita,1999,34:227-240
36.Reply EM.sulfur isotopic abundances of the Dunk Road Cu-Ni deposit Duluth complex Minnesota[J].Economic Geology,1981,76:619-620
37．张招崇，闫升好，陈柏林，何立新，何永胜，周刚．新疆喀拉通克基性杂岩体的地球化学特征及其对矿床成因的约束[J]．岩石矿物学杂志，2003，22(3)：217-224
38.Li C,Ripley EM.Empirical equations to predict the sulfur content of mafic magmas at sulfide saturation and applications to magmatic sulfide deposits[J].Mineralium Deposita 2005,40:218-230
39.Ghiorso MS,Sack RO.Chemical mass transfer in magmatic processes Ⅳ.A revised and internally consistent thermody-namic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures[J].Contrib Miner Petrol.1995,119:197-212
40．钱壮志，王建中，姜常义，焦建刚等．喀拉通克铜镍矿床铂族元素地球化学特征及其成矿作用意义[J]．岩石学报，2009，
41.Maier WD,Barnes S J,De Waal SA.Exploration for magmatic Ni-Cu-PGE sulphide deposits:Areview of recent advances in the use of geochemical tools,and their application to some south African ores[J].South African Geology,1998,101 (3):237-253
42.Courtillot V,Renne P.On the ages of flood basalt events[M].C.R.Geosci,2003,335:113-140
43.Alexander Y and Anatoly N.Noril'sk-Talnakh Cu-Ni-PGE deposits:a revised tectonic model[J].Mineralium Deposita,2004,39(2),125-142
44.RyanB.The Nain-Churehill Boundary and the Nain Plutonic suite:A rergional perspetive on the geologic setting of Voisey's Bay Ni-Cu-Co deposit[J].Eeon.Geol.,2000,95(4):703-724
45.Lambert DD,Frikc LR,Foster GJ et al.Re-Os isotopic systematics of the Voisey's Bay Ni-Cu-Co magmatic sulfide system,Labardor,Canada:Ⅱ Implications for paerental magma chemistry,ore genesis,and metal redistribution[J].Econ.Geol.,2000,867-888
46.Ripley EM,Li chuisi.Paragneiss assimilation in the genesis of magmatic Ni-Cu-Co sulfide mineralization at Voisey's Bay,Labardor:δ~(34)S、 δ~(13)C and Se/S evidence[J].Econ.Geol.,2002,97(6):867-888
47.Li C,Lightfoot PC,Amelin Y,et al.Contrasting petrological and geochemical relationships in the Voisey's Bay and Mushuau intrusions,Labrador:Implications for ore genesis[J].Economic Geology,2000a,95:771-800
48.Li C,Naldrett A J.Melting reactions of gneissic inclusions with enclosing magma at Voisey's Bay,Labrador,Canada:Implications with respect to ore genesis[J].Economic Geology,2000b,95:801-814
49．汤中立，李文渊．金川铜镍硫化物(含铂)矿床成床模式及地质对比[M]．北京：地质出版社，1995
50．汤中立．金川铜镍硫化矿床成矿模式[J]．现代地质，1990,4(4)：55-64
51．罗照华，马拉库舍夫，潘妮娅等．铜镍硫化物矿床的成因：以诺里尔斯克(俄罗斯)和金川(中国)为例[J]．矿床地质,2000,19(4)：330-339
52．解广轰，汪方亮，范彩云等．金川超镁铁岩侵入体及超大型硫化物矿床的成岩成矿机制[J]．中国科学(D辑)，1998,28：31-36
53．翟裕生等．区域成矿学[M]．1999．
54.Song XY,Zhou MF,Hou ZQ et al.Geochemical constraints on the mantle source of the Upper Permian Emeishan Continental Flood Basalts,Southwestern China[J].International Geology Review,2001,43:213-225
55.Zhou MF,Malpas J,Song XY,Robinson PT et al.A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction[J],Earth and Planetary Science Letters,2002,196 (3-4):113-122
56.Wang CY,Zhou MF,Keay RR.Geochemical constraints on the origin of the Permian Baimazhai mafic-ultramafic intrusion,SW China[J].Contribution to Minerlogy and Petrology,2006,152:309-321
57.Song XY,Zhou MF,Keays RR,Cao Z,Sun M,Qi L.Geochemistry of the Emeishan flood basalts at Yangliuping,Sichuan,SW China:implications for sulfide segregation[J].Contrib.Mineral.Petrol,2006,152:53-74
58.Song XY,Zhou MF,Tao Y,Xiao JF.Controls on the metal compositions of magrnatic sulfide deposits in the Emeishan large igneous province,SW China[J].Chemical Geology,2008,253:38-49
59．汤中立，钱壮志，姜常义等．中国超大型镍铜铂岩浆硫化物矿床预测[M]．北京：地质出版社．2006
60．汤中立．中国岩浆硫化物矿床的主要成矿机制[J]．地质学报，1996,36(3)：237-243
61.Keays RR.The role of komatiitic and picritic magmatism and S-saturation in the formation of the ore deposits[J].Lithos,1995.34:1-18
62.Chai G and Naldrett AJ.The Jinchuan uhramafic intrusion:cumulate of a high-Mg basaltic magma[J].Jour.Petrol.,1992,33:27-303.
63．徐章华，汤中立．金川铜镍(含PGE)岩浆硫化物矿床母岩浆成分的估计[J]．现代地质，1998，12(4)：225-229
64．姜常义，夏明哲，钱壮志，余旭等．新疆喀拉通克镁铁质岩体群的岩石成因及其对成矿过程的约束[J]．岩石学报,2009，
65.Amelie YLC,Valeyer O,Naldrett AJ.Nd-Sr-Pb isotope systematics of assimilation in the Voisey's Bay and Mushuan intrusions,Labrador,Canada[J].Economic Geology,2000,95:815-830
66.Horan MF,Walker RJ,Fedorenko VA et al.Os and Nd isotopic constrains on the temporal and spatial evolution of Siberian flood basalt sources[J].Geochim.Cosmochim.Acta.,2000,59:5159-5168
67.Czamenake GK,Wooden Jl,Walker RJ,et al.Geochemical,isotopic,and SHRIMP age data for Precambrian basement rocks,permain volcanic,and sedimentary host rocks to the ore-bearing intrusions,Noril'sk-talnakh district,Siberian Russian[J].International Geology Review,2000,42:895-927
68．张宗清，杜安道，唐索寒等．金川铜镍矿床年龄和源区同位素地球化学特征[J]．地质学报，2004，78(3)：359-365
69．刘民武．中国几个镍矿床的地球化学比较研究[D]．西北大学：博士论文,2003
70．李文渊，汤中立，郭周平等．阿拉善地块南缘镁铁超镁铁岩形成时代及地球化学特征[J]．岩石矿物学杂志，2004,23(2)：117-126
71.Thorpe RS,Francis PW,O' Callagham L.Relative role of source compositions,fractional crystallization and crustal contamination in the petrogenesis of Andean volcanic rocks[J].Philosophical Transactions of the Royal Society of London,1984,A310:675-692
72.Spera F J,Bohrson WA.Open-system magma chamber evolution:an energy-constrained geochemical model incorporating the effects of concurrent eruption,recharge,variable assimilation and fractional crystallization (Ec-E'RAxFC)[J].Journal of Petrology,2004,45(12):2459-2480
73．姜常义，夏明哲，余旭，逯东霞，魏巍，叶书锋．塔里木板块东北部柳园粗面玄武岩带：软流圈地幔减压熔融的产物．岩石学报．2007，23(7)：1777-1790
74．姜常义，张蓬勃，卢登蓉等．新疆塔里木板块西部瓦吉里塔格地区二叠纪超镁铁岩的岩石成因与岩浆源区[J]．岩石学报．2004，20(6)：1433-1444
75．姜常义，卢登蓉，白开寅，张蓬勃，叶书锋，冯金星，陈文革．大陆岩石圈地幔交代作用的产物—且干布拉克蛭石矿床[J]．岩石学报,2005,21(1)：201-210
76．姜常义，钱壮志，姜寒冰，唐冬梅，张蓬勃，朱士飞．云南宾川-永胜-丽江地区低钛玄武岩和苦橄岩的岩石成因与源区性质[J]．岩石学报,2007,23(4)：777-792
77.Foster JG,Lambert DD and Frick LR.1996.Re-Os isotopic evidencefor genesis of Archaean nickel ores from uncontaminated komatiites[J].Nature,382:703-706
78.Keays RR,Ihlenfed C,Mcinnes BIA et al.Re-Os isotope dating of the Jinchuan Ni-Cu-PGE,sulfide deposit,China[A].J.G.Shellnutt,M.F.Zhou and K.N.Pang.Recent advancees in magrnatic ore systems in mafic-ultramafic rocks[C].Hong kong SAR China:Proceedings of the IGCP 479 Hong Gong Workshop,Abstract Volume,2004,41-42
79．李文渊．Re-Os同位素体系及其在岩浆Cu-Ni-PGE矿床研究中的应用[J]．地球科学进展，1996．11(6)：580-584．
80.Mccandless TE,Ruiz J.Re-Os evidence for regional mineralization in North America[J].Scienee.1993,261:1282-1286
81.Walker RJ,Morgan JW,Horan MF et al.Re-Os isotopic evidence for an enriched-mantle plume source for the Noril'sk type ore-bearing intrusions,Siberia[J].Geoehim.Cosmoehim.Acta 1994,58:4179-4198
82．毛景文，杨建民，屈文俊等．新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J]．矿床地质，2002，21(4)：323-330．
83．李月臣，赵国春，屈文军等．新疆香山铜镍硫化物矿床Re-Os测定[J]．岩石学报．2006，22(1)：245-251
84．顾连兴，张遵忠，吴昌志等．关于东天山花岗岩与陆壳的垂向增长的若干认识．[J]．岩石学报．2006，22(5)：1103-1120
85．陈世平，王登红，屈文军等．新疆葫芦铜镍硫化物矿床的地质特征与成矿年代[J]．新疆地质．2005，23(3)：230-233
86．秦克章，方同辉，王书来，朱宝清等．2002．东天山板块构造分区、演化与成矿地质背景研究[J]． 新疆地质,20(4)：302-308．
87．毛启贵，肖文交，韩春明，孙敏等．2006．新疆东天山白石泉铜镍矿床基性-超基性岩体锆石U-Pb同位素年龄、地球化学特征及其对古亚洲洋闭合时限的制约[J]．岩石学报，22(1)：153-162．
88．吴华，李华芹，莫新华等．2005．新疆哈密白石泉铜镍矿区基性-超基性岩的形成时代及其地质意义[J]．地质学报，79(4)：498-502
89．姜常义，程松林，叶书峰，夏明哲，姜寒冰，代玉财．2006．新疆北山地区坡山北镁铁质岩石地球化学与岩石成因[J]．岩石学报，22：115-126
90.Pirajno F,Mao JW,Zhang ZC,Zhang ZH,Chai FM.2007.The association of mafic-ultramafic intrusions and A-type magmatism in the Tian Shan and Altay orogens,NW China:Implications for geodynamic evolution and potential for the discovery of new ore deposits[J].Journal of Asian Earth Sciences,doi:10.1016/j.jseaes.2007.10.012
91．王润民，刘德权，殷定泰．新疆哈密土墩-黄山一带铜镍硫化物矿床成矿控制条件及找矿方向的研究[J]．矿物岩石，1987,7(1)：1-152
92．方国庆．新疆东部大地构造特点及演化[J]．西北地质，1991，1-12
93．白云来．新疆哈密黄山-镜儿泉镍铜成矿系统的地质构造背景[J]．甘肃地质学报,2000,9(2)：1-7
94．白云来．新疆黄山地区蛇绿岩块的地质、地球化学特征及构造意义[J]．新疆地质，1993，11(1)：34-42
95．马瑞士，舒良树，孙家齐等．东天山构造演化与成矿[M]．北京：地质出版社，1997
96．刘德权，唐延龄，周汝洪．新疆北部古生代地壳演化及成矿系列[J]．矿床地质，1992，11(4)：307-314
97．胡受奚，郭继春，顾连兴等．加里东造山带在天山构造格架中的重要地位及其地质特征．新疆地质科学(第1辑)[M]．北京：地质出版社，1990
98．肖文交，韩春明，袁超等．新疆北部石炭纪-二叠纪独特的构造-成矿作用：对古亚洲洋构造域南部大地构造演化的制约[J]．岩石学报，2006，22(5)：1062-1076
99．何国琦，李茂松，刘德权等．中国新疆古生代地壳演化与成矿[M]．乌鲁木齐：新疆人民出版社，香港：香港文化教育出版社，1994
100．王登红，陈毓川，徐志刚等．新疆北部Cu-Ni-PGE硫化物矿床成矿系列探讨[J]．矿床地质,2000，19(2)：147-154．
101．毛景文，Pirajno F，张作衡等．天山-阿尔泰东部地区海西晚期后碰撞铜镍硫化物矿床：主要特点及可能与地幔柱的关系[J]．地质学报，2006，80(7)：925-945
102．王京彬，王玉往，周涛发．新疆北部后碰撞与幔源岩浆有关的成矿谱系[J]．岩石学报，2008，24(4)：743-752
103．傅学明，郭原生，刘凤山等．新疆黄山镁铁-超镁铁杂岩体矿物化学成分特征及与含矿(Ni)性关系[J]．兰州大学学报(自然科学版)，1993，29(4)：236-240
104．杨炳滨．新疆北部岩浆型铜镍硫化物矿床控矿因素的研究[J]．矿产与地质，1994,8：330-333
105．孙赫，秦克章，徐兴旺等．东天山镁铁质-超镁铁质岩带岩石特征及铜镍成矿作用[J]．矿床学，2007，26(1)：98-106
106.Campbell IH and Griffiths RW.The evolution of mantle's chemical structrure[J].1993.Lithos,30: 389-399
107.Pirajno F.Ore Deposits and Mantle Plumes[M].2000.Dordrecht:Kluwer Academic Publishers
108.Tuff,Takahashi E,Gibson SA.2005.Experimental constraints on the role of garnet pyroxenite in the genesis of high-Fe mantle plume derived melts[J].Journal of the Petrology,46(10):2023-2058
109.Altherr R,Henjes KF,Baumann A.Asthenosphere Versus lithosphere as possible sources for basaltic magmas erupted during formation of the Red Sea:constraints from Sr,Pb and Nd isotopes[J].Earth and planetary Science letters,1990,96:269-286
110.Fodor RV,Mukasa SB,Sial AN.Isotopic and trace-element indications of lithospheric and asthenospheric components in Tertiary alkalic basalts,northeastern Brazil.[J]Lithos,1998,43:197-217
111．韩宝福，季建清，宋彪，陈立辉，张磊．新疆准噶尔晚古生代陆壳垂直生长(Ⅰ)-后碰撞深成岩活动的时限[J]．岩石学报，2006，22(5)：1077-1086
112.Todt W,Cliff R A,Hanser A,Hofmann A W.Re-calibration of NBS lead standards using a 202Pb1205Pb double spike (abstract)[J].Terra Nova (Suppl.),1993,5:396
113．王赐银，朱文斌，马瑞士．东天山苦水变质岩带变质作用特征及其成因研究[J]．南京大学学报(自然科学版)，1992，28(4)：595-604
114．徐兴旺，秦克章，三金柱，王瑜等．东天山四顶黑山地区545Ma层状镁铁质-超镁铁质岩体的发现及其大地构造学和成矿学意义[J]．岩石学报，2006，22(11)：2665-2676
115．苏春乾，姜常义，夏明哲，张雷．新疆觉罗塔格构造带新元古代变质核杂岩锆石U-Pb年龄与地质意义[J]．岩石学报，2008，24(12)：2789-2879
116．陈文，孙枢，张彦等．新疆东天山秋格明塔什-黄山韧性剪切带~(40)Ar-~(39)Ar年代学研究[J]．地质学报，2005，79(6)：790-804
117．毛景文，李晓峰，李厚民等．中国造山带内生金属矿床类型、特点和成矿过成探讨[J]．地质学报，2005，79(3)：342-372
118．倪志耀．黄山东镁铁超镁铁杂岩中的辉石化学成分研究[J]．岩石矿物学杂志，1994，13(1)：55-66
119．倪志耀．新疆哈密黄山东镁铁-超镁铁杂岩体中橄榄石的化学成分及其岩石学意义[J]，1991，1(3)：40-47
120．顾连兴，诸建林，郭继春等．造山带环境中的东疆型镁铁-超镁铁杂岩[J]．岩石学报，1994，10(4)：339-356
121．柴凤梅．新疆北部三个与岩浆型Ni-Cu硫化物矿床有关的镁铁—超镁铁质岩的地球化学特征对比研究[D]．博士学位论文，2006，中国地质大学
122．韩春明，肖文交，崔彬等．新疆北部晚古生代铜矿床主要类型和地质特征[J]．地质学报，2006，80(1)：74-89
123．李华芹，谢才富，常海亮等．新疆北部有色贵金属矿床成矿作用年代学[M]．北京：地质出版社，1998
124．孟广路．新疆喀拉通克镁铁质岩体的岩石成因及成矿作用．硕士论文，2008，兰州大学
125.Naldrett AJ.Magrnatic Sulphie Deposits.New York:Oxford University Press.1989.1-186
126.Dick HJB,Natland JH.Late stage melt evolution and transport in the shallow mantle beneath the East Pacific Rise:Deep Sea Drilling Project[M].Initial Reports,1996,147:103-134
127．马润则，肖渊甫，魏显贵等．四川米苍山地区晋宁期基性超基性岩地球化学性质及其成因研究．矿物岩石[J]，1997，17(增刊)：35-47
128．姜常义，安三元．论火成岩中钙质角闪石的化学成分及其岩石学意义[J]．矿物岩石，1984，4(3)
129.Simkin T,Smith JV.Minor element distribution in olivine[J].Journal of Geology,1970,78:304-325
130.Morimoto N.Nomenclature of pyroxenes[J].Mineralogical Magazine,1988,52:535-550
131．张旗．镁铁-超镁铁岩与威尔逊旋回[J]．岩石学报，1992，8(2)：168-176
132.Miyashiro A.Volcanic rock series in island arcs and active continental margins[J].American Journal of Science,1974,274:321-355
133.Sun S S,McDonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantlecomposition and processes.In:Saunders A D and Norry M J(eds).Magmatism in the Ocean Basins[M].Geological Society.London:Special Publication,1989,42:313-345
134.Saunders AD,Norry M J,Tarney J.Origin of MORB and chemically depleted mantle reservoirs:trace element constraints.Pitrol,Special Litho-sphere Isse,1988.425-445
135.Zindler A,Hart SR.Chemical geodynamics:Annual Rev[J].Earth Planet.Sci.,1986.14:493-571
136.Staudigel H,Hart SR.Alteration of basaltic glass:mechanisms and significance for the oceanic crust seawater budget[J].Geochim.Cosmochim.Acta,1983,47:337-350
137.Gibson SA,Kirkpatrick RJ,Emmermann R et al.The trace element composition of lavas and dykes from 3 km vertical section through a lava pile in Eastern Iceland[J].J.Geophys.Res,1982.87:6532-6546
138.Pearce JA,Thirlwall MF,Ingram G et al.Isotopic evidence for the origin of Boninites and related rocks drilled in the Izu-Bonin (Ogasawara) forearc,Leg 125.In:Fryer P,Pearce J A,Stokking L.(Eds.),Proceedings ofthe Ocean Drilling Program[M].Scientific Results,1992,125,237-261
139.Mecdonald R,Rogers NW,Fitton JG et al.Plume-Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa[J].Journal of Petrology,2001,42:877-900
140.Barker JA,Menzies MA,Thirlwall MF,Macpherson CG.Petrogenesis of Quaternary intraplate volcanismSana'a Yenmen:Implication and polybaric melt hybridization[J].Journal of Petrology,1997,38:1359-1390
141.Hofmann W.Chemical differentiation of the earth:the relationship between mantle,continental crust,and oceanic crust[J].Earth and Planetary Science Letters,1986.90:297-314
142.Amelin YV,Neymark LA,Neymark LA et al.1996.Enriehed Nd-Sr-Pb Isotopic signatures in the Dovyren layered intrusion(estern Siberia,Russia):evidence for source contamination by ancient upper-crustal material[J].Chem.Geol,129:39-69
143.Ito E,White WM,Gopel C.The O,Sr,Nd and Pb isotope geochemistry of MORB[J].Chemical Geology,1987,62:157-176
144.Kyser TK,Carmeron WE,Nisbet EG.Boninite petrogenesis and alteration history;constraints from stable isotope compositions of boninites from Caoe Vogel,New Caledonia and Cyprus[J].Contributions to mineralogy and petrology,1982,93:222-226
145.Mattey D,Lowry D,Macpherson C.Oxygen isotope composition of mantle perdiotite[J].Earth and Planetary Science Letters,1994,128:23-241
146．沈渭洲．同位素地质学教程[M]．北京：原子能出版社，1997，237-2
147.Neal CR,Mahoney J J,Chazey WJ.Mantle sources and the highly variable role of continental lithosphere in basalt petrogenesis of the Kerguelen Plateau and Broken Ridge LIP:results from ODP Leg 183[J].Journal of petrology,2002,43:1177-1205
148．Rollison HR著，杨学明，杨晓勇，陈双喜翻译．岩石地球化学[M]．中国科技大学出版社，2000
149.Naldrett AJ.An overview of Ni-Cu mineralization with conclusions guide in exploration[M].Intemational Geological correlation program IGCP479 short course notes,2004,154-164
150.Roeder PL,Emslie RF.Olivine-liquid equilibrium[J].Contributions to Mineralogy and Petrology,1970.29:275-289
151.Green DH.Genesis of archean peridotic magmas and constraints on archean geothermal gradients and tectonics[J].Geology,1975,3:15-18
152.Frey FA,Green DH et al.Integrated models of basalt petrogenesis:A study of quarti tholeiites to olivine melilities from south eastern Australia utilizing geochemical and experimental petrological data[J].Journal of Petrology,1978,19:463-513
153.Hess PC.Phase equilibria constraints on the origin of ocean floor basalts.In:Morgan J P,Blackman D K & Sinton JM(eds).Mantle flow and Melt Generation at Mid-Ocean Ridges[M].Geophysical Monograph,American Geophysical Union,1992,71:67-102
154.Hawkesworth C J,Lightfoot P C,Fedorenko V A,Blake S et al.Magma differentiation and mineralization in the Siberian continental flood basalts[J].Lithos,1995,34:61-88
155.Stanley CR,Russell JK.Petrologic hypothesis testing with pearce element ration diagrams derivation of diagram axes[J].Contrib.Mineral.Petro.,1989,101:78-89
156.Wang KL,Chung SL,O'Reilly SY et al.Geochemical constraints for the genesis of post-collisional magrnatism and geodynamicevolution of the Northem Taiwan Region[J].Petrology,2004,45:975-1011.
157.Pearce JA,Bender JF,De Long SE et al.Genesis of collision volcanism in Eastern Anatolia,Turkey[J].J.Vol.Geo.Res.,1990,44,189-229.
158.Turner S,Sandiford M,Foden J.Some geodynamic and compositional constraints on “postorogenic” magmatism[J].Geology,1992,20:931-934
159.Wilson M.Igneous petrogenesis[M].London:Unwin Hyman.1989,1-466
160.Elliott T,Plank T,Zindler A et al.Elements transport from slab to volcanic front the Mariana arc[J].Journal of Geophysical Research,1997,102:14991-15019
161.Saunders AD,Storey M,Kent RW et al.1992.Consequences of plume-lithosphere interactions.In:Storey BC,Alabaster T,Pankhurst RJ (Eds.),Magmatism and the Cause of Continental Breakup[J].Geological Society of London Special Publication,68:41-60.
162.Woodhead JD,Hergt JM,Davidson JP et al.Hafnium isotope evidence for “conservative” element mobility during subduction zone processes[J].Earth and Planet Science Letters,2001,192:331-346.
163．赵振华，王强，熊小林，张海祥等．新疆北部的两类埃达克岩[J]．岩石学报，2006，22(5)：1249-65
164．吴昌志，张遵忠等．东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J]．岩石学报，2006，22(5)：1121-1134
165．朱永峰，王涛，徐新．新疆及邻区地质与矿产研究进展[J]．岩石学报，2007，23(8)：1785-94
166．朱永峰，郭璇，周晶．新疆中天山巴仑台地区晚石炭世+εNd辉长岩体的岩石学和同位素地球化学研究[J]．岩石学报，2006，22，1178-1192
167.Li CS,Maier WD,Waal SAD.The role of magma mixing in the genesis of PGE mineralisation in the Bushveld complex:thermodynamic calculation and new interpretations[J].Econ.Geol.,2001,96:653-662
166.Donaldson MJ.Redistribution of ore elements during serpentinizarion and tale-carbonate alteration ofsome Arehean dunites,Western Australia[J].Eeon.Geol.,1981,76:1698-1713
167.Henderson P.Rare earth element geochemistry[M].Amsterdam:Elsevier Science Publishers BV,1984,33-54
168.Wang K,Plant T et al.A mantle melting profile across the basin and range,SW USA[J].Journal of Geophysical Research,2002,107.10.1029/2001JB000209
169.Bird P.Continental delamination and the Colorado plateau[J].Joumal of Geophysical Research,1979,84(B13):7561-7571
170.Kimura JI,Manton WI,Sun CH,Iizumi S,Yoshida T,Stren R.Chemical diversity of the Ueno bsalts,central Japan:identification of mantle and crustal contributions to arcbasalts[J].Journal of Petrology,2002,43 (1):1923-1946
171.Rudnick RL,Fountain D M,Nature and composition of the continental crust:a lower crustal perspective[J].Rev.Geophys.,1995,33:267-309
172．张招崇，王福生．一种判别原始岩浆的方法-以苦橄岩和碱性玄武岩为例[J]．吉林大学学报，2003，33(2)：130-134
173.Sp(?)th A,Roex AP et al.2001.Plume-lithosphere interaction and the origin of continental rift-related alkaline volcanism,the Chyulu Hills Volcanic Province,Southern Kenya[J].Journal of Petrology,42:765-778
174.Rollinson HR.Using geochemical data:evaluation,presentation,interpretation[J].Longman Scientific and technical,NewYork,1993,1-352
175.Stolz A J,Jochum KP,Hofmann AW.Fluid-and melt-related enrichment in the subarc mantle;evidence from Nb/Ta variations in island-arc basats[J].Geology,1996,24:587-590
176.Taylor SR,Mclennan SM.1985.The continental crust:its composition and evolution.London:Blackwell Scientific Publications,1985.1-312
177．夏明哲，姜常义，钱壮志，孙涛，夏昭德，芦荣辉．新疆东天山葫芦岩体岩石地球化学特征研究[J]．岩石学报，2008，24(12)：2749-2760
178.Keppler H.Constraints from partitioning experiments on the composition of subduction zone fluids[J].Nature,1996,380:237-240
179.Green TH.1994.Experimental studies of trace element partitioning applicable to igneous petrogenesis Sedona 16 years later[J].Chemical Geology,117:1-36
180.Farmer GL,Perry FV,Semken S,Crowe B,et al.Isotopic evidence on the structure and origin of subcontin-ental lithospheric mantle in Southern Nevada[J].Journal of Geophysical Research,1989,94:7885-7898
181.Menzies A.Cratonic cirumcratonic and oceanic mantle domains beneath the western United States[J].Journal of geophysical research,1989,94:7899-7915
182.Saunders AD,Storey M,Kent RW,Norry MJ.Consequences of plumelithosphere interactions,in Storey BC,Alabaster T and Pankhurst R J,eds.,Magrnatism and the cause of continental breakup[M].London,Geological Society of Special Publication,1992.68:41-60
183.Davidson JP.Deciphering mantle and crustal signatures in subduction zone magmatism.Subduction top to bottom[M].Geophys.Monogr.,American Geophysical Union,Washington DC,1996.251-262
184.Anderson DL.Komatites and picrites:Evidence that “plume” source is depleted[J].Earth and Planetary Science Letters,1994.128:303-311
185．蒋寄云．新疆香山地区含铜镍矿化的镁铁-超镁铁岩研究[J]．矿物岩石地球化学通讯，1991，39(3)：189-191
186．丁玉学．新疆哈密香山铜镍矿床地质特征及成因探讨[J]．矿产地质系列丛书．1993，96-101
187．孙燕，慕纪录，肖渊甫．新疆香山铜镍硫化物矿床浅富矿体特征[J]．矿物岩石，1996，16(1)：51-57
188．秦全新．香山西段钛铁矿床地质特征及成因探讨[J]．矿产与地质，2003，17(4)：533-535
189．王玉往，王京彬，王莉娟等．新疆黄山地区铜镍硫化物矿床的稀土元素特征及意义[J]．岩石学报，2004，20(4)：935-948
190．王玉往，王京彬，王莉娟．东天山地区两类钒钛磁铁矿型矿床含矿岩石对比[J]．岩石学报，2006，22(5)：1425-1436
191．王玉往，王京彬，王莉娟等．．岩浆铜镍矿与钒钛磁铁矿的过渡类型—新疆哈密香山西矿床[J]．地质学报，2006，80(1)：61-73
192.Drake MJ.The oxidation state of europium as an indicatior of oxygen fugacity[J].Geochim.Cosmochim.Acta.,1975,9.55-64
193.Rudnick RL,McDonough WF,Chappell BW.Carbonatite metasomatism in the northern Tanzanian mantle:petrographic and geochemical characteristics[J].Earth Planet.Sci.Lett.,1993,114: 463-475 Hart SR,Gerlach DC,White WM.A possible new Sr-Nd-Pb mantle array and consequences for mantle mixing[J].Geochemica et Cosmochimica Acta,1986,50:1551-1557
194.Weaver BL.The origin of ocean island basalt end-member composition:trace element andisotopic constraints[J].Earth Planet.Sci.Lett.,1991,104:381-397
195.Milner SC,Le Roex A P.Isotope characteristics of the Okenyenya igneous complex,northwestern Namibia:constraints on the composition of the early Tristan plume and the origin of the EMI mantle component[J].Earth Planet.Sci.Lett.,1996,141:277-291
196.Carlson R W.Isotopic inferences on the chemical structure of the Mantle[J].Journal of Geodynamics,1995,20:365-386
198．李曙光，聂永红等．大别山俯冲陆壳的再循环-地球化学证据[J]．中国科学(D辑)，1997，27(5)：412-418
199.Chauvel C,Hofmann AW,Vidal P.HIMU-EM:The French Polynesian connetion[J].Earth Planet.Sci.Lett.,1992,110:99-119
200．赵磊．华北板块北缘中段晚古生代镁铁-超镁铁岩的岩石地球化学特征及其构造意义[D]．博士学位论文．2008．北京大学
201．潘小菲，刘伟．东天山香山镁铁-超镁铁岩中富含CH4流体包裹体的特征及意义[J]．岩石学报，2005，21(1)：211-218
202.Zhou MF,Robinson PT,and Lesher CM et al.,Geochemistry,petrogenesis,and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe-Ti-V-oxide deposits,Sichuan Province,SW China,Journal of Petrology[J],2005,46:2253-2280.
203.Pang KN,Li CS,Zhou MF,Ripley EM.2008.Abundant Fe-Ti oxide inclusion in olivine from the Panzhihua and Hongge layered intrusions,SW China:evidence for early saturation of Fe-Ti oxides in ferrobasaltic magma.Contrib Mineral Petrol,156:307-321
204．仲勇．二红洼镁铁-超镁铁杂岩体的特征及成因．新疆地质．1991，9(2)：150-170
205．仲勇．新疆二红洼基性-超基性杂岩体矿物、岩石化学及岩石学意义．中国地质科学院院报，1993，27-28：43-53
206.Johnson KTM.Experimental cpx/and garnet/melt partitioning of REE and other trace elements at high pressures; petrogenetic implications[J].Mineral.Mag.,1994,58:454-455
207.Riley TR,Leal PT,Curtis ML.Early-Middle Jurassic dolerite dykes from western Droning Maud Land(Antarctuca):identifying mantle source in the Karoo large igneous province[J].Journal of Petrology,2005,46(7):1489-152
208.Bmnan JM,Shaw HF,Ryerson FJ,Phinney DL.Mineral-aqueous fluid partitioning of trace elements at 900℃ and 2.0 GPa:constraints on the trace element chemistry of mantle an d deep crustal fluids[J].Geochimica et Cosmochimica Acta,1995,59:333 1-3350
209. Castillo PR and Newhall CG Geochemical Constraints on Possible Subduction Components in Lavas of Mayon and Taal Volcanoes. Southern Luzon, Philippines[J]. Journal of Petrology , 2004,45:1089-1108
210. Allegre CJ and Minster JF. Quangtitative method of trace element behavior in magmatic processes[J].Earth Planet Sci, 1978, 38:1-25
2.Kerr A.Nickeliferous gabbroic intrusions of the Pants Lake area,Labrador,Canada:implications for the development of magmatic sulfides in mafic systems[J].Am.J.Sci,2005,303:221-258
3.Meibom A,Sleep NH,Chamberlain CP et al.,Re-Os isotopic evidence for long-lived heterogeneity and equilibration processes in the Earth's upper mantle[J].Nature,2002,419:705-708.
4.Niu YL.Bulk-rock Major and Trace Element Compositions of Abyssal Peridotites:Implications for Mantle Melting,Melt Extraction and Post-melting Processes Beneath Mid-Ocean Ridges.Journal of Petrology,2004,45(12):2423-2458
5．金川公司信息中心．世界镍矿资源现状[R]．内部资料．2000
6．汤中立．中国的小岩体岩浆矿床[J]．中国工程科学，2002,4(6)：9-12．
7．毛景文，杨建民，屈文俊等．新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J]．矿床地质，2002，21(4)：323-330
8.Zhou MF,Leshen CM,Yang ZX et al.Geochemistry and petrogenesis of 270 Ma Ni-Cu-(PGE) sulfide-bearing mafic-ultramafic intrusions in Huangshan district,eastern Xinjiang,northwest China:implications for the tectonic evolution of the Central Asian orogenic belt[J].Chemical Geology,2004,209:233-257
9．韩宝福，季建清，宋彪等．新疆喀拉通克和黄山东含铜镍矿镁铁-超镁铁杂岩体的SHRIMP锆石U-Pb年龄及其地质意义[J]．科学通报，2004，49(22)：2324-2328
10.Zhang ZH,Mao JW,Du AD et al.Re-Os dating of two Cu-Ni sulfide deposits in northern Xinjiang,NW China and its geological significance[J].Journal of Asian Earth Sciences,2008,doi:10.1016/j.jseaes.2007.10.005
11．焦建刚．甘肃龙首山地区小岩体成大矿深部过程[D]．长安大学,2007,5
12.Naldrett AJ.IGCP.Projeet No.161 and a Proposed classification of Ni-Cu-PGE sulfide deposits[J].Canadian mineralogist,1979,17:143-145
13.Naldrett AJ.Niekel sulfides deposits:classification,composition,and genesis[J].Eeon.Geol.,1981,6:28-65
14.Naldrett AJ.Magma Sulfide Deposits Geology,Geochemistry And Exploration[M].Springer,2004,1-17
15.Ross JR,Travis GA.The niekel sulfide deposits in westem Australia in global Perspective[J].Economic Geology,1981,76(6):1291-1329
16．陈浩琉，吴水波，傅德彬等．镍矿床[M]．地质出版社，1993，22-57
17．汤中立．中国硫化镍矿床类型[J]．地质学报，1987,27(4)：350～369
18．汤中立S．J．Barnes，岩浆硫化物矿床成矿机制，北京：地质出版社，1998
19．汤中立，闫海卿，焦建刚等．中国岩浆硫化物矿床新分类与小岩体成矿作用[J]．矿床地质．2006．25(1)：1-8
20．汤中立．中国镁铁、超镁铁岩浆矿床成矿系列的聚集与演化[J]．地学前缘，2004，11(1)：113-119．
21.Naldrett A J,Duke JM,Lightfoot PC et al.Quantitative Modelling of the segregation of magrnatic sulfides:an exploration guide[J].Bull Can Inst Min Metall,1984,77:46-57
22.Naldrett AJ.Magmatic sulfide deposit[M]:New York,Oxford University Press,1989
23.Naldrett AJ.An overview of Ni-Cu mineralization with conclusions guide in exploration (Z).International Geological Correlation Programme 479 short course notes,2004,154-164
24.Lightfoot PC and Hawkesworth C J.Flood basalts and magmatic Ni,Cu and PGE sulphide mineralization:Comparative geochemistry of the Noril'sk (Siberian Trap) and West Greenland sequences[A].In:Mahoney JJ and Coffin MF,ed.Large igneous province[M].Washington D C:American Geophysical Union.1997.357-380.
25.Maclean WH.Liquid phase relations in the FeS-FeO-Fe2O3-SiO2 sysytems and their applications in geology[J].Economic Geology,1969,64:865-884
26.Shima H,Naldrett AJ.Solubility of sulfur in ultrmafic melt and the relevance of the system Fe-S-O[J].Economic Geology.1975,70:960-967
27.Holzheid A,Grove TL.Sulfur saturation limits in silicate melts and their implications for core formation scenarios for terrestrial planets[J].American Mineralogist,2002,87:227-237
28.Lorand J P.Are spinel iherzolite xenoliths representative of the sulfur content of the upper mantle[J].Geochim.Cosmochim.Acta,1990,54:1487-1492.
29.McDonough WF and Sun SS.The composition of the earth[J].Chem.Geol.,1995,120:233-253.
30.Keays RR.The role of komatiitic and picritic magrnatism and S saturation in the formation of ore deposits[J].Lithos,1995,34:1-18
31.Wendlandt RE Sulphide saturation of basalt and andesite melts at high pressures and temperature[J].American mineralogist,1982,67:877-885
32.Irvine TN.Crystallization sequences of the Muskox intrusion and other layered intrusion Ⅱ.Origin of chromitite layers and similar deposits of other magmatic ores[J].Geochimical et cosmchimica acta,1975,39:991-1020
33.Lambertt DD,Walker RJ,Morgan JW.Re-Os and Sm-Nd isotope geochemistry of the Stillwater Complex,montana:implications for the prteogenesis of the J-M Reef[J].Journal of petrology,1998,35:1717-1753
34.Naldrett AJ.Fedornko VA,Asif M et al.Controls on the compositions of Ni-Cu sulfide deposits as illustrated by those at Noril'sk,Siberia[J].Economic Geology,1996,91:751-773
35.Naldrett AJ.World-class Ni-Cu-PGE deposits:key factors in their genesis[J].Mineralium Deposita,1999,34:227-240
36.Reply EM.sulfur isotopic abundances of the Dunk Road Cu-Ni deposit Duluth complex Minnesota[J].Economic Geology,1981,76:619-620
37．张招崇，闫升好，陈柏林，何立新，何永胜，周刚．新疆喀拉通克基性杂岩体的地球化学特征及其对矿床成因的约束[J]．岩石矿物学杂志，2003，22(3)：217-224
38.Li C,Ripley EM.Empirical equations to predict the sulfur content of mafic magmas at sulfide saturation and applications to magmatic sulfide deposits[J].Mineralium Deposita 2005,40:218-230
39.Ghiorso MS,Sack RO.Chemical mass transfer in magmatic processes Ⅳ.A revised and internally consistent thermody-namic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures[J].Contrib Miner Petrol.1995,119:197-212
40．钱壮志，王建中，姜常义，焦建刚等．喀拉通克铜镍矿床铂族元素地球化学特征及其成矿作用意义[J]．岩石学报，2009，
41.Maier WD,Barnes S J,De Waal SA.Exploration for magmatic Ni-Cu-PGE sulphide deposits:Areview of recent advances in the use of geochemical tools,and their application to some south African ores[J].South African Geology,1998,101 (3):237-253
42.Courtillot V,Renne P.On the ages of flood basalt events[M].C.R.Geosci,2003,335:113-140
43.Alexander Y and Anatoly N.Noril'sk-Talnakh Cu-Ni-PGE deposits:a revised tectonic model[J].Mineralium Deposita,2004,39(2),125-142
44.RyanB.The Nain-Churehill Boundary and the Nain Plutonic suite:A rergional perspetive on the geologic setting of Voisey's Bay Ni-Cu-Co deposit[J].Eeon.Geol.,2000,95(4):703-724
45.Lambert DD,Frikc LR,Foster GJ et al.Re-Os isotopic systematics of the Voisey's Bay Ni-Cu-Co magmatic sulfide system,Labardor,Canada:Ⅱ Implications for paerental magma chemistry,ore genesis,and metal redistribution[J].Econ.Geol.,2000,867-888
46.Ripley EM,Li chuisi.Paragneiss assimilation in the genesis of magmatic Ni-Cu-Co sulfide mineralization at Voisey's Bay,Labardor:δ~(34)S、 δ~(13)C and Se/S evidence[J].Econ.Geol.,2002,97(6):867-888
47.Li C,Lightfoot PC,Amelin Y,et al.Contrasting petrological and geochemical relationships in the Voisey's Bay and Mushuau intrusions,Labrador:Implications for ore genesis[J].Economic Geology,2000a,95:771-800
48.Li C,Naldrett A J.Melting reactions of gneissic inclusions with enclosing magma at Voisey's Bay,Labrador,Canada:Implications with respect to ore genesis[J].Economic Geology,2000b,95:801-814
49．汤中立，李文渊．金川铜镍硫化物(含铂)矿床成床模式及地质对比[M]．北京：地质出版社，1995
50．汤中立．金川铜镍硫化矿床成矿模式[J]．现代地质，1990,4(4)：55-64
51．罗照华，马拉库舍夫，潘妮娅等．铜镍硫化物矿床的成因：以诺里尔斯克(俄罗斯)和金川(中国)为例[J]．矿床地质,2000,19(4)：330-339
52．解广轰，汪方亮，范彩云等．金川超镁铁岩侵入体及超大型硫化物矿床的成岩成矿机制[J]．中国科学(D辑)，1998,28：31-36
53．翟裕生等．区域成矿学[M]．1999．
54.Song XY,Zhou MF,Hou ZQ et al.Geochemical constraints on the mantle source of the Upper Permian Emeishan Continental Flood Basalts,Southwestern China[J].International Geology Review,2001,43:213-225
55.Zhou MF,Malpas J,Song XY,Robinson PT et al.A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction[J],Earth and Planetary Science Letters,2002,196 (3-4):113-122
56.Wang CY,Zhou MF,Keay RR.Geochemical constraints on the origin of the Permian Baimazhai mafic-ultramafic intrusion,SW China[J].Contribution to Minerlogy and Petrology,2006,152:309-321
57.Song XY,Zhou MF,Keays RR,Cao Z,Sun M,Qi L.Geochemistry of the Emeishan flood basalts at Yangliuping,Sichuan,SW China:implications for sulfide segregation[J].Contrib.Mineral.Petrol,2006,152:53-74
58.Song XY,Zhou MF,Tao Y,Xiao JF.Controls on the metal compositions of magrnatic sulfide deposits in the Emeishan large igneous province,SW China[J].Chemical Geology,2008,253:38-49
59．汤中立，钱壮志，姜常义等．中国超大型镍铜铂岩浆硫化物矿床预测[M]．北京：地质出版社．2006
60．汤中立．中国岩浆硫化物矿床的主要成矿机制[J]．地质学报，1996,36(3)：237-243
61.Keays RR.The role of komatiitic and picritic magmatism and S-saturation in the formation of the ore deposits[J].Lithos,1995.34:1-18
62.Chai G and Naldrett AJ.The Jinchuan uhramafic intrusion:cumulate of a high-Mg basaltic magma[J].Jour.Petrol.,1992,33:27-303.
63．徐章华，汤中立．金川铜镍(含PGE)岩浆硫化物矿床母岩浆成分的估计[J]．现代地质，1998，12(4)：225-229
64．姜常义，夏明哲，钱壮志，余旭等．新疆喀拉通克镁铁质岩体群的岩石成因及其对成矿过程的约束[J]．岩石学报,2009，
65.Amelie YLC,Valeyer O,Naldrett AJ.Nd-Sr-Pb isotope systematics of assimilation in the Voisey's Bay and Mushuan intrusions,Labrador,Canada[J].Economic Geology,2000,95:815-830
66.Horan MF,Walker RJ,Fedorenko VA et al.Os and Nd isotopic constrains on the temporal and spatial evolution of Siberian flood basalt sources[J].Geochim.Cosmochim.Acta.,2000,59:5159-5168
67.Czamenake GK,Wooden Jl,Walker RJ,et al.Geochemical,isotopic,and SHRIMP age data for Precambrian basement rocks,permain volcanic,and sedimentary host rocks to the ore-bearing intrusions,Noril'sk-talnakh district,Siberian Russian[J].International Geology Review,2000,42:895-927
68．张宗清，杜安道，唐索寒等．金川铜镍矿床年龄和源区同位素地球化学特征[J]．地质学报，2004，78(3)：359-365
69．刘民武．中国几个镍矿床的地球化学比较研究[D]．西北大学：博士论文,2003
70．李文渊，汤中立，郭周平等．阿拉善地块南缘镁铁超镁铁岩形成时代及地球化学特征[J]．岩石矿物学杂志，2004,23(2)：117-126
71.Thorpe RS,Francis PW,O' Callagham L.Relative role of source compositions,fractional crystallization and crustal contamination in the petrogenesis of Andean volcanic rocks[J].Philosophical Transactions of the Royal Society of London,1984,A310:675-692
72.Spera F J,Bohrson WA.Open-system magma chamber evolution:an energy-constrained geochemical model incorporating the effects of concurrent eruption,recharge,variable assimilation and fractional crystallization (Ec-E'RAxFC)[J].Journal of Petrology,2004,45(12):2459-2480
73．姜常义，夏明哲，余旭，逯东霞，魏巍，叶书锋．塔里木板块东北部柳园粗面玄武岩带：软流圈地幔减压熔融的产物．岩石学报．2007，23(7)：1777-1790
74．姜常义，张蓬勃，卢登蓉等．新疆塔里木板块西部瓦吉里塔格地区二叠纪超镁铁岩的岩石成因与岩浆源区[J]．岩石学报．2004，20(6)：1433-1444
75．姜常义，卢登蓉，白开寅，张蓬勃，叶书锋，冯金星，陈文革．大陆岩石圈地幔交代作用的产物—且干布拉克蛭石矿床[J]．岩石学报,2005,21(1)：201-210
76．姜常义，钱壮志，姜寒冰，唐冬梅，张蓬勃，朱士飞．云南宾川-永胜-丽江地区低钛玄武岩和苦橄岩的岩石成因与源区性质[J]．岩石学报,2007,23(4)：777-792
77.Foster JG,Lambert DD and Frick LR.1996.Re-Os isotopic evidencefor genesis of Archaean nickel ores from uncontaminated komatiites[J].Nature,382:703-706
78.Keays RR,Ihlenfed C,Mcinnes BIA et al.Re-Os isotope dating of the Jinchuan Ni-Cu-PGE,sulfide deposit,China[A].J.G.Shellnutt,M.F.Zhou and K.N.Pang.Recent advancees in magrnatic ore systems in mafic-ultramafic rocks[C].Hong kong SAR China:Proceedings of the IGCP 479 Hong Gong Workshop,Abstract Volume,2004,41-42
79．李文渊．Re-Os同位素体系及其在岩浆Cu-Ni-PGE矿床研究中的应用[J]．地球科学进展，1996．11(6)：580-584．
80.Mccandless TE,Ruiz J.Re-Os evidence for regional mineralization in North America[J].Scienee.1993,261:1282-1286
81.Walker RJ,Morgan JW,Horan MF et al.Re-Os isotopic evidence for an enriched-mantle plume source for the Noril'sk type ore-bearing intrusions,Siberia[J].Geoehim.Cosmoehim.Acta 1994,58:4179-4198
82．毛景文，杨建民，屈文俊等．新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J]．矿床地质，2002，21(4)：323-330．
83．李月臣，赵国春，屈文军等．新疆香山铜镍硫化物矿床Re-Os测定[J]．岩石学报．2006，22(1)：245-251
84．顾连兴，张遵忠，吴昌志等．关于东天山花岗岩与陆壳的垂向增长的若干认识．[J]．岩石学报．2006，22(5)：1103-1120
85．陈世平，王登红，屈文军等．新疆葫芦铜镍硫化物矿床的地质特征与成矿年代[J]．新疆地质．2005，23(3)：230-233
86．秦克章，方同辉，王书来，朱宝清等．2002．东天山板块构造分区、演化与成矿地质背景研究[J]． 新疆地质,20(4)：302-308．
87．毛启贵，肖文交，韩春明，孙敏等．2006．新疆东天山白石泉铜镍矿床基性-超基性岩体锆石U-Pb同位素年龄、地球化学特征及其对古亚洲洋闭合时限的制约[J]．岩石学报，22(1)：153-162．
88．吴华，李华芹，莫新华等．2005．新疆哈密白石泉铜镍矿区基性-超基性岩的形成时代及其地质意义[J]．地质学报，79(4)：498-502
89．姜常义，程松林，叶书峰，夏明哲，姜寒冰，代玉财．2006．新疆北山地区坡山北镁铁质岩石地球化学与岩石成因[J]．岩石学报，22：115-126
90.Pirajno F,Mao JW,Zhang ZC,Zhang ZH,Chai FM.2007.The association of mafic-ultramafic intrusions and A-type magmatism in the Tian Shan and Altay orogens,NW China:Implications for geodynamic evolution and potential for the discovery of new ore deposits[J].Journal of Asian Earth Sciences,doi:10.1016/j.jseaes.2007.10.012
91．王润民，刘德权，殷定泰．新疆哈密土墩-黄山一带铜镍硫化物矿床成矿控制条件及找矿方向的研究[J]．矿物岩石，1987,7(1)：1-152
92．方国庆．新疆东部大地构造特点及演化[J]．西北地质，1991，1-12
93．白云来．新疆哈密黄山-镜儿泉镍铜成矿系统的地质构造背景[J]．甘肃地质学报,2000,9(2)：1-7
94．白云来．新疆黄山地区蛇绿岩块的地质、地球化学特征及构造意义[J]．新疆地质，1993，11(1)：34-42
95．马瑞士，舒良树，孙家齐等．东天山构造演化与成矿[M]．北京：地质出版社，1997
96．刘德权，唐延龄，周汝洪．新疆北部古生代地壳演化及成矿系列[J]．矿床地质，1992，11(4)：307-314
97．胡受奚，郭继春，顾连兴等．加里东造山带在天山构造格架中的重要地位及其地质特征．新疆地质科学(第1辑)[M]．北京：地质出版社，1990
98．肖文交，韩春明，袁超等．新疆北部石炭纪-二叠纪独特的构造-成矿作用：对古亚洲洋构造域南部大地构造演化的制约[J]．岩石学报，2006，22(5)：1062-1076
99．何国琦，李茂松，刘德权等．中国新疆古生代地壳演化与成矿[M]．乌鲁木齐：新疆人民出版社，香港：香港文化教育出版社，1994
100．王登红，陈毓川，徐志刚等．新疆北部Cu-Ni-PGE硫化物矿床成矿系列探讨[J]．矿床地质,2000，19(2)：147-154．
101．毛景文，Pirajno F，张作衡等．天山-阿尔泰东部地区海西晚期后碰撞铜镍硫化物矿床：主要特点及可能与地幔柱的关系[J]．地质学报，2006，80(7)：925-945
102．王京彬，王玉往，周涛发．新疆北部后碰撞与幔源岩浆有关的成矿谱系[J]．岩石学报，2008，24(4)：743-752
103．傅学明，郭原生，刘凤山等．新疆黄山镁铁-超镁铁杂岩体矿物化学成分特征及与含矿(Ni)性关系[J]．兰州大学学报(自然科学版)，1993，29(4)：236-240
104．杨炳滨．新疆北部岩浆型铜镍硫化物矿床控矿因素的研究[J]．矿产与地质，1994,8：330-333
105．孙赫，秦克章，徐兴旺等．东天山镁铁质-超镁铁质岩带岩石特征及铜镍成矿作用[J]．矿床学，2007，26(1)：98-106
106.Campbell IH and Griffiths RW.The evolution of mantle's chemical structrure[J].1993.Lithos,30: 389-399
107.Pirajno F.Ore Deposits and Mantle Plumes[M].2000.Dordrecht:Kluwer Academic Publishers
108.Tuff,Takahashi E,Gibson SA.2005.Experimental constraints on the role of garnet pyroxenite in the genesis of high-Fe mantle plume derived melts[J].Journal of the Petrology,46(10):2023-2058
109.Altherr R,Henjes KF,Baumann A.Asthenosphere Versus lithosphere as possible sources for basaltic magmas erupted during formation of the Red Sea:constraints from Sr,Pb and Nd isotopes[J].Earth and planetary Science letters,1990,96:269-286
110.Fodor RV,Mukasa SB,Sial AN.Isotopic and trace-element indications of lithospheric and asthenospheric components in Tertiary alkalic basalts,northeastern Brazil.[J]Lithos,1998,43:197-217
111．韩宝福，季建清，宋彪，陈立辉，张磊．新疆准噶尔晚古生代陆壳垂直生长(Ⅰ)-后碰撞深成岩活动的时限[J]．岩石学报，2006，22(5)：1077-1086
112.Todt W,Cliff R A,Hanser A,Hofmann A W.Re-calibration of NBS lead standards using a 202Pb1205Pb double spike (abstract)[J].Terra Nova (Suppl.),1993,5:396
113．王赐银，朱文斌，马瑞士．东天山苦水变质岩带变质作用特征及其成因研究[J]．南京大学学报(自然科学版)，1992，28(4)：595-604
114．徐兴旺，秦克章，三金柱，王瑜等．东天山四顶黑山地区545Ma层状镁铁质-超镁铁质岩体的发现及其大地构造学和成矿学意义[J]．岩石学报，2006，22(11)：2665-2676
115．苏春乾，姜常义，夏明哲，张雷．新疆觉罗塔格构造带新元古代变质核杂岩锆石U-Pb年龄与地质意义[J]．岩石学报，2008，24(12)：2789-2879
116．陈文，孙枢，张彦等．新疆东天山秋格明塔什-黄山韧性剪切带~(40)Ar-~(39)Ar年代学研究[J]．地质学报，2005，79(6)：790-804
117．毛景文，李晓峰，李厚民等．中国造山带内生金属矿床类型、特点和成矿过成探讨[J]．地质学报，2005，79(3)：342-372
118．倪志耀．黄山东镁铁超镁铁杂岩中的辉石化学成分研究[J]．岩石矿物学杂志，1994，13(1)：55-66
119．倪志耀．新疆哈密黄山东镁铁-超镁铁杂岩体中橄榄石的化学成分及其岩石学意义[J]，1991，1(3)：40-47
120．顾连兴，诸建林，郭继春等．造山带环境中的东疆型镁铁-超镁铁杂岩[J]．岩石学报，1994，10(4)：339-356
121．柴凤梅．新疆北部三个与岩浆型Ni-Cu硫化物矿床有关的镁铁—超镁铁质岩的地球化学特征对比研究[D]．博士学位论文，2006，中国地质大学
122．韩春明，肖文交，崔彬等．新疆北部晚古生代铜矿床主要类型和地质特征[J]．地质学报，2006，80(1)：74-89
123．李华芹，谢才富，常海亮等．新疆北部有色贵金属矿床成矿作用年代学[M]．北京：地质出版社，1998
124．孟广路．新疆喀拉通克镁铁质岩体的岩石成因及成矿作用．硕士论文，2008，兰州大学
125.Naldrett AJ.Magrnatic Sulphie Deposits.New York:Oxford University Press.1989.1-186
126.Dick HJB,Natland JH.Late stage melt evolution and transport in the shallow mantle beneath the East Pacific Rise:Deep Sea Drilling Project[M].Initial Reports,1996,147:103-134
127．马润则，肖渊甫，魏显贵等．四川米苍山地区晋宁期基性超基性岩地球化学性质及其成因研究．矿物岩石[J]，1997，17(增刊)：35-47
128．姜常义，安三元．论火成岩中钙质角闪石的化学成分及其岩石学意义[J]．矿物岩石，1984，4(3)
129.Simkin T,Smith JV.Minor element distribution in olivine[J].Journal of Geology,1970,78:304-325
130.Morimoto N.Nomenclature of pyroxenes[J].Mineralogical Magazine,1988,52:535-550
131．张旗．镁铁-超镁铁岩与威尔逊旋回[J]．岩石学报，1992，8(2)：168-176
132.Miyashiro A.Volcanic rock series in island arcs and active continental margins[J].American Journal of Science,1974,274:321-355
133.Sun S S,McDonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantlecomposition and processes.In:Saunders A D and Norry M J(eds).Magmatism in the Ocean Basins[M].Geological Society.London:Special Publication,1989,42:313-345
134.Saunders AD,Norry M J,Tarney J.Origin of MORB and chemically depleted mantle reservoirs:trace element constraints.Pitrol,Special Litho-sphere Isse,1988.425-445
135.Zindler A,Hart SR.Chemical geodynamics:Annual Rev[J].Earth Planet.Sci.,1986.14:493-571
136.Staudigel H,Hart SR.Alteration of basaltic glass:mechanisms and significance for the oceanic crust seawater budget[J].Geochim.Cosmochim.Acta,1983,47:337-350
137.Gibson SA,Kirkpatrick RJ,Emmermann R et al.The trace element composition of lavas and dykes from 3 km vertical section through a lava pile in Eastern Iceland[J].J.Geophys.Res,1982.87:6532-6546
138.Pearce JA,Thirlwall MF,Ingram G et al.Isotopic evidence for the origin of Boninites and related rocks drilled in the Izu-Bonin (Ogasawara) forearc,Leg 125.In:Fryer P,Pearce J A,Stokking L.(Eds.),Proceedings ofthe Ocean Drilling Program[M].Scientific Results,1992,125,237-261
139.Mecdonald R,Rogers NW,Fitton JG et al.Plume-Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa[J].Journal of Petrology,2001,42:877-900
140.Barker JA,Menzies MA,Thirlwall MF,Macpherson CG.Petrogenesis of Quaternary intraplate volcanismSana'a Yenmen:Implication and polybaric melt hybridization[J].Journal of Petrology,1997,38:1359-1390
141.Hofmann W.Chemical differentiation of the earth:the relationship between mantle,continental crust,and oceanic crust[J].Earth and Planetary Science Letters,1986.90:297-314
142.Amelin YV,Neymark LA,Neymark LA et al.1996.Enriehed Nd-Sr-Pb Isotopic signatures in the Dovyren layered intrusion(estern Siberia,Russia):evidence for source contamination by ancient upper-crustal material[J].Chem.Geol,129:39-69
143.Ito E,White WM,Gopel C.The O,Sr,Nd and Pb isotope geochemistry of MORB[J].Chemical Geology,1987,62:157-176
144.Kyser TK,Carmeron WE,Nisbet EG.Boninite petrogenesis and alteration history;constraints from stable isotope compositions of boninites from Caoe Vogel,New Caledonia and Cyprus[J].Contributions to mineralogy and petrology,1982,93:222-226
145.Mattey D,Lowry D,Macpherson C.Oxygen isotope composition of mantle perdiotite[J].Earth and Planetary Science Letters,1994,128:23-241
146．沈渭洲．同位素地质学教程[M]．北京：原子能出版社，1997，237-2
147.Neal CR,Mahoney J J,Chazey WJ.Mantle sources and the highly variable role of continental lithosphere in basalt petrogenesis of the Kerguelen Plateau and Broken Ridge LIP:results from ODP Leg 183[J].Journal of petrology,2002,43:1177-1205
148．Rollison HR著，杨学明，杨晓勇，陈双喜翻译．岩石地球化学[M]．中国科技大学出版社，2000
149.Naldrett AJ.An overview of Ni-Cu mineralization with conclusions guide in exploration[M].Intemational Geological correlation program IGCP479 short course notes,2004,154-164
150.Roeder PL,Emslie RF.Olivine-liquid equilibrium[J].Contributions to Mineralogy and Petrology,1970.29:275-289
151.Green DH.Genesis of archean peridotic magmas and constraints on archean geothermal gradients and tectonics[J].Geology,1975,3:15-18
152.Frey FA,Green DH et al.Integrated models of basalt petrogenesis:A study of quarti tholeiites to olivine melilities from south eastern Australia utilizing geochemical and experimental petrological data[J].Journal of Petrology,1978,19:463-513
153.Hess PC.Phase equilibria constraints on the origin of ocean floor basalts.In:Morgan J P,Blackman D K & Sinton JM(eds).Mantle flow and Melt Generation at Mid-Ocean Ridges[M].Geophysical Monograph,American Geophysical Union,1992,71:67-102
154.Hawkesworth C J,Lightfoot P C,Fedorenko V A,Blake S et al.Magma differentiation and mineralization in the Siberian continental flood basalts[J].Lithos,1995,34:61-88
155.Stanley CR,Russell JK.Petrologic hypothesis testing with pearce element ration diagrams derivation of diagram axes[J].Contrib.Mineral.Petro.,1989,101:78-89
156.Wang KL,Chung SL,O'Reilly SY et al.Geochemical constraints for the genesis of post-collisional magrnatism and geodynamicevolution of the Northem Taiwan Region[J].Petrology,2004,45:975-1011.
157.Pearce JA,Bender JF,De Long SE et al.Genesis of collision volcanism in Eastern Anatolia,Turkey[J].J.Vol.Geo.Res.,1990,44,189-229.
158.Turner S,Sandiford M,Foden J.Some geodynamic and compositional constraints on “postorogenic” magmatism[J].Geology,1992,20:931-934
159.Wilson M.Igneous petrogenesis[M].London:Unwin Hyman.1989,1-466
160.Elliott T,Plank T,Zindler A et al.Elements transport from slab to volcanic front the Mariana arc[J].Journal of Geophysical Research,1997,102:14991-15019
161.Saunders AD,Storey M,Kent RW et al.1992.Consequences of plume-lithosphere interactions.In:Storey BC,Alabaster T,Pankhurst RJ (Eds.),Magmatism and the Cause of Continental Breakup[J].Geological Society of London Special Publication,68:41-60.
162.Woodhead JD,Hergt JM,Davidson JP et al.Hafnium isotope evidence for “conservative” element mobility during subduction zone processes[J].Earth and Planet Science Letters,2001,192:331-346.
163．赵振华，王强，熊小林，张海祥等．新疆北部的两类埃达克岩[J]．岩石学报，2006，22(5)：1249-65
164．吴昌志，张遵忠等．东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J]．岩石学报，2006，22(5)：1121-1134
165．朱永峰，王涛，徐新．新疆及邻区地质与矿产研究进展[J]．岩石学报，2007，23(8)：1785-94
166．朱永峰，郭璇，周晶．新疆中天山巴仑台地区晚石炭世+εNd辉长岩体的岩石学和同位素地球化学研究[J]．岩石学报，2006，22，1178-1192
167.Li CS,Maier WD,Waal SAD.The role of magma mixing in the genesis of PGE mineralisation in the Bushveld complex:thermodynamic calculation and new interpretations[J].Econ.Geol.,2001,96:653-662
166.Donaldson MJ.Redistribution of ore elements during serpentinizarion and tale-carbonate alteration ofsome Arehean dunites,Western Australia[J].Eeon.Geol.,1981,76:1698-1713
167.Henderson P.Rare earth element geochemistry[M].Amsterdam:Elsevier Science Publishers BV,1984,33-54
168.Wang K,Plant T et al.A mantle melting profile across the basin and range,SW USA[J].Journal of Geophysical Research,2002,107.10.1029/2001JB000209
169.Bird P.Continental delamination and the Colorado plateau[J].Joumal of Geophysical Research,1979,84(B13):7561-7571
170.Kimura JI,Manton WI,Sun CH,Iizumi S,Yoshida T,Stren R.Chemical diversity of the Ueno bsalts,central Japan:identification of mantle and crustal contributions to arcbasalts[J].Journal of Petrology,2002,43 (1):1923-1946
171.Rudnick RL,Fountain D M,Nature and composition of the continental crust:a lower crustal perspective[J].Rev.Geophys.,1995,33:267-309
172．张招崇，王福生．一种判别原始岩浆的方法-以苦橄岩和碱性玄武岩为例[J]．吉林大学学报，2003，33(2)：130-134
173.Sp(?)th A,Roex AP et al.2001.Plume-lithosphere interaction and the origin of continental rift-related alkaline volcanism,the Chyulu Hills Volcanic Province,Southern Kenya[J].Journal of Petrology,42:765-778
174.Rollinson HR.Using geochemical data:evaluation,presentation,interpretation[J].Longman Scientific and technical,NewYork,1993,1-352
175.Stolz A J,Jochum KP,Hofmann AW.Fluid-and melt-related enrichment in the subarc mantle;evidence from Nb/Ta variations in island-arc basats[J].Geology,1996,24:587-590
176.Taylor SR,Mclennan SM.1985.The continental crust:its composition and evolution.London:Blackwell Scientific Publications,1985.1-312
177．夏明哲，姜常义，钱壮志，孙涛，夏昭德，芦荣辉．新疆东天山葫芦岩体岩石地球化学特征研究[J]．岩石学报，2008，24(12)：2749-2760
178.Keppler H.Constraints from partitioning experiments on the composition of subduction zone fluids[J].Nature,1996,380:237-240
179.Green TH.1994.Experimental studies of trace element partitioning applicable to igneous petrogenesis Sedona 16 years later[J].Chemical Geology,117:1-36
180.Farmer GL,Perry FV,Semken S,Crowe B,et al.Isotopic evidence on the structure and origin of subcontin-ental lithospheric mantle in Southern Nevada[J].Journal of Geophysical Research,1989,94:7885-7898
181.Menzies A.Cratonic cirumcratonic and oceanic mantle domains beneath the western United States[J].Journal of geophysical research,1989,94:7899-7915
182.Saunders AD,Storey M,Kent RW,Norry MJ.Consequences of plumelithosphere interactions,in Storey BC,Alabaster T and Pankhurst R J,eds.,Magrnatism and the cause of continental breakup[M].London,Geological Society of Special Publication,1992.68:41-60
183.Davidson JP.Deciphering mantle and crustal signatures in subduction zone magmatism.Subduction top to bottom[M].Geophys.Monogr.,American Geophysical Union,Washington DC,1996.251-262
184.Anderson DL.Komatites and picrites:Evidence that “plume” source is depleted[J].Earth and Planetary Science Letters,1994.128:303-311
185．蒋寄云．新疆香山地区含铜镍矿化的镁铁-超镁铁岩研究[J]．矿物岩石地球化学通讯，1991，39(3)：189-191
186．丁玉学．新疆哈密香山铜镍矿床地质特征及成因探讨[J]．矿产地质系列丛书．1993，96-101
187．孙燕，慕纪录，肖渊甫．新疆香山铜镍硫化物矿床浅富矿体特征[J]．矿物岩石，1996，16(1)：51-57
188．秦全新．香山西段钛铁矿床地质特征及成因探讨[J]．矿产与地质，2003，17(4)：533-535
189．王玉往，王京彬，王莉娟等．新疆黄山地区铜镍硫化物矿床的稀土元素特征及意义[J]．岩石学报，2004，20(4)：935-948
190．王玉往，王京彬，王莉娟．东天山地区两类钒钛磁铁矿型矿床含矿岩石对比[J]．岩石学报，2006，22(5)：1425-1436
191．王玉往，王京彬，王莉娟等．．岩浆铜镍矿与钒钛磁铁矿的过渡类型—新疆哈密香山西矿床[J]．地质学报，2006，80(1)：61-73
192.Drake MJ.The oxidation state of europium as an indicatior of oxygen fugacity[J].Geochim.Cosmochim.Acta.,1975,9.55-64
193.Rudnick RL,McDonough WF,Chappell BW.Carbonatite metasomatism in the northern Tanzanian mantle:petrographic and geochemical characteristics[J].Earth Planet.Sci.Lett.,1993,114: 463-475 Hart SR,Gerlach DC,White WM.A possible new Sr-Nd-Pb mantle array and consequences for mantle mixing[J].Geochemica et Cosmochimica Acta,1986,50:1551-1557
194.Weaver BL.The origin of ocean island basalt end-member composition:trace element andisotopic constraints[J].Earth Planet.Sci.Lett.,1991,104:381-397
195.Milner SC,Le Roex A P.Isotope characteristics of the Okenyenya igneous complex,northwestern Namibia:constraints on the composition of the early Tristan plume and the origin of the EMI mantle component[J].Earth Planet.Sci.Lett.,1996,141:277-291
196.Carlson R W.Isotopic inferences on the chemical structure of the Mantle[J].Journal of Geodynamics,1995,20:365-386
198．李曙光，聂永红等．大别山俯冲陆壳的再循环-地球化学证据[J]．中国科学(D辑)，1997，27(5)：412-418
199.Chauvel C,Hofmann AW,Vidal P.HIMU-EM:The French Polynesian connetion[J].Earth Planet.Sci.Lett.,1992,110:99-119
200．赵磊．华北板块北缘中段晚古生代镁铁-超镁铁岩的岩石地球化学特征及其构造意义[D]．博士学位论文．2008．北京大学
201．潘小菲，刘伟．东天山香山镁铁-超镁铁岩中富含CH4流体包裹体的特征及意义[J]．岩石学报，2005，21(1)：211-218
202.Zhou MF,Robinson PT,and Lesher CM et al.,Geochemistry,petrogenesis,and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe-Ti-V-oxide deposits,Sichuan Province,SW China,Journal of Petrology[J],2005,46:2253-2280.
203.Pang KN,Li CS,Zhou MF,Ripley EM.2008.Abundant Fe-Ti oxide inclusion in olivine from the Panzhihua and Hongge layered intrusions,SW China:evidence for early saturation of Fe-Ti oxides in ferrobasaltic magma.Contrib Mineral Petrol,156:307-321
204．仲勇．二红洼镁铁-超镁铁杂岩体的特征及成因．新疆地质．1991，9(2)：150-170
205．仲勇．新疆二红洼基性-超基性杂岩体矿物、岩石化学及岩石学意义．中国地质科学院院报，1993，27-28：43-53
206.Johnson KTM.Experimental cpx/and garnet/melt partitioning of REE and other trace elements at high pressures; petrogenetic implications[J].Mineral.Mag.,1994,58:454-455
207.Riley TR,Leal PT,Curtis ML.Early-Middle Jurassic dolerite dykes from western Droning Maud Land(Antarctuca):identifying mantle source in the Karoo large igneous province[J].Journal of Petrology,2005,46(7):1489-152
208.Bmnan JM,Shaw HF,Ryerson FJ,Phinney DL.Mineral-aqueous fluid partitioning of trace elements at 900℃ and 2.0 GPa:constraints on the trace element chemistry of mantle an d deep crustal fluids[J].Geochimica et Cosmochimica Acta,1995,59:333 1-3350
209. Castillo PR and Newhall CG Geochemical Constraints on Possible Subduction Components in Lavas of Mayon and Taal Volcanoes. Southern Luzon, Philippines[J]. Journal of Petrology , 2004,45:1089-1108
210. Allegre CJ and Minster JF. Quangtitative method of trace element behavior in magmatic processes[J].Earth Planet Sci, 1978, 38:1-25
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |