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
|
摘要
近年来,随着全球对镍需求量的不断增加,与岩浆型Ni-Cu-(PGE)硫化物矿床有关的镁铁-超镁铁质岩体的研究得到了重视。同时,镁铁-超镁铁质岩石对于研究壳幔相互作用、地球深部动力过程等具有重要的意义。
新疆北部是我国,也是全球岩浆型Ni-Cu-(PGE)硫化物矿床分布最密集的地区之一,该区位于中亚造山带南部边缘。研究这些与岩浆型Ni-Cu-(PGE)硫化物矿床有关的镁铁-超镁铁质岩体的成因,对造山带内的岩浆型Ni-Cu-(PGE)硫化物矿床的找矿勘查活动以及研究中亚造山带的形成和演化具有重要的意义。前人对这些岩体的成因研究较为薄弱。本文选择位于不同构造单元的白石泉(中天山)、黄山东(东天山)和喀拉通克(阿尔泰山南缘)镁铁-超镁铁质岩体进行系统的岩石学和地球化学研究,探讨三个典型岩体的岩石成因,以期为研究区的岩浆型Ni-Cu-(PGE)硫化物矿床的找矿提供线索,同时为后造山作用过程提供约束条件。目前取得的主要认识有:
1.白石泉、喀拉通克、黄山东镁铁-超镁铁质侵入体是造山后碰撞阶段岩浆活动的产物,它们具有相同的地球动力学背景。
2.三个岩体的岩石组合及含矿岩石类型不同,但造岩矿物特征大体相同。白石泉岩体与黄山东岩体包括超镁铁质与镁铁质岩石,而喀拉通克岩体缺乏超镁铁质岩石。前两个岩体的主要含矿岩石为橄榄岩与辉石岩,喀拉通克岩体主要为苏长岩含矿。
3.三个岩体均具有大离子亲石元素(LILE)和轻稀土元素(LREE)富集,高场强元素(HFSE)亏损的微量元素特征。均具有低的Sr同位素初始比值,正的εNd值和低的放射性成因Pb,高于地幔的O同位素特征。白石泉岩体与黄山东岩体均具有极低的铂族元素成分,并且铂族元素主要受结晶分异作用的影响。
4.三个岩体的母岩浆性质相似,均为含有水的高镁拉斑玄武岩。但是它们的母岩浆中MgO的含量有别。
5.三个岩体的源区相似,岩浆的演化特征相近。它们的源区均为受到俯冲洋壳物质混染的软流圈地幔。它们的原始岩浆均经过了两个阶段的演化。第一阶段为橄榄石的结晶与硫化物的熔离阶段,第二个阶段为富含橄榄石与硫化物“晶粥”的就地分异阶段。地壳物质混染和橄榄石的结晶是岩浆中S饱和的主控因素。关键词:岩浆型Ni-Cu-(PGE)硫化物,镁铁-超镁铁岩,地球化学,新疆北部
Recently, the increased demand of Cu, Ni, Pt and Pd, etc., greatly promotes the research onthese mafic-ultramafic rocks associated with magmatic Ni-Cu-(PGE) sulfide deposits.Furthermore, the mafic-ultramafic rocks can be an important object to understand crust-mantlemagmatism and the process of continental geodynamics.
In the past twenty years about 20 magmatic Ni-Cu-(PGE) sulfide deposits and occurrenceshave been discovered in northern Xinjiang, China. These Ni-Cu-(PGE) sulfide deposits, relatedto mafic-ultramafic intrusions, are one component of the large scale metallogenesis duringpost-collisional tectonism in Late Carboniferous–Early Permian within the Central AsianOrogenic belt. To understand the origin of these Ni-Cu-(PGE)-bearing mafic-ultramaficintrusions is potentially important not only to the guidence exploration on Ni-Cu-(PGE) sulfidedeposits in orogenic belt but also to the study on the evolution of the CAOB. However, theprevious studies were focused on these Ni-Cu-(PGE) deposits, with little attention to the originand evolution of these mafic-ultramafic intrusions. Thus, three intrusions, including Baishiquanintrusions in Central-Tianshan Block, Huangshandong intrusions in Jueluotage orogenic beltand Kalatongke intrusions in Altay orogenic belts, are chosen for objects in this dissertation.The characteristics of petrology, mineralogy and geochemistry on these intrusions areinvestigated for the purpose as follow: (1) to determine the petrogenesis and evolution of theserocks;(2) to provide some clues for Ni-Cu-(PGE) sulfide ore genesis;(3) to discuss the mantlesource regions to understand the geodynamic processes;(4) to compare these characteristicsand find the reasons of similarities and differences, to discuss the regularities of formation forthe magmatic Ni-Cu-(PGE) sulfide deposits in orogenic belt. (5) to provide some constraints forthe process of post-collisional tectonism.
On the basis of the systematically research on three mafic-ultramafic intrusions hostingNi-Cu-(PGE) sulfide deposits in the CAOB, some conclusion has been drawn:
(1) The Baishiquan, Huangshandong and Kalatongke mafic-ultramafic intrusions occurredin the postcollisional setting and were related to lithospheric delamination and magmatic
underplating.(2) These intrusions have different rock assemblages and host rocks for Ni-Cu deposits,although the petrogenetic minerals are same. The Baishiquan and Huangshandong intrusionsare composed of peridotite, pyroxenite, hornblendite, troctolite, norite, gabbro and diorite, andthe Kalatongke intrusions consist of norite, gabbro-norite and biotite diorite. The peridotite andpyroxenite are the main host rocks for the Cu-Ni ores in the Baishiquan and Huangshandongintrusion, while norite in Kalatongke intrusion.(3) All of the intrusions are characterized by enrichment in large ion lithophile elements(LILE, e.g., Rb, Sr, K, U, Pb and Th) and light rare earth elements (LREE), depletion in highfield strength elements (HFSE, e.g., Nb, Ta, Ti and P) in relative to primitive mantle andMORB. Their Sr, Nd, Pb and O isotope data suggest a mixture of depleted asthenosphericmantle with MORB-like isotopic signature and subducted slab with EMⅡisotopic signature.The absolute PGE abundances are low, and the PGE is mainly affected by crystallizationdifferentiation in the Baishiquan and huangshandong intrusions.(4) The parental magmas are high-magnesium tholeiite, but have different contents in MgO.(5) The primitive magmas are derived from the asthenospheric mantle contaminated bypreviously subduction material. The primary magma with high-magnesium componentsexperienced two stages evolution. Olivine is the main fractionated phase in first stage of magmaevolution, and sulfides segregated from the silicate magma. The parental magma, which isolivine-and sulfide-laden crystal mush, entered the high-level magma chamber anddifferentiated in situ to form these intrusions. The sulfides segregation can be ascribed to thecrust contamination and the olivine crystallization.
新疆北部是我国,也是全球岩浆型Ni-Cu-(PGE)硫化物矿床分布最密集的地区之一,该区位于中亚造山带南部边缘。研究这些与岩浆型Ni-Cu-(PGE)硫化物矿床有关的镁铁-超镁铁质岩体的成因,对造山带内的岩浆型Ni-Cu-(PGE)硫化物矿床的找矿勘查活动以及研究中亚造山带的形成和演化具有重要的意义。前人对这些岩体的成因研究较为薄弱。本文选择位于不同构造单元的白石泉(中天山)、黄山东(东天山)和喀拉通克(阿尔泰山南缘)镁铁-超镁铁质岩体进行系统的岩石学和地球化学研究,探讨三个典型岩体的岩石成因,以期为研究区的岩浆型Ni-Cu-(PGE)硫化物矿床的找矿提供线索,同时为后造山作用过程提供约束条件。目前取得的主要认识有:
1.白石泉、喀拉通克、黄山东镁铁-超镁铁质侵入体是造山后碰撞阶段岩浆活动的产物,它们具有相同的地球动力学背景。
2.三个岩体的岩石组合及含矿岩石类型不同,但造岩矿物特征大体相同。白石泉岩体与黄山东岩体包括超镁铁质与镁铁质岩石,而喀拉通克岩体缺乏超镁铁质岩石。前两个岩体的主要含矿岩石为橄榄岩与辉石岩,喀拉通克岩体主要为苏长岩含矿。
3.三个岩体均具有大离子亲石元素(LILE)和轻稀土元素(LREE)富集,高场强元素(HFSE)亏损的微量元素特征。均具有低的Sr同位素初始比值,正的εNd值和低的放射性成因Pb,高于地幔的O同位素特征。白石泉岩体与黄山东岩体均具有极低的铂族元素成分,并且铂族元素主要受结晶分异作用的影响。
4.三个岩体的母岩浆性质相似,均为含有水的高镁拉斑玄武岩。但是它们的母岩浆中MgO的含量有别。
5.三个岩体的源区相似,岩浆的演化特征相近。它们的源区均为受到俯冲洋壳物质混染的软流圈地幔。它们的原始岩浆均经过了两个阶段的演化。第一阶段为橄榄石的结晶与硫化物的熔离阶段,第二个阶段为富含橄榄石与硫化物“晶粥”的就地分异阶段。地壳物质混染和橄榄石的结晶是岩浆中S饱和的主控因素。关键词:岩浆型Ni-Cu-(PGE)硫化物,镁铁-超镁铁岩,地球化学,新疆北部
Recently, the increased demand of Cu, Ni, Pt and Pd, etc., greatly promotes the research onthese mafic-ultramafic rocks associated with magmatic Ni-Cu-(PGE) sulfide deposits.Furthermore, the mafic-ultramafic rocks can be an important object to understand crust-mantlemagmatism and the process of continental geodynamics.
In the past twenty years about 20 magmatic Ni-Cu-(PGE) sulfide deposits and occurrenceshave been discovered in northern Xinjiang, China. These Ni-Cu-(PGE) sulfide deposits, relatedto mafic-ultramafic intrusions, are one component of the large scale metallogenesis duringpost-collisional tectonism in Late Carboniferous–Early Permian within the Central AsianOrogenic belt. To understand the origin of these Ni-Cu-(PGE)-bearing mafic-ultramaficintrusions is potentially important not only to the guidence exploration on Ni-Cu-(PGE) sulfidedeposits in orogenic belt but also to the study on the evolution of the CAOB. However, theprevious studies were focused on these Ni-Cu-(PGE) deposits, with little attention to the originand evolution of these mafic-ultramafic intrusions. Thus, three intrusions, including Baishiquanintrusions in Central-Tianshan Block, Huangshandong intrusions in Jueluotage orogenic beltand Kalatongke intrusions in Altay orogenic belts, are chosen for objects in this dissertation.The characteristics of petrology, mineralogy and geochemistry on these intrusions areinvestigated for the purpose as follow: (1) to determine the petrogenesis and evolution of theserocks;(2) to provide some clues for Ni-Cu-(PGE) sulfide ore genesis;(3) to discuss the mantlesource regions to understand the geodynamic processes;(4) to compare these characteristicsand find the reasons of similarities and differences, to discuss the regularities of formation forthe magmatic Ni-Cu-(PGE) sulfide deposits in orogenic belt. (5) to provide some constraints forthe process of post-collisional tectonism.
On the basis of the systematically research on three mafic-ultramafic intrusions hostingNi-Cu-(PGE) sulfide deposits in the CAOB, some conclusion has been drawn:
(1) The Baishiquan, Huangshandong and Kalatongke mafic-ultramafic intrusions occurredin the postcollisional setting and were related to lithospheric delamination and magmatic
underplating.(2) These intrusions have different rock assemblages and host rocks for Ni-Cu deposits,although the petrogenetic minerals are same. The Baishiquan and Huangshandong intrusionsare composed of peridotite, pyroxenite, hornblendite, troctolite, norite, gabbro and diorite, andthe Kalatongke intrusions consist of norite, gabbro-norite and biotite diorite. The peridotite andpyroxenite are the main host rocks for the Cu-Ni ores in the Baishiquan and Huangshandongintrusion, while norite in Kalatongke intrusion.(3) All of the intrusions are characterized by enrichment in large ion lithophile elements(LILE, e.g., Rb, Sr, K, U, Pb and Th) and light rare earth elements (LREE), depletion in highfield strength elements (HFSE, e.g., Nb, Ta, Ti and P) in relative to primitive mantle andMORB. Their Sr, Nd, Pb and O isotope data suggest a mixture of depleted asthenosphericmantle with MORB-like isotopic signature and subducted slab with EMⅡisotopic signature.The absolute PGE abundances are low, and the PGE is mainly affected by crystallizationdifferentiation in the Baishiquan and huangshandong intrusions.(4) The parental magmas are high-magnesium tholeiite, but have different contents in MgO.(5) The primitive magmas are derived from the asthenospheric mantle contaminated bypreviously subduction material. The primary magma with high-magnesium componentsexperienced two stages evolution. Olivine is the main fractionated phase in first stage of magmaevolution, and sulfides segregated from the silicate magma. The parental magma, which isolivine-and sulfide-laden crystal mush, entered the high-level magma chamber anddifferentiated in situ to form these intrusions. The sulfides segregation can be ascribed to thecrust contamination and the olivine crystallization.
引文
Barnes S J, Boyd R, Komeliusson A, et al. The use of mantle normalization and metal ratios in discriminatingbetween the effects of partial melting, crystal fractionation and sulphide segregation on platinum-groupelements, gold , nickel and cop-per: examples from Norway. In : Prichard H M, Potts P J, Bowles J F W,Cribb S J, eds . Geo-Platinum 87. London:Elsevier,1988,113～143
Brey J D, Kohler T P. 1990. Geothermobarometry in four-phase iherzolite: Ⅱ. new thermobarometers , andpractical assessment of existing thermobarometers [J]. J. Petrol. , 31: 1335-1378.
Campbell I H, Barnes S J. A model for the origin of the platinum-rich sulphide horizons in the Bushveld andStillwater Complexes. Journal of Petrology, 1983,24: 133～165
Chai G, Naldrett A J. Characteristics of Ni-Cu-PGE mineralization and genesis of the Jinchuan deposit,Northwest China. Economic Geology,1992, 87:1475～1495
Chung S L, Wang K L, Crawford A J, et al. High-Mg potassic rocks from Taiwan: implications for the genesisof orogenic potassic lavas. Lithos, 2001, 59:153～-170
Clayton R N, Mayeda T K. The use of bromine pentafluoride in the extraction of oxygen fromoxides and silicates for isotopic analysis. Geochimica et Cosmochimica Acta, 1963,27: 43～52
Coleman R. Continental growth of Northwest China. Tectonics, 1989, 8:621-635
Dick H J B, Bullen T. Chromian spinel as a petrogenetic indicator in abyssal and alpine-typeperidotites and spatially associated lavas. Contrib. Mineral. Petrol. 1984,86: 54～76
Dick H J B, Natland J H. Late stage melt evolution and transport in the shallow mantle beneath the East PacificRise: Deep Sea Drilling Project. Initial Reports, 1996,147:103～134
Fleet M E, Crocket J H, Stone W E. Partitioning of platinum-group elements (Os , Ir , Ru , Pt , Pd) and goldbetween sulfide liquid and basalt melt. Geochimica et Cosmochimica Acta, 1996,60: 2397～2412
Foster J G, Lambert D D, Frick L R. Re–Os isotopic evidence for genesis of Archaean nickelores from uncontaminated komatiites. Nature, 1996,382:703 ～706
Garuti G, Fershtater G, Bea F,et al. Platinum-group elements as petrological indications in mafic-ultramaficcomplexes of the central and southern Urals: preliminary results. Tectonophysics,1997,276: 181～194
Green T H. Experimental studies of trace-element partitioning applicable to igneous petrogenesisSedona 16 years lutes. Chemical Geology, 1994,117: 1～36
Hammarstrom J M,Zen E A. 1986. Aluminum in hornblende: an empirical igneous geobarometer.American Mineralogist, 1986,71: 1297-1313.
Hart S R, 1984. A large-scale isotope anomaly in the southern hemisphere mantle. Nature, 309,753-756
Haughton D R, Roeder P L,Skinner B J. 1974. Solubility of sulfur in mafic magmas. EconomicGeology,1974, 69: 451～467
Hawkesworth C J, Kempton P D, Rogers N W,et al. Continental mantle lithosphere, and shallowlevel enrichment processes in the Earth's mantle. Earth Planetary Science Letters, 1990, 96:256～268
Hollister L S, Grissom G C, Peters E K, et al. Confirmation of the empirical correlation of Al inhornblende with products of solidification in calc-akaline plutons. American Mineralogist,1987, 72: 231 -239.
Irvine T N, Keith D W, Todd S G. The J-M platinum-palladium reef of the Stillwater Complex, Montana: Ⅱ.Origin by double diffusive convective magma mixing and implications for the Bushveld Complex.Economic Geology, 1983,78: 1287～1334
Irvine T N. Crystallization sequences of the Muskox intrusion and other layered intrusions:Ⅱ.Origin ofchromitite layers and similar deposits of other magmatic ores. Geochimical et cosmchimica acta,1975,39: 991～1020
Ito E, White W M, Gopel C. The O, Sr, Nd, and Pb isotope geochemistry of MORB. ChemicalGeology,1987,62: 157～176
Jagoutz E. The abundances of major, minor and trace elements in the Earth's as derived fromprimitive ultramafic nodules. Proceeding of the 10th Lunar Science Conference,1979,10:2031-2050
Jahn B M, Windley B, Natal'in B, et al. Phanerozoic continental growth in Central Asia. Journal of Asian EarthSciences, Preface, 2004, 23: 599-603
Jahn B M, Wu Fuyuan, Chen Bin. Massive granitoid generation in Central Asia: Nd isotope evidence andimplication for continental growth in the Phanerozoic. Episodes, 2000, 22:82-92
James D E.The combined use of oxygen and radiogenic isotopes as indicators of crustalcontamination. Earth Planetary Science Letters. 1981, 15:395～396
Keays R R. The role of komatiitic and picritic magmatism and S-saturation in the formation of ore deposits.Lithos, 1995,34: 1～18
Kushiro I. Si-Al relation in clinopyroxenes from igneous rocks. Amercian Journal of Science, 1960, 258:518～551
Kyser T K, Carmeron W E,Nisbet E G. Boninite petrogenesis and alteration history;constraintsfrom stable isotope compositions of boninites from Caoe Vogel, New Caledonia and Cyprus.Contributions to mineralogy and petrology, 1982,93:222～226
Lambert D D, Foster J G, Frick L R, et al. Re–Os isotopic systematics of the Voisey's BayNi–Cu–Co magmatic ore system, Labrador, Canada. lithos,1999,47, (1-2): 69～88
Lambert D D, Foster J G, Frick L R, et al. Geodynamics of magmatic Cu-Ni-PGE sulfide deposits : New insights from the Re-Os isotopic system. Economic Geology, 1998a, 93 (2): 121～137
Lambertt D D, Walker R J,Morgan J W. Re-Os and Sm-Nd isotope geochemistry of the Stillwater Complex, montana: implications for the prteogenesis of the J-M Reef. Journal of petrology,1998b, 35: 1717～1753
Larsen L.M, Pedersen A K. Processes in high-Mg, high-T magmas: evidence from olivine, chromite and glass in Palaeogene picrites from West Greenland. Journal of Petrology, 2000,41: 1071～1098
Lassiter J, Depaolo D L. Plume/lithosphere interaction in the generation of continental and oceanic flood basalt: chemical and isotope constraints. In: Mahoney J. (eds). Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. Geophysical Monography 100, Amercian Geophysical Union,1997,335～355
Le Bas M J. IUGS reclassification of the high-Mg and picritic volcanic rocks. Journal of Petrology, 2000, 41:1467～1470
Le Bas M J. The rock of aluminium in igneous clinopyroxenes with relation to their parentage. Amercian Journal of Science, 1962, 260: 267～288
Lesher C M, Campbell I H. Geochemical and fluid dynamic controls on the composition of Komatitite-hosted nickel sulphide ores in Western Australia. Economic geology, 1993,88:804～816
Lesher C M, Lee R F, Groves D I, et al. Geochemistry of komatiites from Kambalda, Western Australia:Ⅰ.Chalcophile element depletion ,a consequence of sulphide liquid separation from komatiitic magmas. Economic geology,1981,76: 1714～1728
Lesher C M, Stone W E. Exploration geochemistry of komatiites. In: Wyman D A, eds. Trace element geochemistry of volcanic rocks: applications for massive sulphide exploration. Geological Association of Canada Short Course Notes, 1996,12: 153～204
Li C S, Xu Z H, De Wall S A,et al. Compositional variations of olivine from the Jinchuan Ni-Cu sulfide deposit, western China: implications for ore genesis. Mineralium deposita, 2004, 39:159～172
Li Jinyi, Xiao Wenjiao, Wang K, et al. Neoproterozoic-Paleozoic tectonostratigraphy, magmatic activities and tectonic evolution of eastern Xinjiang, NW China. in: Mao J W, Goldfarb R J, Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolution and Metallogeny of the Chinese Altay and Tianshan,IAGOD Guidebook Series 10. London:2003, p. 31-74
Lightfoot P C, Hawkesworth C J. 1997. Flood basalts and magmatic Ni, Cu and PGE sulphide mineralization: Comparative geochemistry of the Noril'sk (Siberian Trap) and West Greenland Sequences. In: Mahoney J J, Coffin M F, eds. large igneous province. Washington DC,Amercian Geophysical Union:1997, 357～380
Lindsley D H. Pyroxene thermometry. American Mineralogist, 1983, 68: 477～493
Liu Wei, Fei Xiaopan. Methanerich fluid inclusions from ophiolitic dunite and post-collisional mafic-ultramafic intrusion: the mantle dynamics underneath the Palaeo-Asian Ocean through to the post-collisional period. Earth and Planetary Science Letters, 2006,242: 286～301
Lorand J P, Alard O. Platinum-Group element abundances in the upper mantle : new constraints from in situ and whole-rock analyses of Massif Central xenoliths (France). Geochimica et Cosmochimica Acta, 2001,65 (16): 2789～2806
Lorand J P. Are spinel iherzolite xenoliths representative of the sulfur content of the upper mantle? Geochimical et cosmchimica acta, 1990,54: 1487～1492
Maier W D, Barnes S J, De Waal S A . Exploration for magmatic Ni-Cu-PGE sulphide deposits: A review of recent advances in the use of geochemical tools, and their application to some south African ores. South African Geology, 1998, 101(3): 237～253
Maier W D, Barnes S J,Li C S. A re-evaluation of the role of crustal contamination in the formation of magmatic sulfides in the Bushveld Complex. In: The 9th international PGE symposium. Montana, USA , 2002(July 21-25)
Maier W D, Barnes S J. The origin of Cu sulfide deposits in the Curaca valley, Bahia , Brazil : evidence from Cu, Ni, Se,and platinum-group element concentrations. Economic Geology, 1999, 94(2): 165～183
Maier W D, Li C S,De Wall S A. Why are there no major Ni-Cu sulfide deposits in large layers mafic-ultramafic intrusions? Canada Mineral, 2001,3:547～556
Mao J W, Goldfarb G J, Wang Y T, et al. Late Paleozoic base and precious metal deposits, East Tianshan, Xinjiang, China: Charateristics and geodynamic setting. Episodes, 2005, 28(1): 23-36
Mao J W, Konopelko D, Seltmann R, et al. Postcollisional age of the Kumtor gold deposit and timing of Hercynian events in the Tien Shan, Kyrgyzstan. Economic Geology, 2004, 99(8): 1771-1781
Mattey D, Lowry D, Macpherson C. Oxygen isotope composition of mantle periotite. Earth Planet. Earth and Planetary Science Letters, 1994, 128: 231～241
McDonough W F, Sun S S. The composition of the earth. Chemical Geology, 1995,120 : 233～253 Mckenzie D, O'Nions R K. Partial melt distributions from inversion of rare earth element concentrations. Journal of petrology, 1991,32:1021～1091
Mckenzie D,Bickle M J. The volume and composition of melt generated by extension of the lithosphere. Journal of petrology,1988,29:53～72
Mckenzie D. Cratonic, circumeratonic and oceanic mantle domians beneath the western United states. Journal of geophysical research, 1989,94:7899～7915
Menzies M A. Archaean, Proterozoic, and Phanerzoic lithospheres. In: Menzies M A, eds.Continental mantle. New York: Oxford Science Publications,1990,67～86
Miyashiro A. Volcanic rock series in island arcs and active continental margins. American Journal of Science, 1974, 274: 321～355
Morimoto N. Nomenclature of pyroxenes. Mineralogical Magazine,1988,52: 535～550 Naldrett A J. Magmatic sulfide deposits. Springer Berlin. 2004b, 128: 303-311
Naldrett A J. Magmatic Sulphie Deposits. New York: Oxford University Press. 1989.1～186
Naldrett A J. An overview of Ni-Cu mineralization with conclusions guide in exploration. InternationalGeological correlation program IGCP479 short course notes, 2004a, 154～164
Naldrett A J. Key factors in the genesis of Noril'sk, Sudbury, Jinchuan, Voisey's Bay and other world-classNi-Cu-PGE deposits: implication for exploration. Australian Journal of Earth Sciences, 1997,44: 281～315
Naldrett A J. Nickle sulphide deposits: Their classification and genesis with special emphasis on deposits ofvolcanic association. Canadian Mining and Metallurgical Bull,1973,66: 45～63
Naldrett A J. World-class Ni-Cu-PGE deposits: key factors in their genesis. Mineralium Deposita, 1999,34:227～240
Neal C R, Mahoney J J, Chazey W J. Mantle sources and the highly variable role of continentallithosphere in basalt petrogenesis of the Kerguelen Plateau and Broken Ridge LIP: resultsfrom ODP Leg 183. Journal of petrology, 2002, 43: 1177～1205
Peltonen P. Petrogenesis of ultramafic rocks in the Vammala Nickel Belt: Implication for crustal evolution ofthe early Proterozoic Svecofennian arc terrane. Lithos,1995,34:253～274
Qin Kezhang, Zhang Lianchang, Xiao Wenjiao,et al. Overview of major Au, Cu, Ni and Fe deposits andmetallogenic evolution of the eastern Tianshan Mountains, Northwestern China. in: Mao J W, Goldfarb R J,Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolution and Metallogeny of the Chinese Altayand Tianshan,IAGOD Guidebook Series 10. London:2003, 227～248
Rehkamper M , Halliday A N , Fitton J G ,et al. Ir, Ru, Pt in basalts and komatiites: New constraints for thegeochemical behavior of the platinum-group elements in the mantle. Geochimical et cosmchimicaacta, 1999,63(22):3915～3934
Ripley E M, Lightfoot P C, Li C S , et al . Sulfur isotopic studies of continental flood in the Noril'sk region:implications for the association between lavas and ore-bearing intrusions. Geochimical et cosmchimicaacta, 2003,67 (15): 2805～2817
Ripley E M,Alawi J A .Petrogenesis of pelitic xenoliths at the Babbitt Cu-Ni deposit , Duluth Complex,Minnesota, USA. Lithos, 1988,21: 143～159
Roeder P L, Emslie R F. 1970. Olivine-liquid equilibrium. Contributions to Mineralogy and Petrology,1970,29:275～289
Rollinson H R. Using geochemical data: evolution, presentation, interpretation. New York:Longman Science Technology. 1993.48～51
Sakuyama M. Petrology of arc volcanic rocks and their origin by mantle diapers. Journal ofVolcanology and Geothermonology Research, 1983,18: 297～320
Saunders A D, Norry M J,Tarney J. Origin of MORB and chemically depleted mantle reservoirs:trace element constraints. Journal of Petrology (Special Lithosphere Issue),1988,425～445
Schmidt M W. Amphibole composition in tonalite as a function of p ressure: An experimentalcalibration of the Al-in-hornblende barometer. Contributions to Mineralogy and Petrology,1992,110: 304-310.
Seghedi I, Downes H, Vaselli O, et al. Post-collisional Tertiary–Quaternary mafic alkalic magmatism in theCarpathian–Pannonian region: a review. Tectonophysics,2004, 393:43～62
Seng?r A M C, Natal'in B A, Burtman V S. Evolution of the Altaid tectonic collage and Paleozoic crustalgrowth in Eurasia. Nature, 1993, 364: 209-304
Shima H, Naldrett A J. Solubility of sulfur in an ultramafic melt and the relevance of the system Fe-S-O.Economic geology, 1975,70: 960～967
Simkin T, Smith J V. Minor element distribution in olivine. Journal of Geology, 1970, 78: 304～325
Still P, Unruh D M, Tatsumoto. Pb, Sr, Nd and Hf isotopic evidence of multiple for Oahu, Hawwiibasalt. Nature,1983,304: 25-29
Stolz A J, Jochum K P, Hofmann A W. Fluid-and melt-related enrichment in the subarc mantle;evidence fromNb/Ta variations in island-arc basats. Geology,1996, 24:587～590
Sun S S, de Waal S A, Hoatson D M,et al. Use of geochemistry as a guide to platinum group elementpotentials of mafic-ultramafic rocks: examples from the weat Pilbara Block and Halls Creek Mobile Zone,western Australia. Precambrian Research,1991,50:1～35
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.Geological Society. London:Special Publication, 1989, 42: 313～345
Taylor S R, Mclennan S M. 1985. The continental crust: its composition and evolution. London: BlackwellScientific Publications,1985. 1～312
Thirlwall M F, Smith T E, Graham A M. High field strength element anomalies in arc lavas: Source or process?Journal of Petrology,1994,35: 819～838
Thompson R N. Some high-pressure pyroxenes. Mineralogical Magazine, 1974, 39: 768～787
Vogt J H L. Geenetischen classification der durch magmatische differentions processe under durchprevinathloyse entslandenen erzoskommen. Z. Ponkt. Geol., 1894, 381-399
Wendlandt R F. Sulphide saturation of basalt and andesite melts at high pressures and temperature. Americanmineralogist,1982,67: 877～885
Wilson M. Igneous Petrogenesis, London: Unwin Hyman, 1989
Windley B F, Allen M B, Zhang C, et al. Paleozoic accretion and Cenozoic re-deformation of the Chinese TienShan Range, Central Asia. Geology, 1990, 18:128-131
Wu F Y, Wilde S A, Zhang G L, et al. Geochronology and petrogenesis of the post-orogenicCu–Ni sulfide-bearing mafic–ultramafic complexes in Jilin Province, NE China. Journal ofAsian Earth Sciences, 2004, 23:781～797
Xiao W J, Zhang L C, Qin K Z, et al. Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China): Implications for the continental growth of Central Asia. American Journal of Sciences, 2004,304:370-395
Yan Shenghao, Zhang Zhaochong, Wang Denghong, et al. 2003. Kalatongke magmatic copper-nickl sulfidedeposit. in: Mao J W, Goldfarb R J, Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolutionand Metallogeny of the Chinese Altay and Tianshan, IAGOD Guidebook Series 10. London:2003, 131～151
Zhou, M F, Leshen, C M., Yang, Z X.,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. Chemical Geology,2004, 209,233-257
Zindler A, Hart S R. Chemical dynamics. Ann. Rev. Earth Planetary Science Letters, 1986, 14: 493～571
Zou, H B, Zindler, A, Xu, X S, et al. Major, trace element, and Nd, Sr and Pb isotope studies ofCenozoic basalts in SE China: mantle sources, regional variations, and tectonic significance.Chemical Geology, 2000, 171: 33～47
白云来. 新疆哈密黄山一镜儿泉镍铜成矿系统的地质构造背景.甘肃地质学报, 2000,9(2): 1-7
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.新疆地质,1993,11(1):34一42
柴凤梅, 张招崇,毛景文, 等. 中天山白石泉镁铁-超镁铁质岩体岩石学与矿物学研究. 岩石矿物学杂志, 2006, 25(1):1～12
车自成, 刘洪福, 刘良,等.中天山造山带的形成与演化. 北京: 地质出版社,1994
陈丹玲, 刘良, 车自成,等.中天山骆驼沟火山岩的地球化学特征及其构造环境. 岩石学报,2001,17(3): 378～384
陈光远, 孙岱生, 殷辉安. 成因矿物学与找矿矿物学. 四川:重庆出版社, 1984.1～874
陈浩琉,吴水波,傅德彬,等. 镍矿床. 北京:地质出版社, 1993,1-199
陈衍景.中国区域成矿研究的若干问题及其与陆陆碰撞的关系. 地学前缘,2002,9(4):319～328
陈衍景.中国西北地区中亚型造山—成矿作用的研究意义和进展.高校地质学报,2000,6(1):17～22
陈毓川, 赵 逊, 张之一, 等.世纪之交的地球科学-重大地学领域进展[M] .北京:地质出版社,2000
陈毓川等,1995,阿尔泰黄金有色金属开发区成矿地质条件与矿产资源评价研究,305科研报告
董传万, 徐夕生, 陈小明, 等. 福建平潭角闪辉长岩结晶过程的矿物学记录. 矿物学报,1997,17(3): 285～290
董云鹏, 周鼎武, 张国伟.东秦岭富水基性杂岩体地球化学特征及其形成环境.地球化学,1997,26(3):79～88
范育新,张铭杰.超大型铜镍硫化物矿床研究进展. 甘肃地质学报,1999,8 (2): 47～52方国庆.新疆东部大地构造特点及演化. 西北地质,1991,1-12
冯益民. 新疆西部构造发展史. 中国北方板块构造文集(第一集). 北京: 地质出版社,1986.
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. 兰州大学学报(自然科学版), 1993a, 29(4): 236～240
傅学明, 郭原生, 张铭杰, 等. 新疆黄山镁铁-超镁铁杂岩体化学成分特征及其含矿性关系. 兰州大学学报(自然科学版), 1993b,29(3): 213～221
高怀忠. 新疆坡北基性-超基性岩带1 号岩体地质特征及其含矿性研究. 地球科学-中国地质大学学报, 1992,17(4): 391～401
葛文春,林强,孙德有.大兴安岭中生代玄武岩的地球化学特征: 壳幔相互作用的证据.岩石学报,1999,15(3):396～407
顾连兴, 苟晓琴 , 张遵忠,等.东天山一个多相带高铷氟花岗岩的地球化学及成岩作用. 岩石学报, 2003,19(4): 585～600
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. 岩石学报, 1994. 10 (4): 339～356
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. 科学通报, 2004, 49(22): 2324～2328
韩宝福,何国琦,王式洸,等. 新疆北部后碰撞幔源岩浆活动与陆壳纵向生长.地质论评,1998,44, 396～406
韩宝福,何国琦,王式洸. 后碰撞幔源岩浆活动底垫作用及准噶尔盆地基底的性质.中国科学(D辑),1999,29(1):16～21
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.地质学报,2006,80(1):74～89
何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化与成矿. 乌鲁木齐: 新疆人民出版社,香港: 香港文化教育出版社,1994
洪大卫,王式洸,谢锡林,等. 兴蒙造山带正εNd值花岗岩的成因和大陆地壳生长. 地学前缘, 2000,7:441～456
洪大卫,王式洸,谢锡林,等.从中亚正εNd 值花岗岩看超大陆演化和大陆地壳生长的关系.地质学报,2003,77(2):203～209
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).北京:地质出版社, 1990
胡素芳.攀西地区红格、新街岩体的岩石地球化学特征.博士学位论文.北京:中国科学院地质地球物理研究所,2001
黄智龙,王联奎.云南老王寨金矿区黄斑岩的地球化学.地球化学,1996,25(3):5-263
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. 矿物岩石, 1984, 4(3)
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. 北京: 地质出版社, 1998, 202-221
李锦轶, 王克卓, 李文铅,等.东天山晚古生代以来大地构造与矿产勘查. 新疆地质, 2002, 20 (4) : 296～301
李锦轶,徐新.新疆北部地质构造和成矿作用的主要问题.新疆地质,2004,22(2):119～124
李锦轶.试论中国新疆准噶尔山系古生代板块构造演化.见肖序常、汤耀庆主编.古中亚复合巨型缝合带南缘构造演化.北京:北京科学技术出版社,1991,92-108
李锦轶.新疆东部新元古代晚期和古生代构造格局及其意义.地质论评,2004,50(3):304-322.
李凯明 , 赵海玲 , 邓晋福 . 2002 . 山西平顺岩体岩石学/矿物学特征及角闪石成因 [J] . 北京地质 , 14 (4): 41-47.
李曙光, 聂永红, 郑双根,等. 俯冲陆壳与上地幔的相互作用——Ⅰ. 大别山同碰撞镁铁-超镁铁岩的主要元素及痕量元素地球化学. 中国科学 (D 辑), 1997,27 (6): 488～493
李文渊. Re-Os同位素体系及其在岩浆Cu-N i-PGE矿床研究中的应用. 地球科学进展 , 1996,11 (6): 580～584
李先梓, 李行, 洛长义, 等. 新疆铂族元素成矿地质条件及找矿方向研究. 中国地质科学院西安地质矿产研究所所刊, 1991, 33: 1～93
李献华, 周汉文, 韦刚健, 等, 滇西新生代超钾质煌斑岩的元素和 Sr-Nd 同位素特征及其对岩石圈地幔组成的制约. 地球化学, 2002,31(1):26～35
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. 矿床地质, 1992, 11 (4): 307～314
刘德权,唐延龄,周汝洪.中亚古生代造山带成矿作用基本特征.西北地质,2001,34(2):1-10
刘德权. 新疆板块构造与矿产分布.西北地质,1983,4(2):1～12
刘民武.中国几个镍矿床的地球化学比较研究:博士学位论文.西安:西北大学, 2003
刘月星.铜镍硫化物矿床成矿作用及成矿模式研究.矿产与地质,1997,11(4):225～231
龙小平, 王立社, 余能. 东昆仑山清水泉镁铁质-超镁铁质岩的地球化学特征. 地质通报, 2004,23 (7): 664-669
马鸿文. 结晶岩热力学概论. 北京:高等教育出版社, 2001.1～297
马鸿文.介绍改进的单斜辉石地质温度计公式. 地质科技情报, 1985,4(2): 82～84
马瑞士,舒良树,孙家齐,等.东天山构造演化与成矿.北京:地质出版社, 1997
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, 1997, 17(增刊): 35～47
马润则, 肖渊甫. 米仓山地区晋宁期基性超基性侵入岩中造岩矿物研究. 成都理工学院学报, 2001, 28 (1): 34～39
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. 矿床地质, 2002,21(4): 323～330
毛景文,Franco Pirajno,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:主要特点及与地幔柱关系(待发表). 2006.
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.地质学报,2005,79(3):342-372
倪志耀, 卫管一. 新疆东部基性超基性岩的地质地球化学特征. 矿物岩石, 1995, 15(1):8～17
倪志耀. 黄山东镁铁超镁铁杂岩中的辉石化学成分研究. 岩石矿物学杂志, 1994, 13(1):55～66
倪志耀. 新疆哈密黄山东镁铁-超镁铁杂岩体成因探讨. 西北地质, 1992, 13(2):9～16
倪志耀. 新疆哈密黄山东镁铁一超镁铁杂岩体中橄榄石的化学成分及其岩石学意义.1991,1(3):40～47
倪志耀. 岩浆深渊分异在新疆黄山杂岩体成岩成矿中的作用. 成都地质学院学报, 1993, 20(2):33～39
帕拉提·阿布都卡迪尔,黄建华,吴兆宁.喀拉通克铜镍矿床伴生贵金属赋存富集规律.新疆工学院学报,1996,17(2):79～85
潘长云,王润民,赵昌龙.新疆喀拉通克 Y_1 含矿岩体的岩石化学特征及其与成矿的关系.岩石学报,1994,10(3):261～274
秦克章.新疆北部中亚型造山与成矿作用.博士后研究报告.北京:中国科学院地质与地球物理研究所地质学博士后流动站,2000
邱家骧, 廖群安. 中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息. 岩石矿物学杂志, 1987,6(1):56-63
邱家骧, 林景仟.岩石化学. 北京: 地质出版社,1991.140～156
冉红彦, 肖森宏.喀拉通克含矿岩体的微量元素与成岩构造环境. 地球化学, 1994,23(4):392-401
申茂德. 东天山香山铜镍矿区构造特征与成岩成矿. 新疆地质, 2003, 21(2):195～198
师占义. 橄榄石标型特征及其找矿意义. 西北地质科学, 1994,15(1):11～16
舒良树,卢华复,印栋浩,等.新疆北部古生代大陆增生构造.新疆地质,2001,19(1):59～63
孙传敏. 四川盐边元古代蛇绿岩中辉石的成因矿物学及其大地构造意义. 矿物岩石, 1994, 14(3): 1～15
汤耀庆, 高俊, 赵民,等.西南天山蛇绿岩与蓝片岩. 北京: 地质出版社,1995
汤中立,李文渊. 金川铜镍硫化物模式及地质特征对比. 北京 :地质出版社.1995
汤中立. 超大型岩浆硫化物矿床的类型及地质对比意义.甘肃地质学报 ,1992,1(1):24～47
王崇义, 石长运, 王晓亭. 黄山基性-超基性岩体成岩机制及其含矿性初步探讨. 新疆地质, 1986, 4(1): 1～11
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. 矿床地质, 2000, 19(2):147～155
王登红, 陈毓川, 徐志刚, 李天德,傅旭杰. 阿尔泰成矿省的成矿系列及成矿规律. 北京: 原子能出版社,2002.1～492
王京彬, 徐新. 新疆北部后碰撞构造演化与成矿. 地质学报, 2006, 80: 23～31
王京彬,李博泉,张积斌,等.额尔齐斯聚矿带金铜成矿条件及找矿预测.北京:冶金工业出版社,1999.
王瑞廷, 毛景文, 赫英等.煎茶岭硫化镍矿床的铂族元素地球化学特征及其意义 . 岩石学报, 2005,21(1): 219～226
王瑞廷, 毛景文, 柯洪,等. 铜镍岩浆硫化物矿床成矿作用研究综述. 矿产与地质, 2003, 17 (增刊): 281～284
王瑞廷. 煎茶岭与金川镍矿床成矿作用比较研究: [博士学位论文]. 西安: 西北大学, 2002
王润民, 王志辉. 新疆喀拉通克一号岩体及铜镍硫化物矿床地质特征.中国地质科学院院报, 1993, 95～102
王润民,李思楚.新疆哈密黄山东铜镍硫化物矿床成岩成矿物理化学条件.成都地质学院,1987, 14(3):1～10
王润民、赵昌龙.新疆喀拉通克一号铜镍硫化物矿床.北京:地质出版社,1991. 1～298
王有标. 新疆铜镍硫化物矿床地基本地质特点.1990, 8: 305～320
王玉往, 王京彬,王莉娟,等.新疆哈密黄山地区铜镍硫化物矿床的稀土元素特征及意义.岩石学报,2004,20(4):935-948
王中刚,赵振华,邹天人,等.新疆北部花岗岩类的成因类型及其成矿作用.见:涂光炽主编, 新疆北部固体地球科学新进展.北京: 科学出版社,1993. 127～136
吴福元,江博明,林强.中国北方造山带造山后花岗岩的同位素特点与地壳生长意义.科学通报,1997,42(20):2188～2192
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. 地质学报, 79(4):498～502
吴利仁. 论中国基性岩、超基性岩的成矿专属性. 地质科学, 1963, (1):29～41
吴平霄, 吴金平, 李才伟,等.斜长石韵律环带的结晶速率方程及其动力学机制. 岩石学报, 1998,14(3): 388～394
吴平霄, 吴金平, 肖文丁, 等. 斜长石环带的成因机制. 地质地球化学, 1997,(4): 40～49
夏林圻,夏祖春,徐学义,等.天山石炭纪大火成岩省与地幔柱.地质通报,2004,23(9-10):903～910
夏林圻,张国伟,夏祖春,等.天山古生代洋盆开启、闭合时限的岩石学约束—— 来自震旦纪、石炭纪火山岩的证据. 地质通报,2002,21(2):56-62.
夏祖春, 徐学义, 夏林圻,等.天山石炭-二叠纪后碰撞花岗质岩石地球化学研究。西北地质,2005, 38(1):1～14
肖序常, 汤耀庆. 古中亚复合巨型缝合带南缘构造演化. 北京: 北京科学技术出版社, 1991, 1-29
肖序常,汤耀庆,冯益民,等. 新疆北部及其邻区大地构造.北京: 地质出版社,1992. 1～169
肖序常.从扩张速率试论蛇绿岩的类型划分. 岩石学报,1995, 11(增刊):10～23
肖渊甫, 马润则, 魏显贵, 等. 米仓山澄江期基性侵入杂岩特征及其成因探讨. 成都理工学院学报, 1998, 25(4): 537～-542
熊小林,赵振华,白正华,等.西天山阿吾拉勒埃达克质岩石成因:Nd 和 Sr 同位素组成限制.岩石学报,2001,17(4):514～522
熊永良. 铼-锇同位素体系对揭示矿质来源的作用. 地学前缘 ,1994,1 (3-4): 199～203
徐学义, 夏林沂, 夏祖春, 等. 岚皋早古生代碱质煌斑杂岩地球化学特征及成因探讨. 地球学报, 2001,22 (1): 55～60
徐学义,马中平,夏祖春等.天山石炭—二叠纪后碰撞花岗岩的Nd、Sr、Pb 同位素源区示踪.西北地质,2005,38(2):1～18
闫峻, 陈江峰, 喻钢,等.长江中下游晚中生代中基性岩的铅同位素特征 : 富集地幔的证据. 高校地质学报, 2003,9(2): 195～206
杨炳滨. 新疆北部岩浆型铜镍硫化物矿床控矿因素的研究. 矿产与地质, 1994, 8: 330～333
杨甲全, 钟莉, 邓刚. 北山地区坡北1号、10号基性一超基性岩体成矿预测及找矿方向. 新疆地质, 2002, 20(3): 214～218
杨学明,杨晓勇,陈双喜.岩石地球化学.合肥:中国科学技术大学出版社,2000.1～243
永文富.新疆哈密土墩基性—超基性岩岩体特征及其含矿性研究. 新疆有色金属, 2002, (3):1～6
张旗. 镁铁-超镁铁岩与威尔逊旋回. 岩石学报, 1992, 8(2):168～176
张儒瑗,从柏林.矿物温度计和矿物压力计. 北京:地质出版社,1983.1～280
张树明, 王方正.玄武岩在研究岩石圈深部过程及构造背景中的应用. 地球科学进展, 2002,17 (5): 685～692
张湘炳,隋静霞,李志纯,等.额尔齐斯构造带构造演化与成矿系列.北京:科学出版社,1996.
张招崇 , 阎升好, 陈柏林, 等. 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. 岩石矿物学杂志, 2003,22(3): 217～224
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. 吉林大学学报(地球科学版), 2003,33 (2): 130～134
张招崇,闫升好,陈柏林,等.阿尔泰铜矿带东段找矿靶区优选及评价,国家305项目2001BA609A-07-02专题科研报告,2005
张招崇,闫升好,陈柏林,等.阿尔泰造山带南缘镁铁质—超镁铁质杂岩体的 Sr、Nd、O 同位素地球化学及其源区特征探讨.地质论评,2006,52(1):38～42
张作衡,柴凤梅,杜安道,等. 新疆喀拉通克铜镍硫化物矿床 Re_Os 同位素测年及成矿物质来源示踪. 岩石矿物学杂志, 2005, 24(4):285～293
赵振华, 王中刚, 邹天人, 等. 新疆乌伦古富碱花岗岩成因探讨. 地球化学, 1996, 25: 205～220
郑详身. 西南极利文斯顿岛中部中一新生代火山岩的岩相学和矿物学特征. 南极研究(中文版),1995,7(1): 1～16
支霞臣, 靳永斌, 孟庆,等. 大别山北部饶拔寨超镁铁岩体微量元素地球化学. 岩石学报, 2004,20(3): 463～472
周英森. 喀拉通克铜镍硫化矿床Y_1号岩体岩相划分及岩石特征. 新疆地质, 1987, 5(3):9～15
朱维光. 扬子地块西缘新元古代镁铁质—超镁铁质岩的地球化学特征及其地质背景——以盐边高家村杂岩体和冷水箐101号杂岩体为例:[博士学位论文].北京:中国科学院地球化学研究所,2004
朱文斌, 马瑞士, 王赐银. 论新疆东部黄山-镜儿泉杂岩带的构造属性. 地质科学, 1996, 31, (1): 22～31
朱永峰.硫在岩浆熔体中的溶解行为综述.地质科技情报,1998,17(2):35～38
竺国强, 杨树锋, 陈汉林.东疆香山铜镍含矿镁铁超镁铁杂岩体控岩控矿构造探讨. 1995, 10(3):1～13
邹天人,曹惠志,吴柏青.新疆阿尔泰造山花岗岩和非造山花岗岩及其判别标志.地质学报,1988,62(3):228～243
Brey J D, Kohler T P. 1990. Geothermobarometry in four-phase iherzolite: Ⅱ. new thermobarometers , andpractical assessment of existing thermobarometers [J]. J. Petrol. , 31: 1335-1378.
Campbell I H, Barnes S J. A model for the origin of the platinum-rich sulphide horizons in the Bushveld andStillwater Complexes. Journal of Petrology, 1983,24: 133～165
Chai G, Naldrett A J. Characteristics of Ni-Cu-PGE mineralization and genesis of the Jinchuan deposit,Northwest China. Economic Geology,1992, 87:1475～1495
Chung S L, Wang K L, Crawford A J, et al. High-Mg potassic rocks from Taiwan: implications for the genesisof orogenic potassic lavas. Lithos, 2001, 59:153～-170
Clayton R N, Mayeda T K. The use of bromine pentafluoride in the extraction of oxygen fromoxides and silicates for isotopic analysis. Geochimica et Cosmochimica Acta, 1963,27: 43～52
Coleman R. Continental growth of Northwest China. Tectonics, 1989, 8:621-635
Dick H J B, Bullen T. Chromian spinel as a petrogenetic indicator in abyssal and alpine-typeperidotites and spatially associated lavas. Contrib. Mineral. Petrol. 1984,86: 54～76
Dick H J B, Natland J H. Late stage melt evolution and transport in the shallow mantle beneath the East PacificRise: Deep Sea Drilling Project. Initial Reports, 1996,147:103～134
Fleet M E, Crocket J H, Stone W E. Partitioning of platinum-group elements (Os , Ir , Ru , Pt , Pd) and goldbetween sulfide liquid and basalt melt. Geochimica et Cosmochimica Acta, 1996,60: 2397～2412
Foster J G, Lambert D D, Frick L R. Re–Os isotopic evidence for genesis of Archaean nickelores from uncontaminated komatiites. Nature, 1996,382:703 ～706
Garuti G, Fershtater G, Bea F,et al. Platinum-group elements as petrological indications in mafic-ultramaficcomplexes of the central and southern Urals: preliminary results. Tectonophysics,1997,276: 181～194
Green T H. Experimental studies of trace-element partitioning applicable to igneous petrogenesisSedona 16 years lutes. Chemical Geology, 1994,117: 1～36
Hammarstrom J M,Zen E A. 1986. Aluminum in hornblende: an empirical igneous geobarometer.American Mineralogist, 1986,71: 1297-1313.
Hart S R, 1984. A large-scale isotope anomaly in the southern hemisphere mantle. Nature, 309,753-756
Haughton D R, Roeder P L,Skinner B J. 1974. Solubility of sulfur in mafic magmas. EconomicGeology,1974, 69: 451～467
Hawkesworth C J, Kempton P D, Rogers N W,et al. Continental mantle lithosphere, and shallowlevel enrichment processes in the Earth's mantle. Earth Planetary Science Letters, 1990, 96:256～268
Hollister L S, Grissom G C, Peters E K, et al. Confirmation of the empirical correlation of Al inhornblende with products of solidification in calc-akaline plutons. American Mineralogist,1987, 72: 231 -239.
Irvine T N, Keith D W, Todd S G. The J-M platinum-palladium reef of the Stillwater Complex, Montana: Ⅱ.Origin by double diffusive convective magma mixing and implications for the Bushveld Complex.Economic Geology, 1983,78: 1287～1334
Irvine T N. Crystallization sequences of the Muskox intrusion and other layered intrusions:Ⅱ.Origin ofchromitite layers and similar deposits of other magmatic ores. Geochimical et cosmchimica acta,1975,39: 991～1020
Ito E, White W M, Gopel C. The O, Sr, Nd, and Pb isotope geochemistry of MORB. ChemicalGeology,1987,62: 157～176
Jagoutz E. The abundances of major, minor and trace elements in the Earth's as derived fromprimitive ultramafic nodules. Proceeding of the 10th Lunar Science Conference,1979,10:2031-2050
Jahn B M, Windley B, Natal'in B, et al. Phanerozoic continental growth in Central Asia. Journal of Asian EarthSciences, Preface, 2004, 23: 599-603
Jahn B M, Wu Fuyuan, Chen Bin. Massive granitoid generation in Central Asia: Nd isotope evidence andimplication for continental growth in the Phanerozoic. Episodes, 2000, 22:82-92
James D E.The combined use of oxygen and radiogenic isotopes as indicators of crustalcontamination. Earth Planetary Science Letters. 1981, 15:395～396
Keays R R. The role of komatiitic and picritic magmatism and S-saturation in the formation of ore deposits.Lithos, 1995,34: 1～18
Kushiro I. Si-Al relation in clinopyroxenes from igneous rocks. Amercian Journal of Science, 1960, 258:518～551
Kyser T K, Carmeron W E,Nisbet E G. Boninite petrogenesis and alteration history;constraintsfrom stable isotope compositions of boninites from Caoe Vogel, New Caledonia and Cyprus.Contributions to mineralogy and petrology, 1982,93:222～226
Lambert D D, Foster J G, Frick L R, et al. Re–Os isotopic systematics of the Voisey's BayNi–Cu–Co magmatic ore system, Labrador, Canada. lithos,1999,47, (1-2): 69～88
Lambert D D, Foster J G, Frick L R, et al. Geodynamics of magmatic Cu-Ni-PGE sulfide deposits : New insights from the Re-Os isotopic system. Economic Geology, 1998a, 93 (2): 121～137
Lambertt D D, Walker R J,Morgan J W. Re-Os and Sm-Nd isotope geochemistry of the Stillwater Complex, montana: implications for the prteogenesis of the J-M Reef. Journal of petrology,1998b, 35: 1717～1753
Larsen L.M, Pedersen A K. Processes in high-Mg, high-T magmas: evidence from olivine, chromite and glass in Palaeogene picrites from West Greenland. Journal of Petrology, 2000,41: 1071～1098
Lassiter J, Depaolo D L. Plume/lithosphere interaction in the generation of continental and oceanic flood basalt: chemical and isotope constraints. In: Mahoney J. (eds). Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. Geophysical Monography 100, Amercian Geophysical Union,1997,335～355
Le Bas M J. IUGS reclassification of the high-Mg and picritic volcanic rocks. Journal of Petrology, 2000, 41:1467～1470
Le Bas M J. The rock of aluminium in igneous clinopyroxenes with relation to their parentage. Amercian Journal of Science, 1962, 260: 267～288
Lesher C M, Campbell I H. Geochemical and fluid dynamic controls on the composition of Komatitite-hosted nickel sulphide ores in Western Australia. Economic geology, 1993,88:804～816
Lesher C M, Lee R F, Groves D I, et al. Geochemistry of komatiites from Kambalda, Western Australia:Ⅰ.Chalcophile element depletion ,a consequence of sulphide liquid separation from komatiitic magmas. Economic geology,1981,76: 1714～1728
Lesher C M, Stone W E. Exploration geochemistry of komatiites. In: Wyman D A, eds. Trace element geochemistry of volcanic rocks: applications for massive sulphide exploration. Geological Association of Canada Short Course Notes, 1996,12: 153～204
Li C S, Xu Z H, De Wall S A,et al. Compositional variations of olivine from the Jinchuan Ni-Cu sulfide deposit, western China: implications for ore genesis. Mineralium deposita, 2004, 39:159～172
Li Jinyi, Xiao Wenjiao, Wang K, et al. Neoproterozoic-Paleozoic tectonostratigraphy, magmatic activities and tectonic evolution of eastern Xinjiang, NW China. in: Mao J W, Goldfarb R J, Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolution and Metallogeny of the Chinese Altay and Tianshan,IAGOD Guidebook Series 10. London:2003, p. 31-74
Lightfoot P C, Hawkesworth C J. 1997. Flood basalts and magmatic Ni, Cu and PGE sulphide mineralization: Comparative geochemistry of the Noril'sk (Siberian Trap) and West Greenland Sequences. In: Mahoney J J, Coffin M F, eds. large igneous province. Washington DC,Amercian Geophysical Union:1997, 357～380
Lindsley D H. Pyroxene thermometry. American Mineralogist, 1983, 68: 477～493
Liu Wei, Fei Xiaopan. Methanerich fluid inclusions from ophiolitic dunite and post-collisional mafic-ultramafic intrusion: the mantle dynamics underneath the Palaeo-Asian Ocean through to the post-collisional period. Earth and Planetary Science Letters, 2006,242: 286～301
Lorand J P, Alard O. Platinum-Group element abundances in the upper mantle : new constraints from in situ and whole-rock analyses of Massif Central xenoliths (France). Geochimica et Cosmochimica Acta, 2001,65 (16): 2789～2806
Lorand J P. Are spinel iherzolite xenoliths representative of the sulfur content of the upper mantle? Geochimical et cosmchimica acta, 1990,54: 1487～1492
Maier W D, Barnes S J, De Waal S A . Exploration for magmatic Ni-Cu-PGE sulphide deposits: A review of recent advances in the use of geochemical tools, and their application to some south African ores. South African Geology, 1998, 101(3): 237～253
Maier W D, Barnes S J,Li C S. A re-evaluation of the role of crustal contamination in the formation of magmatic sulfides in the Bushveld Complex. In: The 9th international PGE symposium. Montana, USA , 2002(July 21-25)
Maier W D, Barnes S J. The origin of Cu sulfide deposits in the Curaca valley, Bahia , Brazil : evidence from Cu, Ni, Se,and platinum-group element concentrations. Economic Geology, 1999, 94(2): 165～183
Maier W D, Li C S,De Wall S A. Why are there no major Ni-Cu sulfide deposits in large layers mafic-ultramafic intrusions? Canada Mineral, 2001,3:547～556
Mao J W, Goldfarb G J, Wang Y T, et al. Late Paleozoic base and precious metal deposits, East Tianshan, Xinjiang, China: Charateristics and geodynamic setting. Episodes, 2005, 28(1): 23-36
Mao J W, Konopelko D, Seltmann R, et al. Postcollisional age of the Kumtor gold deposit and timing of Hercynian events in the Tien Shan, Kyrgyzstan. Economic Geology, 2004, 99(8): 1771-1781
Mattey D, Lowry D, Macpherson C. Oxygen isotope composition of mantle periotite. Earth Planet. Earth and Planetary Science Letters, 1994, 128: 231～241
McDonough W F, Sun S S. The composition of the earth. Chemical Geology, 1995,120 : 233～253 Mckenzie D, O'Nions R K. Partial melt distributions from inversion of rare earth element concentrations. Journal of petrology, 1991,32:1021～1091
Mckenzie D,Bickle M J. The volume and composition of melt generated by extension of the lithosphere. Journal of petrology,1988,29:53～72
Mckenzie D. Cratonic, circumeratonic and oceanic mantle domians beneath the western United states. Journal of geophysical research, 1989,94:7899～7915
Menzies M A. Archaean, Proterozoic, and Phanerzoic lithospheres. In: Menzies M A, eds.Continental mantle. New York: Oxford Science Publications,1990,67～86
Miyashiro A. Volcanic rock series in island arcs and active continental margins. American Journal of Science, 1974, 274: 321～355
Morimoto N. Nomenclature of pyroxenes. Mineralogical Magazine,1988,52: 535～550 Naldrett A J. Magmatic sulfide deposits. Springer Berlin. 2004b, 128: 303-311
Naldrett A J. Magmatic Sulphie Deposits. New York: Oxford University Press. 1989.1～186
Naldrett A J. An overview of Ni-Cu mineralization with conclusions guide in exploration. InternationalGeological correlation program IGCP479 short course notes, 2004a, 154～164
Naldrett A J. Key factors in the genesis of Noril'sk, Sudbury, Jinchuan, Voisey's Bay and other world-classNi-Cu-PGE deposits: implication for exploration. Australian Journal of Earth Sciences, 1997,44: 281～315
Naldrett A J. Nickle sulphide deposits: Their classification and genesis with special emphasis on deposits ofvolcanic association. Canadian Mining and Metallurgical Bull,1973,66: 45～63
Naldrett A J. World-class Ni-Cu-PGE deposits: key factors in their genesis. Mineralium Deposita, 1999,34:227～240
Neal C R, Mahoney J J, Chazey W J. Mantle sources and the highly variable role of continentallithosphere in basalt petrogenesis of the Kerguelen Plateau and Broken Ridge LIP: resultsfrom ODP Leg 183. Journal of petrology, 2002, 43: 1177～1205
Peltonen P. Petrogenesis of ultramafic rocks in the Vammala Nickel Belt: Implication for crustal evolution ofthe early Proterozoic Svecofennian arc terrane. Lithos,1995,34:253～274
Qin Kezhang, Zhang Lianchang, Xiao Wenjiao,et al. Overview of major Au, Cu, Ni and Fe deposits andmetallogenic evolution of the eastern Tianshan Mountains, Northwestern China. in: Mao J W, Goldfarb R J,Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolution and Metallogeny of the Chinese Altayand Tianshan,IAGOD Guidebook Series 10. London:2003, 227～248
Rehkamper M , Halliday A N , Fitton J G ,et al. Ir, Ru, Pt in basalts and komatiites: New constraints for thegeochemical behavior of the platinum-group elements in the mantle. Geochimical et cosmchimicaacta, 1999,63(22):3915～3934
Ripley E M, Lightfoot P C, Li C S , et al . Sulfur isotopic studies of continental flood in the Noril'sk region:implications for the association between lavas and ore-bearing intrusions. Geochimical et cosmchimicaacta, 2003,67 (15): 2805～2817
Ripley E M,Alawi J A .Petrogenesis of pelitic xenoliths at the Babbitt Cu-Ni deposit , Duluth Complex,Minnesota, USA. Lithos, 1988,21: 143～159
Roeder P L, Emslie R F. 1970. Olivine-liquid equilibrium. Contributions to Mineralogy and Petrology,1970,29:275～289
Rollinson H R. Using geochemical data: evolution, presentation, interpretation. New York:Longman Science Technology. 1993.48～51
Sakuyama M. Petrology of arc volcanic rocks and their origin by mantle diapers. Journal ofVolcanology and Geothermonology Research, 1983,18: 297～320
Saunders A D, Norry M J,Tarney J. Origin of MORB and chemically depleted mantle reservoirs:trace element constraints. Journal of Petrology (Special Lithosphere Issue),1988,425～445
Schmidt M W. Amphibole composition in tonalite as a function of p ressure: An experimentalcalibration of the Al-in-hornblende barometer. Contributions to Mineralogy and Petrology,1992,110: 304-310.
Seghedi I, Downes H, Vaselli O, et al. Post-collisional Tertiary–Quaternary mafic alkalic magmatism in theCarpathian–Pannonian region: a review. Tectonophysics,2004, 393:43～62
Seng?r A M C, Natal'in B A, Burtman V S. Evolution of the Altaid tectonic collage and Paleozoic crustalgrowth in Eurasia. Nature, 1993, 364: 209-304
Shima H, Naldrett A J. Solubility of sulfur in an ultramafic melt and the relevance of the system Fe-S-O.Economic geology, 1975,70: 960～967
Simkin T, Smith J V. Minor element distribution in olivine. Journal of Geology, 1970, 78: 304～325
Still P, Unruh D M, Tatsumoto. Pb, Sr, Nd and Hf isotopic evidence of multiple for Oahu, Hawwiibasalt. Nature,1983,304: 25-29
Stolz A J, Jochum K P, Hofmann A W. Fluid-and melt-related enrichment in the subarc mantle;evidence fromNb/Ta variations in island-arc basats. Geology,1996, 24:587～590
Sun S S, de Waal S A, Hoatson D M,et al. Use of geochemistry as a guide to platinum group elementpotentials of mafic-ultramafic rocks: examples from the weat Pilbara Block and Halls Creek Mobile Zone,western Australia. Precambrian Research,1991,50:1～35
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.Geological Society. London:Special Publication, 1989, 42: 313～345
Taylor S R, Mclennan S M. 1985. The continental crust: its composition and evolution. London: BlackwellScientific Publications,1985. 1～312
Thirlwall M F, Smith T E, Graham A M. High field strength element anomalies in arc lavas: Source or process?Journal of Petrology,1994,35: 819～838
Thompson R N. Some high-pressure pyroxenes. Mineralogical Magazine, 1974, 39: 768～787
Vogt J H L. Geenetischen classification der durch magmatische differentions processe under durchprevinathloyse entslandenen erzoskommen. Z. Ponkt. Geol., 1894, 381-399
Wendlandt R F. Sulphide saturation of basalt and andesite melts at high pressures and temperature. Americanmineralogist,1982,67: 877～885
Wilson M. Igneous Petrogenesis, London: Unwin Hyman, 1989
Windley B F, Allen M B, Zhang C, et al. Paleozoic accretion and Cenozoic re-deformation of the Chinese TienShan Range, Central Asia. Geology, 1990, 18:128-131
Wu F Y, Wilde S A, Zhang G L, et al. Geochronology and petrogenesis of the post-orogenicCu–Ni sulfide-bearing mafic–ultramafic complexes in Jilin Province, NE China. Journal ofAsian Earth Sciences, 2004, 23:781～797
Xiao W J, Zhang L C, Qin K Z, et al. Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China): Implications for the continental growth of Central Asia. American Journal of Sciences, 2004,304:370-395
Yan Shenghao, Zhang Zhaochong, Wang Denghong, et al. 2003. Kalatongke magmatic copper-nickl sulfidedeposit. in: Mao J W, Goldfarb R J, Seltmann R, Wang D H, Xiao W J., Hart C J, eds. Tectonic Evolutionand Metallogeny of the Chinese Altay and Tianshan, IAGOD Guidebook Series 10. London:2003, 131～151
Zhou, M F, Leshen, C M., Yang, Z X.,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. Chemical Geology,2004, 209,233-257
Zindler A, Hart S R. Chemical dynamics. Ann. Rev. Earth Planetary Science Letters, 1986, 14: 493～571
Zou, H B, Zindler, A, Xu, X S, et al. Major, trace element, and Nd, Sr and Pb isotope studies ofCenozoic basalts in SE China: mantle sources, regional variations, and tectonic significance.Chemical Geology, 2000, 171: 33～47
白云来. 新疆哈密黄山一镜儿泉镍铜成矿系统的地质构造背景.甘肃地质学报, 2000,9(2): 1-7
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.新疆地质,1993,11(1):34一42
柴凤梅, 张招崇,毛景文, 等. 中天山白石泉镁铁-超镁铁质岩体岩石学与矿物学研究. 岩石矿物学杂志, 2006, 25(1):1～12
车自成, 刘洪福, 刘良,等.中天山造山带的形成与演化. 北京: 地质出版社,1994
陈丹玲, 刘良, 车自成,等.中天山骆驼沟火山岩的地球化学特征及其构造环境. 岩石学报,2001,17(3): 378～384
陈光远, 孙岱生, 殷辉安. 成因矿物学与找矿矿物学. 四川:重庆出版社, 1984.1～874
陈浩琉,吴水波,傅德彬,等. 镍矿床. 北京:地质出版社, 1993,1-199
陈衍景.中国区域成矿研究的若干问题及其与陆陆碰撞的关系. 地学前缘,2002,9(4):319～328
陈衍景.中国西北地区中亚型造山—成矿作用的研究意义和进展.高校地质学报,2000,6(1):17～22
陈毓川, 赵 逊, 张之一, 等.世纪之交的地球科学-重大地学领域进展[M] .北京:地质出版社,2000
陈毓川等,1995,阿尔泰黄金有色金属开发区成矿地质条件与矿产资源评价研究,305科研报告
董传万, 徐夕生, 陈小明, 等. 福建平潭角闪辉长岩结晶过程的矿物学记录. 矿物学报,1997,17(3): 285～290
董云鹏, 周鼎武, 张国伟.东秦岭富水基性杂岩体地球化学特征及其形成环境.地球化学,1997,26(3):79～88
范育新,张铭杰.超大型铜镍硫化物矿床研究进展. 甘肃地质学报,1999,8 (2): 47～52方国庆.新疆东部大地构造特点及演化. 西北地质,1991,1-12
冯益民. 新疆西部构造发展史. 中国北方板块构造文集(第一集). 北京: 地质出版社,1986.
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. 兰州大学学报(自然科学版), 1993a, 29(4): 236～240
傅学明, 郭原生, 张铭杰, 等. 新疆黄山镁铁-超镁铁杂岩体化学成分特征及其含矿性关系. 兰州大学学报(自然科学版), 1993b,29(3): 213～221
高怀忠. 新疆坡北基性-超基性岩带1 号岩体地质特征及其含矿性研究. 地球科学-中国地质大学学报, 1992,17(4): 391～401
葛文春,林强,孙德有.大兴安岭中生代玄武岩的地球化学特征: 壳幔相互作用的证据.岩石学报,1999,15(3):396～407
顾连兴, 苟晓琴 , 张遵忠,等.东天山一个多相带高铷氟花岗岩的地球化学及成岩作用. 岩石学报, 2003,19(4): 585～600
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. 岩石学报, 1994. 10 (4): 339～356
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. 科学通报, 2004, 49(22): 2324～2328
韩宝福,何国琦,王式洸,等. 新疆北部后碰撞幔源岩浆活动与陆壳纵向生长.地质论评,1998,44, 396～406
韩宝福,何国琦,王式洸. 后碰撞幔源岩浆活动底垫作用及准噶尔盆地基底的性质.中国科学(D辑),1999,29(1):16～21
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.地质学报,2006,80(1):74～89
何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化与成矿. 乌鲁木齐: 新疆人民出版社,香港: 香港文化教育出版社,1994
洪大卫,王式洸,谢锡林,等. 兴蒙造山带正εNd值花岗岩的成因和大陆地壳生长. 地学前缘, 2000,7:441～456
洪大卫,王式洸,谢锡林,等.从中亚正εNd 值花岗岩看超大陆演化和大陆地壳生长的关系.地质学报,2003,77(2):203～209
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).北京:地质出版社, 1990
胡素芳.攀西地区红格、新街岩体的岩石地球化学特征.博士学位论文.北京:中国科学院地质地球物理研究所,2001
黄智龙,王联奎.云南老王寨金矿区黄斑岩的地球化学.地球化学,1996,25(3):5-263
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. 矿物岩石, 1984, 4(3)
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. 北京: 地质出版社, 1998, 202-221
李锦轶, 王克卓, 李文铅,等.东天山晚古生代以来大地构造与矿产勘查. 新疆地质, 2002, 20 (4) : 296～301
李锦轶,徐新.新疆北部地质构造和成矿作用的主要问题.新疆地质,2004,22(2):119～124
李锦轶.试论中国新疆准噶尔山系古生代板块构造演化.见肖序常、汤耀庆主编.古中亚复合巨型缝合带南缘构造演化.北京:北京科学技术出版社,1991,92-108
李锦轶.新疆东部新元古代晚期和古生代构造格局及其意义.地质论评,2004,50(3):304-322.
李凯明 , 赵海玲 , 邓晋福 . 2002 . 山西平顺岩体岩石学/矿物学特征及角闪石成因 [J] . 北京地质 , 14 (4): 41-47.
李曙光, 聂永红, 郑双根,等. 俯冲陆壳与上地幔的相互作用——Ⅰ. 大别山同碰撞镁铁-超镁铁岩的主要元素及痕量元素地球化学. 中国科学 (D 辑), 1997,27 (6): 488～493
李文渊. Re-Os同位素体系及其在岩浆Cu-N i-PGE矿床研究中的应用. 地球科学进展 , 1996,11 (6): 580～584
李先梓, 李行, 洛长义, 等. 新疆铂族元素成矿地质条件及找矿方向研究. 中国地质科学院西安地质矿产研究所所刊, 1991, 33: 1～93
李献华, 周汉文, 韦刚健, 等, 滇西新生代超钾质煌斑岩的元素和 Sr-Nd 同位素特征及其对岩石圈地幔组成的制约. 地球化学, 2002,31(1):26～35
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. 矿床地质, 1992, 11 (4): 307～314
刘德权,唐延龄,周汝洪.中亚古生代造山带成矿作用基本特征.西北地质,2001,34(2):1-10
刘德权. 新疆板块构造与矿产分布.西北地质,1983,4(2):1～12
刘民武.中国几个镍矿床的地球化学比较研究:博士学位论文.西安:西北大学, 2003
刘月星.铜镍硫化物矿床成矿作用及成矿模式研究.矿产与地质,1997,11(4):225～231
龙小平, 王立社, 余能. 东昆仑山清水泉镁铁质-超镁铁质岩的地球化学特征. 地质通报, 2004,23 (7): 664-669
马鸿文. 结晶岩热力学概论. 北京:高等教育出版社, 2001.1～297
马鸿文.介绍改进的单斜辉石地质温度计公式. 地质科技情报, 1985,4(2): 82～84
马瑞士,舒良树,孙家齐,等.东天山构造演化与成矿.北京:地质出版社, 1997
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, 1997, 17(增刊): 35～47
马润则, 肖渊甫. 米仓山地区晋宁期基性超基性侵入岩中造岩矿物研究. 成都理工学院学报, 2001, 28 (1): 34～39
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. 矿床地质, 2002,21(4): 323～330
毛景文,Franco Pirajno,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:主要特点及与地幔柱关系(待发表). 2006.
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.地质学报,2005,79(3):342-372
倪志耀, 卫管一. 新疆东部基性超基性岩的地质地球化学特征. 矿物岩石, 1995, 15(1):8～17
倪志耀. 黄山东镁铁超镁铁杂岩中的辉石化学成分研究. 岩石矿物学杂志, 1994, 13(1):55～66
倪志耀. 新疆哈密黄山东镁铁-超镁铁杂岩体成因探讨. 西北地质, 1992, 13(2):9～16
倪志耀. 新疆哈密黄山东镁铁一超镁铁杂岩体中橄榄石的化学成分及其岩石学意义.1991,1(3):40～47
倪志耀. 岩浆深渊分异在新疆黄山杂岩体成岩成矿中的作用. 成都地质学院学报, 1993, 20(2):33～39
帕拉提·阿布都卡迪尔,黄建华,吴兆宁.喀拉通克铜镍矿床伴生贵金属赋存富集规律.新疆工学院学报,1996,17(2):79～85
潘长云,王润民,赵昌龙.新疆喀拉通克 Y_1 含矿岩体的岩石化学特征及其与成矿的关系.岩石学报,1994,10(3):261～274
秦克章.新疆北部中亚型造山与成矿作用.博士后研究报告.北京:中国科学院地质与地球物理研究所地质学博士后流动站,2000
邱家骧, 廖群安. 中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息. 岩石矿物学杂志, 1987,6(1):56-63
邱家骧, 林景仟.岩石化学. 北京: 地质出版社,1991.140～156
冉红彦, 肖森宏.喀拉通克含矿岩体的微量元素与成岩构造环境. 地球化学, 1994,23(4):392-401
申茂德. 东天山香山铜镍矿区构造特征与成岩成矿. 新疆地质, 2003, 21(2):195～198
师占义. 橄榄石标型特征及其找矿意义. 西北地质科学, 1994,15(1):11～16
舒良树,卢华复,印栋浩,等.新疆北部古生代大陆增生构造.新疆地质,2001,19(1):59～63
孙传敏. 四川盐边元古代蛇绿岩中辉石的成因矿物学及其大地构造意义. 矿物岩石, 1994, 14(3): 1～15
汤耀庆, 高俊, 赵民,等.西南天山蛇绿岩与蓝片岩. 北京: 地质出版社,1995
汤中立,李文渊. 金川铜镍硫化物模式及地质特征对比. 北京 :地质出版社.1995
汤中立. 超大型岩浆硫化物矿床的类型及地质对比意义.甘肃地质学报 ,1992,1(1):24～47
王崇义, 石长运, 王晓亭. 黄山基性-超基性岩体成岩机制及其含矿性初步探讨. 新疆地质, 1986, 4(1): 1～11
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. 矿床地质, 2000, 19(2):147～155
王登红, 陈毓川, 徐志刚, 李天德,傅旭杰. 阿尔泰成矿省的成矿系列及成矿规律. 北京: 原子能出版社,2002.1～492
王京彬, 徐新. 新疆北部后碰撞构造演化与成矿. 地质学报, 2006, 80: 23～31
王京彬,李博泉,张积斌,等.额尔齐斯聚矿带金铜成矿条件及找矿预测.北京:冶金工业出版社,1999.
王瑞廷, 毛景文, 赫英等.煎茶岭硫化镍矿床的铂族元素地球化学特征及其意义 . 岩石学报, 2005,21(1): 219～226
王瑞廷, 毛景文, 柯洪,等. 铜镍岩浆硫化物矿床成矿作用研究综述. 矿产与地质, 2003, 17 (增刊): 281～284
王瑞廷. 煎茶岭与金川镍矿床成矿作用比较研究: [博士学位论文]. 西安: 西北大学, 2002
王润民, 王志辉. 新疆喀拉通克一号岩体及铜镍硫化物矿床地质特征.中国地质科学院院报, 1993, 95～102
王润民,李思楚.新疆哈密黄山东铜镍硫化物矿床成岩成矿物理化学条件.成都地质学院,1987, 14(3):1～10
王润民、赵昌龙.新疆喀拉通克一号铜镍硫化物矿床.北京:地质出版社,1991. 1～298
王有标. 新疆铜镍硫化物矿床地基本地质特点.1990, 8: 305～320
王玉往, 王京彬,王莉娟,等.新疆哈密黄山地区铜镍硫化物矿床的稀土元素特征及意义.岩石学报,2004,20(4):935-948
王中刚,赵振华,邹天人,等.新疆北部花岗岩类的成因类型及其成矿作用.见:涂光炽主编, 新疆北部固体地球科学新进展.北京: 科学出版社,1993. 127～136
吴福元,江博明,林强.中国北方造山带造山后花岗岩的同位素特点与地壳生长意义.科学通报,1997,42(20):2188～2192
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. 地质学报, 79(4):498～502
吴利仁. 论中国基性岩、超基性岩的成矿专属性. 地质科学, 1963, (1):29～41
吴平霄, 吴金平, 李才伟,等.斜长石韵律环带的结晶速率方程及其动力学机制. 岩石学报, 1998,14(3): 388～394
吴平霄, 吴金平, 肖文丁, 等. 斜长石环带的成因机制. 地质地球化学, 1997,(4): 40～49
夏林圻,夏祖春,徐学义,等.天山石炭纪大火成岩省与地幔柱.地质通报,2004,23(9-10):903～910
夏林圻,张国伟,夏祖春,等.天山古生代洋盆开启、闭合时限的岩石学约束—— 来自震旦纪、石炭纪火山岩的证据. 地质通报,2002,21(2):56-62.
夏祖春, 徐学义, 夏林圻,等.天山石炭-二叠纪后碰撞花岗质岩石地球化学研究。西北地质,2005, 38(1):1～14
肖序常, 汤耀庆. 古中亚复合巨型缝合带南缘构造演化. 北京: 北京科学技术出版社, 1991, 1-29
肖序常,汤耀庆,冯益民,等. 新疆北部及其邻区大地构造.北京: 地质出版社,1992. 1～169
肖序常.从扩张速率试论蛇绿岩的类型划分. 岩石学报,1995, 11(增刊):10～23
肖渊甫, 马润则, 魏显贵, 等. 米仓山澄江期基性侵入杂岩特征及其成因探讨. 成都理工学院学报, 1998, 25(4): 537～-542
熊小林,赵振华,白正华,等.西天山阿吾拉勒埃达克质岩石成因:Nd 和 Sr 同位素组成限制.岩石学报,2001,17(4):514～522
熊永良. 铼-锇同位素体系对揭示矿质来源的作用. 地学前缘 ,1994,1 (3-4): 199～203
徐学义, 夏林沂, 夏祖春, 等. 岚皋早古生代碱质煌斑杂岩地球化学特征及成因探讨. 地球学报, 2001,22 (1): 55～60
徐学义,马中平,夏祖春等.天山石炭—二叠纪后碰撞花岗岩的Nd、Sr、Pb 同位素源区示踪.西北地质,2005,38(2):1～18
闫峻, 陈江峰, 喻钢,等.长江中下游晚中生代中基性岩的铅同位素特征 : 富集地幔的证据. 高校地质学报, 2003,9(2): 195～206
杨炳滨. 新疆北部岩浆型铜镍硫化物矿床控矿因素的研究. 矿产与地质, 1994, 8: 330～333
杨甲全, 钟莉, 邓刚. 北山地区坡北1号、10号基性一超基性岩体成矿预测及找矿方向. 新疆地质, 2002, 20(3): 214～218
杨学明,杨晓勇,陈双喜.岩石地球化学.合肥:中国科学技术大学出版社,2000.1～243
永文富.新疆哈密土墩基性—超基性岩岩体特征及其含矿性研究. 新疆有色金属, 2002, (3):1～6
张旗. 镁铁-超镁铁岩与威尔逊旋回. 岩石学报, 1992, 8(2):168～176
张儒瑗,从柏林.矿物温度计和矿物压力计. 北京:地质出版社,1983.1～280
张树明, 王方正.玄武岩在研究岩石圈深部过程及构造背景中的应用. 地球科学进展, 2002,17 (5): 685～692
张湘炳,隋静霞,李志纯,等.额尔齐斯构造带构造演化与成矿系列.北京:科学出版社,1996.
张招崇 , 阎升好, 陈柏林, 等. 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. 岩石矿物学杂志, 2003,22(3): 217～224
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. 吉林大学学报(地球科学版), 2003,33 (2): 130～134
张招崇,闫升好,陈柏林,等.阿尔泰铜矿带东段找矿靶区优选及评价,国家305项目2001BA609A-07-02专题科研报告,2005
张招崇,闫升好,陈柏林,等.阿尔泰造山带南缘镁铁质—超镁铁质杂岩体的 Sr、Nd、O 同位素地球化学及其源区特征探讨.地质论评,2006,52(1):38～42
张作衡,柴凤梅,杜安道,等. 新疆喀拉通克铜镍硫化物矿床 Re_Os 同位素测年及成矿物质来源示踪. 岩石矿物学杂志, 2005, 24(4):285～293
赵振华, 王中刚, 邹天人, 等. 新疆乌伦古富碱花岗岩成因探讨. 地球化学, 1996, 25: 205～220
郑详身. 西南极利文斯顿岛中部中一新生代火山岩的岩相学和矿物学特征. 南极研究(中文版),1995,7(1): 1～16
支霞臣, 靳永斌, 孟庆,等. 大别山北部饶拔寨超镁铁岩体微量元素地球化学. 岩石学报, 2004,20(3): 463～472
周英森. 喀拉通克铜镍硫化矿床Y_1号岩体岩相划分及岩石特征. 新疆地质, 1987, 5(3):9～15
朱维光. 扬子地块西缘新元古代镁铁质—超镁铁质岩的地球化学特征及其地质背景——以盐边高家村杂岩体和冷水箐101号杂岩体为例:[博士学位论文].北京:中国科学院地球化学研究所,2004
朱文斌, 马瑞士, 王赐银. 论新疆东部黄山-镜儿泉杂岩带的构造属性. 地质科学, 1996, 31, (1): 22～31
朱永峰.硫在岩浆熔体中的溶解行为综述.地质科技情报,1998,17(2):35～38
竺国强, 杨树锋, 陈汉林.东疆香山铜镍含矿镁铁超镁铁杂岩体控岩控矿构造探讨. 1995, 10(3):1～13
邹天人,曹惠志,吴柏青.新疆阿尔泰造山花岗岩和非造山花岗岩及其判别标志.地质学报,1988,62(3):228～243