云南武定左所辉绿岩铂族元素地球化学、Pb同位素及其地质意义
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摘要
古元古代晚期至中元古代早期,西南康滇地区发生过一次强烈的构造、岩浆及成矿事件,即昆阳裂谷,以广泛出露1.8~1.5 Ga基性岩浆岩及铁铜矿床为重要标志。文章报道了滇中武定地区左所辉绿岩的岩石化学、微量元素、Pb同位素及铂族元素地球化学特征,通过铂族元素地球化学对昆阳裂谷期的岩石圈演化、壳幔相互作用进行了探讨。左所辉绿岩相对富碱(w(Na_2O+K_2O)平均为3.55%),低w(Si O_2),较高的w(Ti O_2)(均值为3.30%)、w(P_2O_5)(平均值0.35%),Ca O/Ti O_2比值(平均值为2.4)及Al_2O_3/Ti O_2比值(平均值为3.4)低,具有典型地幔热柱玄武岩的岩石化学特征。左所辉绿岩微量元素中相对富集大离子半径元素,高场强元素弱亏损,稀土元素中出现弱的Eu负异常,反映了斜长石的轻度结晶分异。辉绿岩具有较高的铂族元素含量,PPGE和IPGE明显分异,PGE原始地幔标准化配分曲线呈较明显的左陡倾型。辉绿岩的Cu/Pd比值均低于原始地幔值,表明原始岩浆S不饱和,亦未发生硫化物的熔离过程,较高的PGE含量可能与初始岩浆本身的S含量较高有关。高的Pd/Ir比值可能与IPGE在部分熔融过程中更倾向于残留相以及岩浆演化早期铬铁矿和橄榄石的结晶分异有关。低程度的地幔部分熔融、Pb同位素特征暗示左所地区辉绿岩的形成过程:陆内裂谷环境下,富硫的原始岩浆在上升过程中受到较少下地壳物质的混染,侵位至浅表并较快冷却,形成辉绿岩。
Late Paleoproterozoic and Early Neoproterozoic Kunyang rift was an intense tectonic, magmatic and metallogenic event, which was characterized by the formation of plenty of 1. 8 ~ 1. 5 Ga basic rocks and Fe-Cu deposits in Kangdian area, Southwest China. Much research work has been carried out on the petrogeochemistry and geochemistry of mineral deposits for investigating geological background and mineralization of Kunyan rift. In this paper, the characteristics of petrochemistry, trace elements, Pb isotope and platinum group elements( PGE) of diabases at Zu osuo in central Kangdian area are reported to discuss the lithospheric evolution and interaction of mantle and crust through PGE geochemistry. The diabases have the typical chemical characteristics of mantle plume basalts, such as rich alkali( the average of w( Na_2 O + K_2O) is 3. 55%), low w( Si O_2), high w( Ti O_2)( averagely 3. 30%) and w( P_2O_5)( averagely 0. 35%), and low ratios of Ca O/Ti O_2( 2. 4% on average) and Al_2O_3/Ti O_2( 3. 4 on average).The Zuosuo diabases are relatively enriched in large ion radius elements, with weak depletion of high field strength elements and weak negative Eu anomalies in REEs. The diabases have high content of platinum group elements with obvious differentiation of PPGE( Pt, Pd and Rh) and IPGE( Os, Ir and Ru), and the PGE primitive mantlenormalized patterns exhibit obvious left steep curve. Cu/Pd ratios of diabases are lower than those of primary mantle, indicating that the primary magma was S-unsaturated magma without PGE-enriched sulfide separation. The high Pd/Ir ratio of diabases may be related to that IPGEs are more likely to be hosted in residual phase in partial melting, and crystallization differentiation of chromite and olivine for the primary magma in the early stage. Low partial melting of upper mantle and Pb isotopes indicate the formation process of the basite in Zuosuo: In the environment of inner continental rift, original basic S-rich magma was contaminated by lower crust materials during the rising process, and was then emplaced near the surface of the crust, where it became cool quickly, thus forming the diabases.
Late Paleoproterozoic and Early Neoproterozoic Kunyang rift was an intense tectonic, magmatic and metallogenic event, which was characterized by the formation of plenty of 1. 8 ~ 1. 5 Ga basic rocks and Fe-Cu deposits in Kangdian area, Southwest China. Much research work has been carried out on the petrogeochemistry and geochemistry of mineral deposits for investigating geological background and mineralization of Kunyan rift. In this paper, the characteristics of petrochemistry, trace elements, Pb isotope and platinum group elements( PGE) of diabases at Zu osuo in central Kangdian area are reported to discuss the lithospheric evolution and interaction of mantle and crust through PGE geochemistry. The diabases have the typical chemical characteristics of mantle plume basalts, such as rich alkali( the average of w( Na_2 O + K_2O) is 3. 55%), low w( Si O_2), high w( Ti O_2)( averagely 3. 30%) and w( P_2O_5)( averagely 0. 35%), and low ratios of Ca O/Ti O_2( 2. 4% on average) and Al_2O_3/Ti O_2( 3. 4 on average).The Zuosuo diabases are relatively enriched in large ion radius elements, with weak depletion of high field strength elements and weak negative Eu anomalies in REEs. The diabases have high content of platinum group elements with obvious differentiation of PPGE( Pt, Pd and Rh) and IPGE( Os, Ir and Ru), and the PGE primitive mantlenormalized patterns exhibit obvious left steep curve. Cu/Pd ratios of diabases are lower than those of primary mantle, indicating that the primary magma was S-unsaturated magma without PGE-enriched sulfide separation. The high Pd/Ir ratio of diabases may be related to that IPGEs are more likely to be hosted in residual phase in partial melting, and crystallization differentiation of chromite and olivine for the primary magma in the early stage. Low partial melting of upper mantle and Pb isotopes indicate the formation process of the basite in Zuosuo: In the environment of inner continental rift, original basic S-rich magma was contaminated by lower crust materials during the rising process, and was then emplaced near the surface of the crust, where it became cool quickly, thus forming the diabases.
引文
Agiorgitis G and Wolf R.1978.Aspects of osmium,ruthenium and iridium content in some Greek chomites[J].Chemical Geology,23:267-272.
Aland O,Griffin W L and Lorand J P.2000.Non-chondritic distribution of the highly sidemphile elements in mantle sulphides[J].Nature,407:891-894
Ballhaus C and Ryan C G.1995.Platinum-group elements in the Merensky reef.ⅠPGE in solid solution in base metal sulfides and downtemperature equilibration history of Merensky ores[J].Contrb.Mineral.Petrol.,122:241-251.
Barnes S,Naldrett A J and Gorlon M P.1985.The origin of the fractionation of platinum-group elements in terrestrial magmas[J].Chemical Geology,53:303-323.
Barnes S J and Naldrett A J.1987.Fractionation of the platinum-group elements and gold in some komatiites of the Abitibi greenstone blet,Northern Ontario[J].Econ.Geol.,82(1):165-183.
Barnes S J,Boyd R,Korneliussern A,Nilsson L P,Often M,Pedersen RB and Robins B.1988.The use of mantle normalization and metal ratios in discriminating between the effects of partial melting,crystal fractionation and sulfide segregation on platinum-group elements,gold,nicked and copper:Examples from Norway[M].In:Prichard H M,Potts P J,Bowles J F W,et al.eds.Geo-platinum 87.London:Elsevier.113-143.
Barnes S J.1990.The use of metal ratios in prospecting for platinumgroup element deposits in mafic and ultramafic intrusions[J].Journal of Geochemical Exploration,37:91-99.
Barnes S J and Picard C P.1993.The behavior of platinum-group elements during partial melting,crystal fractionation,and sulphide segregation:An example from the Cape Smith fold belt,northern Quebec[J].Geochimica et Cosmochimica Acta,57:79-87.
Barnes S J and Maier W D.1999.The fraction at ion of Ni-Cu and the noble metals in silicate and sulphide liquids[J].Geological association of Canada Short Course,13:69-106.
Biugmann G E,Naldrett A J.Asif M,Lightfoot P C,Gorbachev N S and Fedorenko V A.1993.Siderophile and chalcophile metals as tracers of the evolution of the Siberian Traps in the Noril'sk region,Russia[J].Geochimica et Cosmochimica Acta,57:2001-2018.
Brugmann G E,Arndt N T,Hoffmann A W and Tobschall H J.1987.Noble metal abundances in komatiite suites form Alexo,Ontario,and Corgana Island,Columbia[J].Geochimica et Cosmochimica Acta,51:2159-2169.
Capobianco C JHervig R Land Darke M J.1994.Experiments on Ru,Rh and Pd compatibility for magnetite and hematite solid solutions crystallized from silicate melts[J].Chemical Geology,113:23-44.
Chen W T,Zhou M F and Zhao X F.2013.Late paleoproterozoic sedimentary and mafic rocks in the Hekou area,SW China:Implication for the reconstruction of the Yangtze block in Columbia[J].Precambrian Research,231:61-77.
Crocket J H and Teruta Y.1977.Palladium iridium and gold contents of nafic and ultramafic rocks drilled from the mid-Atlantic ridge,Leg37,Deep Sea Drilling Project[J].Canadian Journal of Earth Sciences,14:777-784.
Garuti G,Gorgoni C and Sighinolfi G P.1984.Sulfide mineralogy and chalcophile and siderophile element aboundances in the Ivrea-Verbano mantle peridotites(western Italian Alps)[J].Earth Planetary Science Letters,70:69-87.
Garuti G,Fershtater G,Bea F,Montero P,Pushkarev E V and Zaccarini F.1997.Platinum-group elements as petrological indicators in maficultramafic complexes of the central and southern Urals:Preliminary results[J].Tectonophysics,276:181-194.
Geng Y S,Liu Y Q,Gao L Z,Peng N and Jiang X J.2012.Geochronology of the Mesoproterozoic Toang'an Formation in southwestern margin of Yangtze craton:New evidence from zircon LA-ICP-MS U-Pb ages[J].Acta Geologica Sinica,86(9):1479-1490(in Chinese with English abstract)..
Gong L and He Y T.1996.The Proterozoic rift type copper in Yunnan Province[M].Beijing:Press of Metallurgy Industry.2-28(in Chinese).
Green M G,Sylvester P J and Buick R.2000.Growth and recycling of early Archaean continental crust:Geochemical evidence from the Coonterunah and Warrawoona Groups,Pilbara Craton,Australia[J].Tectonophysics,322(1):69-88.
Greentree M R and Li Z X.2008.The oldest known rocks in south-western China:SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group[J].Journal of Asian Earth Sciences,33(5-6):289-302.
Guan J L,Zhen L L,Liu J H,Sun Z M and Cheng W H.2011.Zircon SHRIMP U-Pb dating of diabase from Hekou,Si Chuan Province,China and its geological significance[J].Acta Geologica Sinica,85(4):482-490(in Chinese with English abstract).
Guo Y,Wang S W,Sun X M,Liao Z W,Wang Z Z,Zhou B G and Yang B.2014a.Zircon U-Pb age of the Paleoproterozoic diabase from the Yinachang iron-copper deposit,Yunnan Province,and its geological implication[J].Geotectonica et Metallogenia,38(1):208-215(in Chinese with English abstract).
Guo Y,Wang S W,Sun X M,Wang Z Z,Yang B,Liao Z W,Zhou BG,Jiang X F,Hou L and Yang B.2014b.The Paleoproterozoic breakup event in the southwest Yangtze block:evidence from U-Pb zircon age and geochemistry of diabase in Wuding,Yunnan Province,SW China[J].Acta Geologica Sinica,88(9):1651-1655(in Chinese with English abstract).
Hauri E H.1996.Major-element variability in the Hawaiian mantle plume[J].Nature,382(1):415-419.
Hou Z Q,Lu J R,Li H Y,Wang D H and LüQ T.1996a.Tectonic evolution of the Tethys in southwestern China:Is controlled by plume tectonics[J].Acta Geoscientia Sinica,17(4):439-453(in Chinese with English abstract).
Hou Z Q,Mo X X,Zhu Q W and Shen S Y.1996b.Mantle plume in the Sanjiang paleo-Tethyan region,China:Evidence from ocean-island basalts[J].Acta Geoscientia Sinica,17(4):343-361(in Chinese with English abstract).
Hou Z Q,Mo X X,Zhu Q W and Shen S Y.1996c.Mantle plume in the Sanjiang Paleo-Tethyan lithosphere:Evidence from mid-ocean radge basalts[J].Acta Geoscientia Sinica,17(4):362-375(in Chinese with English abstract).
Hua R M.1990.On the Kunyang aulacogen[J].Acta Geologica Sinica,4:289-301(in Chinese with English abstract).
Jiang S Y,Yang J H,Ling H F,Feng H Z,Chen Y Q and Chen J H.2003.Re-Os isotopes and PGE geochemistry of black shales and intercalated Ni-Mo polymetallic sulfide bed from the Lower Cambrian Niutitang Formation,South China[J].Progress in Natural Sciences,13(10):788-794.
Keays R R.1995.The role of komatiitic and picritic magmatism and S-saturation in the formation of the ore deposits[J].Lithos,34:1-18.
Lee D C,Halliday A N,Fitton J G and Poli G.1994.Isotopic variations with with distance and time in the volcanic islands of the Cameroon line:Evidence for a mantle plume origin[J].Earth and Planetary Science Letters,123:119-138.
Liao Z W,Wang S W,Yu Y S,et al.2010.The basement metallogenesis and prospecting direction of western margin of Yangtze Platform[R].Internal report of Chengdu Institute of Geology and Mineral Resourses.22-26(in Chinese).
Liu Q,Hou Q L,Zhou X H and Xie L W.2005.The distribution of platinum-group elements in gabbros from Zhujiapu Dabie orogen[J].Acta Petrologica Sinica,21(1):227-239(in Chinese with English abstract).
Maier W D,Barnes S J,De klerk W J,Teigler B and Mitchell A A.1996.Cu/Pd and Cu/Pt of silicate rocks in the Bushveld complex:Implications for platinum-group element exploration[J].Econ.Geol.,91:1151-1158.
Maier W D,Bames S J and Marsh J S.2003.The concentrations of the noblemetals in southern African flood-type basalts and MORB Implications for petrogenes is and magmatic sulphide exploration[J].Contributions to Mineralogy and Petrology,146:44-61.
Middlemost E A K.1994.Naming materials in magma/igneous rock system[J].Earth Sci.Rev.,37:215-224.
Mitchell R H and Keays R R.1981.Abundance and distribution of gold,palladium and iridium in some spinel and garnet lherzolites:Implication for the nature and origin of precious metal rich intergranular component in the upper mantle[J].Geochimca et Cosmochimica Acta,45:2425-2445.
Naldrett A J and Cabri L J.1976.Ultramafic and related rocks:Their classification and genesis with special reference to the concentration of nickel sulfides and platinum-group elements[J].Econ.Geol.,76:1131-1158.
Naldrett A J and Duke M.1980.Platinum metals in magmatic sulfide ores[J].Science,208:1417-1424
Oshin I O and Crocket J H.1982.Noble metal in Thetford mines ophiolite,Quebec,Canada.PartⅠ:Distribution of gold,iridium,platinum,and palladium in the ultramafic and gabbroic rocks[J].Econ.Geol.,77:1556-1570.
Pang X N,Zhao J X,Zhuang X Y,Zhen H X,Yang X H,Zhou G F and Tao D L.1985.Tectonics and rifting in kangdian region[M].Chongqing:Chongqing Publishing House.1-298(in Chinese with English abstract).
Qi L and Gregoire D C.2000.Determination of trace elements in twenty six Chinese geochemistry reference materials by inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research,24(1):51-63.
Song X Y,Hu R Z and Chen L M.2009.Geochemical natures of copper,nickel and PGE and their significance for the study of origin and evolution of mantle-derived magmas and magmatic sulfide deposits[J].Earth.Science Frontiers,16(4):287-305(in Chinese with English abstract).
Steiger R H and J8)ger E.1977.Subcommission on geochronology:Convention on the use of decay constants in geo-and cosmochronology[J].Earth and Planetary Science Letters,36(3):359-362.
Stein M and Hofmann A W.1992.Fossil plume head beneath the Arabian lithosphere[J]?Earth and planetary Science Letters,114(1):193-210.
Stern R A,Syme E C and Lueas S B.1995.Geochemistry of 1.9 Ga MORB-and OIB-like basalts from the Amisk collage,Flin Flon belt,Canada:Evidence for an intr-oceanic origin[J].Geochimica et Cosmochimica Acta,59(15):3131-3154.
Sun H,Qin K Z,Li J X,Teng D M,Fan X and Xiao Q H.2008.Constraint of mantle partial melting on PGE mineralization of mafic-ultramafic intrusions in Eastern Tianshan:Case study on Tulargen and Xiangshan Cu-Ni deposits[J].Acta Petrologica Sinica,24(5):1079-1086(in Chinese with English abstract).
Sun S S and Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalt:Implications for mantle composition and process[A].In:Saunders A D and Norry M J,eds.Magmatism in the Ocean Basins[C].Spc.Publ.Geol.Soc.Lond.,42:528-548.
Sun X M,Xiong D X,Wang S W,Shi G Y and Zhai W.2006.Platinum group elements(PGE)geochemistry of Mojiang Au-Nideposit and its constraint on ore genesis[J].25(4):438-446(in Chinese with English abstract).
Sun Z M,Yin F G,Guan J L,Liu J H,Li J M,Geng Q R and Wang LQ.2009.SHRIMP U-Pb dating and its stratigraphic significance of tuff zircons from Heishan formation of Kunyang Group,Dongchuan area,Yunnan Province,China[J].Geological Bulletin of China,28(7):896-900(in Chinese with English abstract).
Wang D B,Sun Z M,Yin F G,Wang L Q,Wang B D and Zhang W P.2012.Geochronology of the Hekou Group on the western margin of the Yangtze block:Evidence from zircon LA-ICP-MS U-Pb dating of volcanic rocks[J].Journal of Stratigraphy,36(3):630-635(in Chinese with English abstract).
Wang D B,Yin F G,Sun Z M,Wang L Q,Wang B D,Liao S Y,Tang Y and Ren G M.2013.Zircon U-Pb age and Hf isotope of Paleoproterozoic mafic intrusion on the western margin of the Yangtze block and their implication[J].Geological Bulletin of China,32(4):617-630(in Chinese with English abstract).
Wang S W,Sun X M,Shi G Y,Xiong D X and Zhai W.2006.Platinum group elements(PGE)geochemistry of Baimazhai Ni-Cu sulfide deposit and its constraints on the ore genesis[J].Acta Geologica Sinica,80(9):1474-1486(in Chinese with English abstract).
Wang S W,Sun X M,Shi G Y,Xiong D X and Zhai W.2007.Distinction of platinum group elements(PGE)geochemistry between the Jinbaoshan and Baimazhai magmatic sulfide deposits in Yunnan Province,China,and its implication for ore genesis[J].Acta Geologica Sinica,81(1):93-108(in Chinese with English abstract).
Wang S W,Jiang X F,Liao Z W,Yu Y S,Zhang H,Zhou B G,Wang Z Z,Li Y C,Yang B,Guo Y,Hou L and Lu S L.2011.Research report on metallogenesis and prospecting direction of basement in the southwest of Yangtze platform[M].Chengdu and Chengdu Institute of Mineral Resources.1-259(in Chinese).
Wang S W,Sun X M,Jiang X F,Qu W J,Liao Z W and Li C.2012.Re-Os isotopic age and mineralization setting of protosomatic chalcopyrites from Donghcuan copper deposit[J].Mineral Deposits,31(Supp.):609-610(in Chinese with English abstract).
Wang S W,Liao Z W,Sun X M,Jiang X F,Zhou B G,Guo Y,Luo MJ,Zhu H P and Ma D.2013a.Geochemistry of Paleoproterozoic diabases in the Dongchuan copper deposit,Yunnan,SW China:Response to breakup of the Columbia supercontinent in the Southwestern Margin of Yangtze block[J].Acta Geologica Sinica,87(12):1834-1852(in Chinese with English abstract).
Wang S W,Sun X M,Liao Z W,Qu W J,Yang B,Jiang X F,Li C and Li Y C.2013b.Platinum group elements and Re-Os isotope geochemistry of harzburgites form Caiziyuan nickel deposit in Huili county of Sichuan Province and its geological significance[J].Mineral Deposits,32(3):515-532(in Chinese with English abstract).
Wang S W,Jiang X F,Yang B,Sun X M,Liao Z W,Zhou Q,Guo Y,Wang Z Z and Yang B.2016.The Proterozoic tectonic movement In Kangdian area I:Kunyang Intracontinental Rift,mantle plume and its metallogenesis[J].Geological Review,62(6):1353-1377(in Chinese with English abstract).
Wang Y L,Zhang C J and Xiu S Z.2001.Th/Hf-Ta/Hf identification of tectonic setting of basalts[J].Acta Petrologica Sinica,17(3):413-421(in Chinese with English abstract).
Wang Z Z Guo Y,Yang B,Wang S W,Sun X M,Hou L,Zhou B G and Liao Z W.2013.Discovery of the 1.73 Ga Haizi anorogenic type granite in the western margin of Yangtze craton,and its geological significance[J].Acta Geologica Sinica,87(7):931-942(in Chinese with English abstract).
Weis D,Frey F A,Leyrit H and Gautier I.1993.Kerguelen archipelago revisited:Implication and isotopic study of the southeast province lavas[J].Earth and Planetary Science Letters,118:101-119.
Xiao L,Xu Y G and He B.2003a.Emei mantle plume-subcontinental lithosphere interaction:Sr-Nd and O isotopic evidences from low-Ti and high-Ti basalts[J].Geological Jounal of China Universities,9(2):207-217(in Chinese with English abstract).
Xiao L,Xu Y M,Mei H J and He B.2003b.Late Permian flood basalts at Jinping area and its relation to Emei mantle plume:Geochemical evidence[J].Acta Petrologica Sinica,19(1):38-48(in Chinese with English abstract).
Xiao L,Xu Y G,Mei H J and Yu R P.2003c.Petrogenesis of the basalts of Woniusi Formation at Baoshan area,Yunnan:Is it of mantle plume origin[J]?Acta Petrologica et Mineralogica,22(1):20-28(in Chinese with English abstract).
Yang H,Liu F L,Du L L,Liu P H and Wang F.2012.Zircon U-Pb dating for metavolcanites in the Laochanghe formating of the Dahongshan group in southwestern Yangtze block,and its geological significance[J].Acta Petrologica Sinica,28(9):2994-3014(in Chinese with English abstract).
Zartman R E and Doe B R.1981.Plumbotectonics-the model[J].Tectonophysics,75:135-162
Zhang C J,Wang Y L,Li X L,Xiu S Z and Huang Y J.1998.Geochemistry of platinum elements in mafic-ultramafic rocks from the Xinjie intrusion[J].Geochimica,27(5):458-466(in Chinese with English abstract).
Zhao X F,Zhou M F,Li J W,Sun M,Gao J F,Sun W H and Yang J H.2010.Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan,SW China:Implications for tectonic evolution of the Yangtze Block[J].Precambian Research,182:57-69.
Zhao X F and Zhou M F.2011.Fe-Cu deposits in the Kangdian region,SW China:A proterozoic IOCG(iron-oxide-copper-gold)metallogenic province[J].Mineralium Deposita,46:731-747.
Zhao X F,Zhou M F,Li J W,Selby D,Li X H and Qi L.2013.Sulfide Re-Os and Rb-Sr isotope dating of the Kangdian IOCG metallogenic province,southwest China:Implications for regional metallogenesis[J].Econ.Geol.,108:1489-1498.
Zhao Z H.1997.Trace elements Geochemistry theory[M].Beijing:Geological Publishing House.218p(in Chinese).
Zhou J Y,Mao J W,Liu F Y,Tan H Q,Shen B,Zhu Z M,Chen J B,Luo L P,Zhou X and Wang Y.2011.SHRIMP U-Pb zircon chronology and geochemistry of albitite form the Hekou group in the western Yangtze block[J].J.Mineral Petrol.,31(3):66-73(in Chinese with English abstract).
Zhou M F.1994.PGE distribution in 2.7 Ga layered komatiite flows from the Blingwe greenstone belt,Zimbabwe[J].Chemical Geology,118:155-172.
Zhu D C,Pan G T,Mo X X,Wang L Q,Zhao Z D,Liao Z L,Geng QR and Dong G C.2006.Identification for the Mesozoic OIB-type basalts in Central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting[J].Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract).
Zhu H P,Fan W Y,Zhou B G,Wang S W,Luo M J,Liao Z W and Guo Y.2011.Assessing Precambrian stratigraphic sequence of Dongchuan area:Evidence from zircon SHRIMP and LA-ICP-MS dating[J].Geological Journal of China Universities,17(3):1-12(in Chinese with English abstract).
Zhu Z M,Hou K J,Zhu K Y and Tan H Q.2013.Geochronology and geochemistry of the Hekou Group in Sichuan Province,SW China[J].Geochemical Journal,47:51-64.
附中文参考文献
耿元生,柳永清,高林志,彭楠,江小均.2012.扬子克拉通西南缘中元古代通安组的形成时代---锆石LA-ICP-MS U-Pb年龄[J].地质学报,86(9):1479-1490.
龚琳,何毅特.1996.云南东川元古宙裂谷型铜矿[M].北京:冶金工业出版社.2-28.
关俊雷,郑来林,刘建辉,孙志明,程万华.2011.四川省会理县河口地区辉绿岩体的锆石SHRIMP U-Pb年龄及其地质意义[J].地质学报,85(4):482-490.
郭阳,王生伟,孙晓明,廖震文,王子正,周邦国,杨斌.2014a.云南省武定县迤纳厂铁铜矿区古元古代辉绿岩锆石的U-Pb年龄及其地质意义[J].大地构造与成矿学,38(1):208-215.
郭阳,王生伟,孙晓明,王子正,杨斌,廖震文,周邦国,蒋小芳,侯林,杨波.2014b.扬子地台西南缘古元古代末的裂解事件---来自武定地区辉绿岩锆石U-Pb年龄和地球化学证据[J].地质学报,88(9):1651-1655.
侯增谦,卢记仁,李红阳.1996a.中国西南特提斯构造演化-幔柱构造控制[J].地球学报,17(4):439-453.
侯增谦,莫宣学,朱勤文.1996b.“三江"古特提斯地幔热柱-洋岛玄武岩证据[J].地球学报,17(4):343-361.
侯增谦,莫宣学,朱勤文.1996c.“三江"古特提斯地幔热柱-洋脊玄武岩证据[J].地球学报,17(4):3623-375.
华仁民.1990.论昆阳拗拉谷[J].地质学报,4:289-301.
廖震文,王生伟,于远山,等.2010.扬子地台西缘基底成矿作用与找矿方向研究2010年度工作方案[R].成都地质矿产研究所内部报告.22-26.
刘庆,候泉林,周新华.2005.大别造山带祝家铺辉长岩的铂族元素特征[J].岩石学报,21(1):227-239.
潘杏南,赵济湘,张选阳,郑海翔,杨暹和,周国富,陶大理.1985.康滇构造与裂谷作用[M].重庆:重庆出版社.1-298.
宋谢炎,胡瑞忠,陈列锰.2009.铜、镍、铂族元素地球化学性质及其在幔源岩浆起源、演化和岩浆硫化物矿床研究中的意义[J].地学前缘,16(4):287-305.
孙赫,秦克章,李金祥,唐冬梅,范新,肖庆华.2008.地幔部分熔融程度对东天山镁铁质遛镁铁质岩铂族元素矿化的约束---以图拉根和香山铜镍矿为例[J].岩石学报,24(5):1079-1086.
孙晓明,熊德信,王生伟,石贵勇,翟伟.2006.云南哀牢山金矿带墨江金镍矿床铂族元素(PGE)地球化学及其对矿床成因的制约[J].矿床地质,25(4):438-446.
孙志明,尹福光,关俊雷,刘建辉,李军敏,耿全如,王立全.2009.云南东川地区昆阳群黑山组凝灰岩锆石SHRIMP U-Pb测年及其地层学意义[J].地质通报,28(7):896-900.
汪云亮,张成江,修淑芝.2001.玄武岩形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J].岩石学报,17(3):413-421.
王冬兵,孙志明,尹福光,王立全,王保弟,张万平.2012.扬子地块西缘河口群的时代:来自火山岩锆石LA-ICP-MS U-Pb年龄的证据[J].地层学杂志,36(3):630-635.
王冬兵,尹福光,孙志明,王立全,王保弟,廖世勇,唐渊,任光明.2013.扬子陆块西缘古元古代基性侵入岩LA-ICP-MS锆石U-Pb年龄和Hf同位素及其地质意义[J].地质通报,32(4):617-630.
王生伟,孙晓明,石贵勇,熊德信,翟伟.2006.云南白马寨铜镍硫化物矿床铂族元素地球化学及其对矿床成因的制约[J].地质学报,80(9):1474-1486.
王生伟,孙晓明,石贵勇,熊德信,翟伟.2007.云南金宝山和白马寨铜镍硫化物矿床铂族元素(PGE)地球化学的差异及其成因意义[J].地质学报,81(1):94-108.
王生伟,蒋小芳,廖震文,于远山,张海,周邦国,王子正,李永灿,杨波,郭阳,侯林,陆生林.2011.扬子地台西缘基底成矿作用及找矿方向研究成果报告[M].成都:成都地质矿产研究所.1-259.
王生伟,孙晓明,蒋小芳,屈文俊,廖震文,李超.2012.东川铜矿原生黄铜矿的Re-Os年龄及其成矿背景[J].矿床地质,31(增刊):609-610.
王生伟,廖震文,孙晓明,蒋小芳,周邦国,郭阳,罗茂金,朱华平,马东.2013a.云南东川铜矿区古元古代辉绿岩地球化学---Columbia超级大陆裂解在扬子陆块西缘的响应[J].地质学报,87(12):1834-1852.
王生伟,孙晓明,廖震文,屈文俊,杨波,蒋小芳,李超,李永灿.2013b.会理菜子园镍矿床方辉橄榄岩铂族元素、Re-Os同位素及其地质意义[J].矿床地质,32(3):515-532.
王生伟,蒋小芳,杨波,孙晓明,廖震文,周清,郭阳,王子正,杨斌.2016.康滇地区元古宙构造运动Ⅰ:昆阳陆内裂谷、地幔柱及其成矿作用[J].地质论评,62(6):1353-1377.
王子正,郭阳,杨斌,王生伟,孙晓明,侯林,周邦国,廖震文.2013.扬子克拉通西缘1.73 Ga海孜A型花岗斑岩岩体的发现及其构造意义[J].地质学报,87(7):931-942.
肖龙,徐义刚,何斌.2003a.峨眉地幔柱-岩石圈的相互作用:来自低钛和高钛玄武岩的Sr-Nd和O同位素证据[J].高校地质学报,9(2):207-217.
肖龙,徐义刚,梅厚均,何斌.2003b.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系---地球化学证据[J].岩石学报,19(1):38-48.
肖龙,徐义刚,梅厚均,于荣坪.2003c.云南保山卧牛寺玄武岩成因:地幔柱活动的产物[J]?岩石矿物学杂志,22(1):20-28.
杨红,刘福来,杜利林,刘平华,王舫.2012.扬子地块西南缘大红山群老厂河组变质火山岩的锆石U-Pb定年及其地质意义[J].岩石学报,28(9):2994-3014.
张成江,汪云亮,李晓林,修淑芝,黄永建.1998.新街镁铁-超镁铁岩侵入体的铂族元素地球化学特征[J].地球化学,27(5):458-466.
赵振华.1997,微量元素地球化学原理[M].北京:科学出版社.122-177.
周家云,毛景文,刘飞燕,谭洪旗,沈冰,朱志敏,陈家彪,罗丽萍,周雄,王越.2011.扬子地台西缘河口群钠长岩锆石SHRIMP年龄及岩石地球化学特征[J].矿物岩石,31(3):66-73.
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境[J].地质学报,80(9):1312-1328.
朱华平,范文玉,周邦国,王生伟,罗茂金,廖震文,郭阳.2011.论东川地区前震旦系地层层序:来自锆石SHRIMP及La-ICP-MS测年的证据[J].高校地质学报,17(3):1-12.
Aland O,Griffin W L and Lorand J P.2000.Non-chondritic distribution of the highly sidemphile elements in mantle sulphides[J].Nature,407:891-894
Ballhaus C and Ryan C G.1995.Platinum-group elements in the Merensky reef.ⅠPGE in solid solution in base metal sulfides and downtemperature equilibration history of Merensky ores[J].Contrb.Mineral.Petrol.,122:241-251.
Barnes S,Naldrett A J and Gorlon M P.1985.The origin of the fractionation of platinum-group elements in terrestrial magmas[J].Chemical Geology,53:303-323.
Barnes S J and Naldrett A J.1987.Fractionation of the platinum-group elements and gold in some komatiites of the Abitibi greenstone blet,Northern Ontario[J].Econ.Geol.,82(1):165-183.
Barnes S J,Boyd R,Korneliussern A,Nilsson L P,Often M,Pedersen RB and Robins B.1988.The use of mantle normalization and metal ratios in discriminating between the effects of partial melting,crystal fractionation and sulfide segregation on platinum-group elements,gold,nicked and copper:Examples from Norway[M].In:Prichard H M,Potts P J,Bowles J F W,et al.eds.Geo-platinum 87.London:Elsevier.113-143.
Barnes S J.1990.The use of metal ratios in prospecting for platinumgroup element deposits in mafic and ultramafic intrusions[J].Journal of Geochemical Exploration,37:91-99.
Barnes S J and Picard C P.1993.The behavior of platinum-group elements during partial melting,crystal fractionation,and sulphide segregation:An example from the Cape Smith fold belt,northern Quebec[J].Geochimica et Cosmochimica Acta,57:79-87.
Barnes S J and Maier W D.1999.The fraction at ion of Ni-Cu and the noble metals in silicate and sulphide liquids[J].Geological association of Canada Short Course,13:69-106.
Biugmann G E,Naldrett A J.Asif M,Lightfoot P C,Gorbachev N S and Fedorenko V A.1993.Siderophile and chalcophile metals as tracers of the evolution of the Siberian Traps in the Noril'sk region,Russia[J].Geochimica et Cosmochimica Acta,57:2001-2018.
Brugmann G E,Arndt N T,Hoffmann A W and Tobschall H J.1987.Noble metal abundances in komatiite suites form Alexo,Ontario,and Corgana Island,Columbia[J].Geochimica et Cosmochimica Acta,51:2159-2169.
Capobianco C JHervig R Land Darke M J.1994.Experiments on Ru,Rh and Pd compatibility for magnetite and hematite solid solutions crystallized from silicate melts[J].Chemical Geology,113:23-44.
Chen W T,Zhou M F and Zhao X F.2013.Late paleoproterozoic sedimentary and mafic rocks in the Hekou area,SW China:Implication for the reconstruction of the Yangtze block in Columbia[J].Precambrian Research,231:61-77.
Crocket J H and Teruta Y.1977.Palladium iridium and gold contents of nafic and ultramafic rocks drilled from the mid-Atlantic ridge,Leg37,Deep Sea Drilling Project[J].Canadian Journal of Earth Sciences,14:777-784.
Garuti G,Gorgoni C and Sighinolfi G P.1984.Sulfide mineralogy and chalcophile and siderophile element aboundances in the Ivrea-Verbano mantle peridotites(western Italian Alps)[J].Earth Planetary Science Letters,70:69-87.
Garuti G,Fershtater G,Bea F,Montero P,Pushkarev E V and Zaccarini F.1997.Platinum-group elements as petrological indicators in maficultramafic complexes of the central and southern Urals:Preliminary results[J].Tectonophysics,276:181-194.
Geng Y S,Liu Y Q,Gao L Z,Peng N and Jiang X J.2012.Geochronology of the Mesoproterozoic Toang'an Formation in southwestern margin of Yangtze craton:New evidence from zircon LA-ICP-MS U-Pb ages[J].Acta Geologica Sinica,86(9):1479-1490(in Chinese with English abstract)..
Gong L and He Y T.1996.The Proterozoic rift type copper in Yunnan Province[M].Beijing:Press of Metallurgy Industry.2-28(in Chinese).
Green M G,Sylvester P J and Buick R.2000.Growth and recycling of early Archaean continental crust:Geochemical evidence from the Coonterunah and Warrawoona Groups,Pilbara Craton,Australia[J].Tectonophysics,322(1):69-88.
Greentree M R and Li Z X.2008.The oldest known rocks in south-western China:SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group[J].Journal of Asian Earth Sciences,33(5-6):289-302.
Guan J L,Zhen L L,Liu J H,Sun Z M and Cheng W H.2011.Zircon SHRIMP U-Pb dating of diabase from Hekou,Si Chuan Province,China and its geological significance[J].Acta Geologica Sinica,85(4):482-490(in Chinese with English abstract).
Guo Y,Wang S W,Sun X M,Liao Z W,Wang Z Z,Zhou B G and Yang B.2014a.Zircon U-Pb age of the Paleoproterozoic diabase from the Yinachang iron-copper deposit,Yunnan Province,and its geological implication[J].Geotectonica et Metallogenia,38(1):208-215(in Chinese with English abstract).
Guo Y,Wang S W,Sun X M,Wang Z Z,Yang B,Liao Z W,Zhou BG,Jiang X F,Hou L and Yang B.2014b.The Paleoproterozoic breakup event in the southwest Yangtze block:evidence from U-Pb zircon age and geochemistry of diabase in Wuding,Yunnan Province,SW China[J].Acta Geologica Sinica,88(9):1651-1655(in Chinese with English abstract).
Hauri E H.1996.Major-element variability in the Hawaiian mantle plume[J].Nature,382(1):415-419.
Hou Z Q,Lu J R,Li H Y,Wang D H and LüQ T.1996a.Tectonic evolution of the Tethys in southwestern China:Is controlled by plume tectonics[J].Acta Geoscientia Sinica,17(4):439-453(in Chinese with English abstract).
Hou Z Q,Mo X X,Zhu Q W and Shen S Y.1996b.Mantle plume in the Sanjiang paleo-Tethyan region,China:Evidence from ocean-island basalts[J].Acta Geoscientia Sinica,17(4):343-361(in Chinese with English abstract).
Hou Z Q,Mo X X,Zhu Q W and Shen S Y.1996c.Mantle plume in the Sanjiang Paleo-Tethyan lithosphere:Evidence from mid-ocean radge basalts[J].Acta Geoscientia Sinica,17(4):362-375(in Chinese with English abstract).
Hua R M.1990.On the Kunyang aulacogen[J].Acta Geologica Sinica,4:289-301(in Chinese with English abstract).
Jiang S Y,Yang J H,Ling H F,Feng H Z,Chen Y Q and Chen J H.2003.Re-Os isotopes and PGE geochemistry of black shales and intercalated Ni-Mo polymetallic sulfide bed from the Lower Cambrian Niutitang Formation,South China[J].Progress in Natural Sciences,13(10):788-794.
Keays R R.1995.The role of komatiitic and picritic magmatism and S-saturation in the formation of the ore deposits[J].Lithos,34:1-18.
Lee D C,Halliday A N,Fitton J G and Poli G.1994.Isotopic variations with with distance and time in the volcanic islands of the Cameroon line:Evidence for a mantle plume origin[J].Earth and Planetary Science Letters,123:119-138.
Liao Z W,Wang S W,Yu Y S,et al.2010.The basement metallogenesis and prospecting direction of western margin of Yangtze Platform[R].Internal report of Chengdu Institute of Geology and Mineral Resourses.22-26(in Chinese).
Liu Q,Hou Q L,Zhou X H and Xie L W.2005.The distribution of platinum-group elements in gabbros from Zhujiapu Dabie orogen[J].Acta Petrologica Sinica,21(1):227-239(in Chinese with English abstract).
Maier W D,Barnes S J,De klerk W J,Teigler B and Mitchell A A.1996.Cu/Pd and Cu/Pt of silicate rocks in the Bushveld complex:Implications for platinum-group element exploration[J].Econ.Geol.,91:1151-1158.
Maier W D,Bames S J and Marsh J S.2003.The concentrations of the noblemetals in southern African flood-type basalts and MORB Implications for petrogenes is and magmatic sulphide exploration[J].Contributions to Mineralogy and Petrology,146:44-61.
Middlemost E A K.1994.Naming materials in magma/igneous rock system[J].Earth Sci.Rev.,37:215-224.
Mitchell R H and Keays R R.1981.Abundance and distribution of gold,palladium and iridium in some spinel and garnet lherzolites:Implication for the nature and origin of precious metal rich intergranular component in the upper mantle[J].Geochimca et Cosmochimica Acta,45:2425-2445.
Naldrett A J and Cabri L J.1976.Ultramafic and related rocks:Their classification and genesis with special reference to the concentration of nickel sulfides and platinum-group elements[J].Econ.Geol.,76:1131-1158.
Naldrett A J and Duke M.1980.Platinum metals in magmatic sulfide ores[J].Science,208:1417-1424
Oshin I O and Crocket J H.1982.Noble metal in Thetford mines ophiolite,Quebec,Canada.PartⅠ:Distribution of gold,iridium,platinum,and palladium in the ultramafic and gabbroic rocks[J].Econ.Geol.,77:1556-1570.
Pang X N,Zhao J X,Zhuang X Y,Zhen H X,Yang X H,Zhou G F and Tao D L.1985.Tectonics and rifting in kangdian region[M].Chongqing:Chongqing Publishing House.1-298(in Chinese with English abstract).
Qi L and Gregoire D C.2000.Determination of trace elements in twenty six Chinese geochemistry reference materials by inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research,24(1):51-63.
Song X Y,Hu R Z and Chen L M.2009.Geochemical natures of copper,nickel and PGE and their significance for the study of origin and evolution of mantle-derived magmas and magmatic sulfide deposits[J].Earth.Science Frontiers,16(4):287-305(in Chinese with English abstract).
Steiger R H and J8)ger E.1977.Subcommission on geochronology:Convention on the use of decay constants in geo-and cosmochronology[J].Earth and Planetary Science Letters,36(3):359-362.
Stein M and Hofmann A W.1992.Fossil plume head beneath the Arabian lithosphere[J]?Earth and planetary Science Letters,114(1):193-210.
Stern R A,Syme E C and Lueas S B.1995.Geochemistry of 1.9 Ga MORB-and OIB-like basalts from the Amisk collage,Flin Flon belt,Canada:Evidence for an intr-oceanic origin[J].Geochimica et Cosmochimica Acta,59(15):3131-3154.
Sun H,Qin K Z,Li J X,Teng D M,Fan X and Xiao Q H.2008.Constraint of mantle partial melting on PGE mineralization of mafic-ultramafic intrusions in Eastern Tianshan:Case study on Tulargen and Xiangshan Cu-Ni deposits[J].Acta Petrologica Sinica,24(5):1079-1086(in Chinese with English abstract).
Sun S S and Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalt:Implications for mantle composition and process[A].In:Saunders A D and Norry M J,eds.Magmatism in the Ocean Basins[C].Spc.Publ.Geol.Soc.Lond.,42:528-548.
Sun X M,Xiong D X,Wang S W,Shi G Y and Zhai W.2006.Platinum group elements(PGE)geochemistry of Mojiang Au-Nideposit and its constraint on ore genesis[J].25(4):438-446(in Chinese with English abstract).
Sun Z M,Yin F G,Guan J L,Liu J H,Li J M,Geng Q R and Wang LQ.2009.SHRIMP U-Pb dating and its stratigraphic significance of tuff zircons from Heishan formation of Kunyang Group,Dongchuan area,Yunnan Province,China[J].Geological Bulletin of China,28(7):896-900(in Chinese with English abstract).
Wang D B,Sun Z M,Yin F G,Wang L Q,Wang B D and Zhang W P.2012.Geochronology of the Hekou Group on the western margin of the Yangtze block:Evidence from zircon LA-ICP-MS U-Pb dating of volcanic rocks[J].Journal of Stratigraphy,36(3):630-635(in Chinese with English abstract).
Wang D B,Yin F G,Sun Z M,Wang L Q,Wang B D,Liao S Y,Tang Y and Ren G M.2013.Zircon U-Pb age and Hf isotope of Paleoproterozoic mafic intrusion on the western margin of the Yangtze block and their implication[J].Geological Bulletin of China,32(4):617-630(in Chinese with English abstract).
Wang S W,Sun X M,Shi G Y,Xiong D X and Zhai W.2006.Platinum group elements(PGE)geochemistry of Baimazhai Ni-Cu sulfide deposit and its constraints on the ore genesis[J].Acta Geologica Sinica,80(9):1474-1486(in Chinese with English abstract).
Wang S W,Sun X M,Shi G Y,Xiong D X and Zhai W.2007.Distinction of platinum group elements(PGE)geochemistry between the Jinbaoshan and Baimazhai magmatic sulfide deposits in Yunnan Province,China,and its implication for ore genesis[J].Acta Geologica Sinica,81(1):93-108(in Chinese with English abstract).
Wang S W,Jiang X F,Liao Z W,Yu Y S,Zhang H,Zhou B G,Wang Z Z,Li Y C,Yang B,Guo Y,Hou L and Lu S L.2011.Research report on metallogenesis and prospecting direction of basement in the southwest of Yangtze platform[M].Chengdu and Chengdu Institute of Mineral Resources.1-259(in Chinese).
Wang S W,Sun X M,Jiang X F,Qu W J,Liao Z W and Li C.2012.Re-Os isotopic age and mineralization setting of protosomatic chalcopyrites from Donghcuan copper deposit[J].Mineral Deposits,31(Supp.):609-610(in Chinese with English abstract).
Wang S W,Liao Z W,Sun X M,Jiang X F,Zhou B G,Guo Y,Luo MJ,Zhu H P and Ma D.2013a.Geochemistry of Paleoproterozoic diabases in the Dongchuan copper deposit,Yunnan,SW China:Response to breakup of the Columbia supercontinent in the Southwestern Margin of Yangtze block[J].Acta Geologica Sinica,87(12):1834-1852(in Chinese with English abstract).
Wang S W,Sun X M,Liao Z W,Qu W J,Yang B,Jiang X F,Li C and Li Y C.2013b.Platinum group elements and Re-Os isotope geochemistry of harzburgites form Caiziyuan nickel deposit in Huili county of Sichuan Province and its geological significance[J].Mineral Deposits,32(3):515-532(in Chinese with English abstract).
Wang S W,Jiang X F,Yang B,Sun X M,Liao Z W,Zhou Q,Guo Y,Wang Z Z and Yang B.2016.The Proterozoic tectonic movement In Kangdian area I:Kunyang Intracontinental Rift,mantle plume and its metallogenesis[J].Geological Review,62(6):1353-1377(in Chinese with English abstract).
Wang Y L,Zhang C J and Xiu S Z.2001.Th/Hf-Ta/Hf identification of tectonic setting of basalts[J].Acta Petrologica Sinica,17(3):413-421(in Chinese with English abstract).
Wang Z Z Guo Y,Yang B,Wang S W,Sun X M,Hou L,Zhou B G and Liao Z W.2013.Discovery of the 1.73 Ga Haizi anorogenic type granite in the western margin of Yangtze craton,and its geological significance[J].Acta Geologica Sinica,87(7):931-942(in Chinese with English abstract).
Weis D,Frey F A,Leyrit H and Gautier I.1993.Kerguelen archipelago revisited:Implication and isotopic study of the southeast province lavas[J].Earth and Planetary Science Letters,118:101-119.
Xiao L,Xu Y G and He B.2003a.Emei mantle plume-subcontinental lithosphere interaction:Sr-Nd and O isotopic evidences from low-Ti and high-Ti basalts[J].Geological Jounal of China Universities,9(2):207-217(in Chinese with English abstract).
Xiao L,Xu Y M,Mei H J and He B.2003b.Late Permian flood basalts at Jinping area and its relation to Emei mantle plume:Geochemical evidence[J].Acta Petrologica Sinica,19(1):38-48(in Chinese with English abstract).
Xiao L,Xu Y G,Mei H J and Yu R P.2003c.Petrogenesis of the basalts of Woniusi Formation at Baoshan area,Yunnan:Is it of mantle plume origin[J]?Acta Petrologica et Mineralogica,22(1):20-28(in Chinese with English abstract).
Yang H,Liu F L,Du L L,Liu P H and Wang F.2012.Zircon U-Pb dating for metavolcanites in the Laochanghe formating of the Dahongshan group in southwestern Yangtze block,and its geological significance[J].Acta Petrologica Sinica,28(9):2994-3014(in Chinese with English abstract).
Zartman R E and Doe B R.1981.Plumbotectonics-the model[J].Tectonophysics,75:135-162
Zhang C J,Wang Y L,Li X L,Xiu S Z and Huang Y J.1998.Geochemistry of platinum elements in mafic-ultramafic rocks from the Xinjie intrusion[J].Geochimica,27(5):458-466(in Chinese with English abstract).
Zhao X F,Zhou M F,Li J W,Sun M,Gao J F,Sun W H and Yang J H.2010.Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan,SW China:Implications for tectonic evolution of the Yangtze Block[J].Precambian Research,182:57-69.
Zhao X F and Zhou M F.2011.Fe-Cu deposits in the Kangdian region,SW China:A proterozoic IOCG(iron-oxide-copper-gold)metallogenic province[J].Mineralium Deposita,46:731-747.
Zhao X F,Zhou M F,Li J W,Selby D,Li X H and Qi L.2013.Sulfide Re-Os and Rb-Sr isotope dating of the Kangdian IOCG metallogenic province,southwest China:Implications for regional metallogenesis[J].Econ.Geol.,108:1489-1498.
Zhao Z H.1997.Trace elements Geochemistry theory[M].Beijing:Geological Publishing House.218p(in Chinese).
Zhou J Y,Mao J W,Liu F Y,Tan H Q,Shen B,Zhu Z M,Chen J B,Luo L P,Zhou X and Wang Y.2011.SHRIMP U-Pb zircon chronology and geochemistry of albitite form the Hekou group in the western Yangtze block[J].J.Mineral Petrol.,31(3):66-73(in Chinese with English abstract).
Zhou M F.1994.PGE distribution in 2.7 Ga layered komatiite flows from the Blingwe greenstone belt,Zimbabwe[J].Chemical Geology,118:155-172.
Zhu D C,Pan G T,Mo X X,Wang L Q,Zhao Z D,Liao Z L,Geng QR and Dong G C.2006.Identification for the Mesozoic OIB-type basalts in Central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting[J].Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract).
Zhu H P,Fan W Y,Zhou B G,Wang S W,Luo M J,Liao Z W and Guo Y.2011.Assessing Precambrian stratigraphic sequence of Dongchuan area:Evidence from zircon SHRIMP and LA-ICP-MS dating[J].Geological Journal of China Universities,17(3):1-12(in Chinese with English abstract).
Zhu Z M,Hou K J,Zhu K Y and Tan H Q.2013.Geochronology and geochemistry of the Hekou Group in Sichuan Province,SW China[J].Geochemical Journal,47:51-64.
附中文参考文献
耿元生,柳永清,高林志,彭楠,江小均.2012.扬子克拉通西南缘中元古代通安组的形成时代---锆石LA-ICP-MS U-Pb年龄[J].地质学报,86(9):1479-1490.
龚琳,何毅特.1996.云南东川元古宙裂谷型铜矿[M].北京:冶金工业出版社.2-28.
关俊雷,郑来林,刘建辉,孙志明,程万华.2011.四川省会理县河口地区辉绿岩体的锆石SHRIMP U-Pb年龄及其地质意义[J].地质学报,85(4):482-490.
郭阳,王生伟,孙晓明,廖震文,王子正,周邦国,杨斌.2014a.云南省武定县迤纳厂铁铜矿区古元古代辉绿岩锆石的U-Pb年龄及其地质意义[J].大地构造与成矿学,38(1):208-215.
郭阳,王生伟,孙晓明,王子正,杨斌,廖震文,周邦国,蒋小芳,侯林,杨波.2014b.扬子地台西南缘古元古代末的裂解事件---来自武定地区辉绿岩锆石U-Pb年龄和地球化学证据[J].地质学报,88(9):1651-1655.
侯增谦,卢记仁,李红阳.1996a.中国西南特提斯构造演化-幔柱构造控制[J].地球学报,17(4):439-453.
侯增谦,莫宣学,朱勤文.1996b.“三江"古特提斯地幔热柱-洋岛玄武岩证据[J].地球学报,17(4):343-361.
侯增谦,莫宣学,朱勤文.1996c.“三江"古特提斯地幔热柱-洋脊玄武岩证据[J].地球学报,17(4):3623-375.
华仁民.1990.论昆阳拗拉谷[J].地质学报,4:289-301.
廖震文,王生伟,于远山,等.2010.扬子地台西缘基底成矿作用与找矿方向研究2010年度工作方案[R].成都地质矿产研究所内部报告.22-26.
刘庆,候泉林,周新华.2005.大别造山带祝家铺辉长岩的铂族元素特征[J].岩石学报,21(1):227-239.
潘杏南,赵济湘,张选阳,郑海翔,杨暹和,周国富,陶大理.1985.康滇构造与裂谷作用[M].重庆:重庆出版社.1-298.
宋谢炎,胡瑞忠,陈列锰.2009.铜、镍、铂族元素地球化学性质及其在幔源岩浆起源、演化和岩浆硫化物矿床研究中的意义[J].地学前缘,16(4):287-305.
孙赫,秦克章,李金祥,唐冬梅,范新,肖庆华.2008.地幔部分熔融程度对东天山镁铁质遛镁铁质岩铂族元素矿化的约束---以图拉根和香山铜镍矿为例[J].岩石学报,24(5):1079-1086.
孙晓明,熊德信,王生伟,石贵勇,翟伟.2006.云南哀牢山金矿带墨江金镍矿床铂族元素(PGE)地球化学及其对矿床成因的制约[J].矿床地质,25(4):438-446.
孙志明,尹福光,关俊雷,刘建辉,李军敏,耿全如,王立全.2009.云南东川地区昆阳群黑山组凝灰岩锆石SHRIMP U-Pb测年及其地层学意义[J].地质通报,28(7):896-900.
汪云亮,张成江,修淑芝.2001.玄武岩形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J].岩石学报,17(3):413-421.
王冬兵,孙志明,尹福光,王立全,王保弟,张万平.2012.扬子地块西缘河口群的时代:来自火山岩锆石LA-ICP-MS U-Pb年龄的证据[J].地层学杂志,36(3):630-635.
王冬兵,尹福光,孙志明,王立全,王保弟,廖世勇,唐渊,任光明.2013.扬子陆块西缘古元古代基性侵入岩LA-ICP-MS锆石U-Pb年龄和Hf同位素及其地质意义[J].地质通报,32(4):617-630.
王生伟,孙晓明,石贵勇,熊德信,翟伟.2006.云南白马寨铜镍硫化物矿床铂族元素地球化学及其对矿床成因的制约[J].地质学报,80(9):1474-1486.
王生伟,孙晓明,石贵勇,熊德信,翟伟.2007.云南金宝山和白马寨铜镍硫化物矿床铂族元素(PGE)地球化学的差异及其成因意义[J].地质学报,81(1):94-108.
王生伟,蒋小芳,廖震文,于远山,张海,周邦国,王子正,李永灿,杨波,郭阳,侯林,陆生林.2011.扬子地台西缘基底成矿作用及找矿方向研究成果报告[M].成都:成都地质矿产研究所.1-259.
王生伟,孙晓明,蒋小芳,屈文俊,廖震文,李超.2012.东川铜矿原生黄铜矿的Re-Os年龄及其成矿背景[J].矿床地质,31(增刊):609-610.
王生伟,廖震文,孙晓明,蒋小芳,周邦国,郭阳,罗茂金,朱华平,马东.2013a.云南东川铜矿区古元古代辉绿岩地球化学---Columbia超级大陆裂解在扬子陆块西缘的响应[J].地质学报,87(12):1834-1852.
王生伟,孙晓明,廖震文,屈文俊,杨波,蒋小芳,李超,李永灿.2013b.会理菜子园镍矿床方辉橄榄岩铂族元素、Re-Os同位素及其地质意义[J].矿床地质,32(3):515-532.
王生伟,蒋小芳,杨波,孙晓明,廖震文,周清,郭阳,王子正,杨斌.2016.康滇地区元古宙构造运动Ⅰ:昆阳陆内裂谷、地幔柱及其成矿作用[J].地质论评,62(6):1353-1377.
王子正,郭阳,杨斌,王生伟,孙晓明,侯林,周邦国,廖震文.2013.扬子克拉通西缘1.73 Ga海孜A型花岗斑岩岩体的发现及其构造意义[J].地质学报,87(7):931-942.
肖龙,徐义刚,何斌.2003a.峨眉地幔柱-岩石圈的相互作用:来自低钛和高钛玄武岩的Sr-Nd和O同位素证据[J].高校地质学报,9(2):207-217.
肖龙,徐义刚,梅厚均,何斌.2003b.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系---地球化学证据[J].岩石学报,19(1):38-48.
肖龙,徐义刚,梅厚均,于荣坪.2003c.云南保山卧牛寺玄武岩成因:地幔柱活动的产物[J]?岩石矿物学杂志,22(1):20-28.
杨红,刘福来,杜利林,刘平华,王舫.2012.扬子地块西南缘大红山群老厂河组变质火山岩的锆石U-Pb定年及其地质意义[J].岩石学报,28(9):2994-3014.
张成江,汪云亮,李晓林,修淑芝,黄永建.1998.新街镁铁-超镁铁岩侵入体的铂族元素地球化学特征[J].地球化学,27(5):458-466.
赵振华.1997,微量元素地球化学原理[M].北京:科学出版社.122-177.
周家云,毛景文,刘飞燕,谭洪旗,沈冰,朱志敏,陈家彪,罗丽萍,周雄,王越.2011.扬子地台西缘河口群钠长岩锆石SHRIMP年龄及岩石地球化学特征[J].矿物岩石,31(3):66-73.
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境[J].地质学报,80(9):1312-1328.
朱华平,范文玉,周邦国,王生伟,罗茂金,廖震文,郭阳.2011.论东川地区前震旦系地层层序:来自锆石SHRIMP及La-ICP-MS测年的证据[J].高校地质学报,17(3):1-12.