班-怒结合带西段革吉地区帕阿岩基的成因:元素地球化学、锆石U-Pb年代学及Hf同位素约束
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摘要
班公湖-怒江结合带是藏北一条重要的特提斯主洋残余,在洋盆消减过程中发生了强烈岩浆作用,在其南缘形成了沿狮泉河-永珠缝合带两侧广泛分布的白垩纪大规模岩浆岩和火山岩,为了解班公湖-怒江特提斯洋俯冲和闭合过程提供了良好窗口。本文对出露于革吉地区帕阿花岗闪长岩岩基进行了详细的野外地质填图、全岩元素地球化学、锆石U-Pb年代学和Hf同位素组成研究。研究结果表明,花岗闪长岩和其闪长质包体的锆石206Pb/238U年龄分别为155. 7±1. 0Ma(谐和年龄,MSWD=0. 26,N=18)和156. 5±2. 3Ma(年龄加权平均值,MSWD=2. 6,N=16),岩浆侵位于晚侏罗世,不是以往所认为的白垩纪岩浆产物。花岗闪长岩主要属于高钾钙碱性系列,高铝饱和指数(A/CNK=0. 91～1. 04),显示了过铝质特征。花岗闪长岩富集轻稀土元素(LREE/HREE)=5. 51～8. 54,(La/Yb)N=6. 27～20. 2)和大离子亲石元素,亏损Nb、Ta、Sr、Ti等高场强元素,具有中等至弱Eu负异常(δEu=0. 61～0. 85)。锆石Hf同位素分布集中,花岗闪长岩和闪长质包体的锆石εHf(t)均为负值,分别为(-9. 4～-6. 3)和(-10. 9～-8. 6),Hf地壳模式年龄分别为(1. 32～1. 48Ga)和(1. 44～1. 56Ga),指示了帕阿花岗闪长岩岩基主体系古老地壳基底部分熔融产物,存在少量地幔物质的加入,形成于弧环境,可能属于班公湖-怒江洋盆南向俯冲到拉萨地块古老结晶基底重熔形成的一套具弧属性的未分异I型花岗岩。
The Bangong Co-Nujiang River suture zone,locating in the boundary zone of South Qiangtang Terrane and Lhasa Terrane,has widely been accepted as a vital remnant of the main Meso-Tethys. Abundant magmatic rocks were induced by the oceanic subduction and closure. A large-scale Cretaceous material-thermal activity product widely distributed along the southern margin of the Shiquanhe-Yongzhu suture zone,which provided us good opportunity for understanding the tectonic evolution of the Bangong Co-Nujiang River Tethys ocean. In this paper,the whole rock element geochemistry,zircon U-Pb chronology and Hf isotopic composition were studied in the Pa'a batholiths that were exposed in the north region of Geji County in the western part of the Bangong Co-Nujiang River suture zone. The zircon206 Pb/238 U age of the experimental samples granodiorite and its dirorite inclusions were 155. 7 ± 1. 0 Ma( concordia age,MSWD = 0. 26,N = 18) and 156. 5 ± 2. 3 Ma( weighted average age,MSWD = 2. 6,N = 16) respectively,reflecting the magma emplacement occurred in the Late Jurassic,which was not the Cretaceous magma products previously thought. Granodiorites belong to the high-K calc-alkaline series with aluminum feature. Samples of granodiorite were enriched in light rare earth elements( LREE/HREE = 5. 51 ～ 8. 54,( La/Yb)N= 6. 27 ～ 20. 2),large ion lithophile and depleted Nb,Ta,Sr,Ti and other high field strength elements,and a weak Eu negative anomaly( δEu = 0. 61 ～ 0. 85). The Hf isotopes of zircons from granodiorite and diorite inclusion are concentrated,the values of εHf( t) are both negative(-9. 4 ～-6. 3 and-10. 9 ～-8. 6),Hf crustal age are older( 1. 32 ～ 1. 48 Ga and 1. 44 ～ 1. 56 Ga),which indicated the most of the Pa'a batholiths were the product of partial melting of the ancient crust basement with a small amount of mantle material added. Combined with the chronological dating results in the study area and regional tectonic evolution,the Pa 'a batholith was formed in the Late Jurassic. The Pa 'a batholith probably belong to undifferentiated I-type granites with arc feature and formed by the south-direction subduction of the Bangong Co-Nujiang River oceanic crust to the ancient crystalline basement of the Lhasa block.
The Bangong Co-Nujiang River suture zone,locating in the boundary zone of South Qiangtang Terrane and Lhasa Terrane,has widely been accepted as a vital remnant of the main Meso-Tethys. Abundant magmatic rocks were induced by the oceanic subduction and closure. A large-scale Cretaceous material-thermal activity product widely distributed along the southern margin of the Shiquanhe-Yongzhu suture zone,which provided us good opportunity for understanding the tectonic evolution of the Bangong Co-Nujiang River Tethys ocean. In this paper,the whole rock element geochemistry,zircon U-Pb chronology and Hf isotopic composition were studied in the Pa'a batholiths that were exposed in the north region of Geji County in the western part of the Bangong Co-Nujiang River suture zone. The zircon206 Pb/238 U age of the experimental samples granodiorite and its dirorite inclusions were 155. 7 ± 1. 0 Ma( concordia age,MSWD = 0. 26,N = 18) and 156. 5 ± 2. 3 Ma( weighted average age,MSWD = 2. 6,N = 16) respectively,reflecting the magma emplacement occurred in the Late Jurassic,which was not the Cretaceous magma products previously thought. Granodiorites belong to the high-K calc-alkaline series with aluminum feature. Samples of granodiorite were enriched in light rare earth elements( LREE/HREE = 5. 51 ～ 8. 54,( La/Yb)N= 6. 27 ～ 20. 2),large ion lithophile and depleted Nb,Ta,Sr,Ti and other high field strength elements,and a weak Eu negative anomaly( δEu = 0. 61 ～ 0. 85). The Hf isotopes of zircons from granodiorite and diorite inclusion are concentrated,the values of εHf( t) are both negative(-9. 4 ～-6. 3 and-10. 9 ～-8. 6),Hf crustal age are older( 1. 32 ～ 1. 48 Ga and 1. 44 ～ 1. 56 Ga),which indicated the most of the Pa'a batholiths were the product of partial melting of the ancient crust basement with a small amount of mantle material added. Combined with the chronological dating results in the study area and regional tectonic evolution,the Pa 'a batholith was formed in the Late Jurassic. The Pa 'a batholith probably belong to undifferentiated I-type granites with arc feature and formed by the south-direction subduction of the Bangong Co-Nujiang River oceanic crust to the ancient crystalline basement of the Lhasa block.
引文
Barbarin B.2005.Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith,California:Nature,origin,and relations with the hosts.Lithos,80(1-4):155-177
Blichert TJ and Albarède F.1997.The Lu-Hf geochemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148:243-258
Cao MJ,Qin KZ,Li GM,Li JX,Zhao JX,Evans NJ and Hollings P.2016.Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane,Tibet.Gondwana Research,39:386-400
Chappell BW and White AJR.1974.Two contrasting granite types.Pacific Geology,8(2):173-174
Chappell BW and White AJR.1992.I-and S-type granites in the Lachlan fold belt.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,83(1-2):1-26
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Chappell BW,Bryant CJ and Wyborn D.2012.Peraluminous I-type granites.Lithos,153:142-153
Chen Y,Zhu DC,Zhao ZD,Zhang LL,Liu M,Yu F,Guan Q and Mo XX.2010.Geochronology,geochemistry and petrogenesis of the Bamco andesites from the northern Gangdese,Tibet.Acta Petrologica Sinica,26(7):2193-2206(in Chinese with English abstract)
Chen Y,Zhu DC,Zhao ZD,Meng FY,Wang Q,Santosh M,Wang LQ,Dong GC and Mo XX.2014.Slab breakoff triggered ca.113Ma magmatism around Xainza area of the Lhasa Terrane,Tibet.Gondwana Research,26(2):449-463
Clemens JD.2003.S-type granitic magmas-petrogenetic issues,models and evidence.Earth-Science Reviews,61(1-2):1-18
Collins WJ,Beams SD,White AJR and Chappell BW.1982.Nature and origin of A-type granites with particular reference to southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200
Collins WJ and Richards SW.2008.Geodynamic significance of S-type granites in circum-Pacific orogens.Geology,36(7):559-562
Coney PJ and Reynolds SJ.1977.Cordilleran Benioff zones.Nature,270(5636):403-406
Coulon C,Maluski H,Bollinger C and Wang S.1986.Mesozoic and Cenozoic volcanic rocks from central and southern Tibet:30Ar-40Ar dating,petrological characteristics and geodynamical significance.Earth and Planetary Science Letters,79(3-4):281-302
Crosson RS and Owens TJ.1987.Slab geometry of the Cascadia subduction zone beneath Washington from earthquake hypocenters and teleseismic converted waves.Geophysical Research Letters,14(8):824-827
Defant MJ and Drummond MS.1990.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,347(6294):662-665
Ding L,Kapp P,Zhong DL and Deng WM.2003.Cenozoic volcanism in Tibet:Evidence for a transition from oceanic to continental subduction.Journal of Petrology,44(10):1833-1865
Du DD,Qu XM,Wang GH,Xin HB and Liu ZB.2011.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang suture,Tibet:Evidence from zircon U-Pb LAICPMS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993-2002(in Chinese with English abstract)
Du DD.2012.Geochemical characteristics and implications for tectonic settings of the middle segment and western segment of Bangong LakeNu River suture,the Tibet Plateau.Master Degree Thesis.Beijing:China University of Geosciences,1-52(in Chinese with English summary)
Geng QR,Zhang Z,Peng ZM,Guan JL,Zhu XP and Mao XC.2016.Jurassic-Cretaceous granitoids and related tectono-metallogenesis in the Zapug-Duobuza arc,western Tibet.Ore Geology Reviews,77:163-175
Griffin WL,Pearson NJ,Belousova E,Jackson SE,Achterbergh EV,O’Reilly SY and Shee SR.2000.The Hf isotope compositon of cratonic mantle:LAM-MC-ICP-MS analysis of zircon magacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin WL,Wang X,Jackson SE,Pearspm NJ,O’Reilly SY,Xu XSand Zhou XM.2002.Zircon chemistry and magma mixing,SEChina:In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269
Gutscher MA,Olivet JL,Aslanian D,Eissen JP and Maury R.1999.The“lost inca plateau”:Cause of flat subduction beneath Peru?Earth and Planetary Science Letters,171(3):335-341
Guynn JH,Kapp P,Pullen A,Heizler M,Gehrels G and Ding L.2006.Tibetan basement rocks near Amdo reveal“missing”Mesozoic tectonism along the Bangong suture,central Tibet.Geology,34(6):505-508
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hou KJ,Li YH,Zou TR,Qu XM,Shi YR and Xie GQ.2007.Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications.Acta Petrologica Sinica,23(10):2595-2604(in Chinese with English abstract)
Ji WQ,Wu FY,Chung SL,Li JX and Liu CZ.2009.Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith,southern Tibet.Chemical Geology,262(3-4):229-245
Jiang X,Zhao ZD,Zhu DC,Zhang FQ,Dong GC,Mo XX and Guo TY.2010.Zircon U-Pb geochronology and Hf isotopic geochemistry of Jiangba,Bangba,and Xiongba granitoids in western Gangdese,Tibet.Acta Petrologica Sinica,26(7):2155-2164(in Chinese with English abstract)
Kang ZQ,Xu JF,Dong YH and Wang BD.2008.Cretaceous volcanic rocks of Zenong Group in north-middle Lhasa block:Products of southward subducting of the Slainajap ocean?Acta Petrologica Sinica,24(2):303-314(in Chinese with English abstract)
Kang ZQ,Xu JF,Wang BD and Chen JL.2010.Qushenla formation volcanic rocks in north Lhasa block:Products of Bangong Co-Nujiang Tethy’s southward subduction.Acta Petrologica Sinica,26(10):3106-3116(in Chinese with English abstract)
Kapp P,De Celles PG,Gehrels GE,Heizler M and Ding L.2007.Geological records of the Lhasa-Qiangtang and Indo-Asian collisions in the Nima area of Central Tibet.GSA Bulletin,119(7-8):917-933
Karsli O,Chen B,Aydin F and爦en C.2007.Geochemical and Sr-NdPb isotopic compositions of the Eocene D9lek and Sari9i9ek Plutons,Eastern Turkey:Implications for magma interaction in the genesis of high-K calc-alkaline granitoids in a post-collision extensional setting.Lithos,98(1-4):67-96
Kaygusuz A and Aydn9akr E.2009.Mineralogy,whole-rock and Sr-Nd isotope geochemistry of mafic microgranular enclaves in Cretaceous Dagbasi granitoids,Eastern Pontides,NE Turkey:Evidence of magma mixing,mingling and chemical equilibration.Chemie der Erde-Geochemistry,69(3):247-277
Kemp AIS,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
Le Maitre RW.2002.Igneous Rocks:A Classification and Glossary of Terms:Recommendations of the International Union of Geological Sciences,Subcommission on the Systematics of Igneous Rocks.2nd Edition.Cambridge:Cambridge University Press,33-39
Li BL,Song Y,Peng B,Gong FZ,Yang SG and Zhou L.2018.Discovery of ophiolitic mélange in the north region of Geji County,Northwest Tibet and its zircon U-Pb age.Acta Geologica Sinica,92(5):2032-2033
Li GM,Duan ZM,Liu B,Zhang H,Dong SL and Zhang L.2011.The discovery of Jurassic accretionary complexes in Duolong area,northern Bangong Co-Nujiang suture zone,Tibet,and its geologic significance.Geological Bulletin of China,30(8):1256-1260(in Chinese with English abstract)
Li JX,Qin KZ,Li GM,Richards JP,Zhao JX and Cao MJ.2014.Geochronology,geochemistry,and zircon Hf isotopic compositions of Mesozoic intermediate-felsic intrusions in central Tibet:Petrogenetic and tectonic implications.Lithos,198-199:77-91
Li XH,Li WY,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role of mantle-derived magma in genesis of Early Yanshanian granites in the Nanling Range,South China:In situ zircon Hf-O isotopic constraints.Science in China(Series D),52(9):1262-1278
Li YG,Wang SS,Liu MW,Meng E,Wei XY,Zhao HB and Jin MQ.2015.U-Pb dating study of baddeleyite by LA-ICP-MS:Technique and application.Acta Geologica Sinica,89(12):2400-2418(in Chinese with English abstract)
Li ZJ,Zhao RD,He ZX,Zhang Z,Li PR,You M,He S,Guo QQ and Ou J.2017.Source of ore-forming materials in the Galale coppergold deposit of Tibet:Evidence from geochemical characteristics of sulfur,lead,carbon and hydrogen-oxygen isotopes.Acta Geoscientica Sinica,38(5):651-658(in Chinese with English abstract)
Lin B,Tang JX,Chen YC,Song Y,Hall G,Wang Q,Yang C,Fang X,Duan JL,Yang HH,Liu ZB,Wang YY and Feng J.2017.Geochronology and genesis of the Tiegelongnan porphyry Cu(Au)deposit in Tibet:Evidence from U-Pb,Re-Os dating and Hf,S,and H-O isotopes.Resource Geology,67(1):1-21
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Livaccari RF,Burke K and爦eng9r AMC.1981.Was the Laramide orogeny related to subduction of an oceanic plateau?Nature,289(5795):276-278
Loiselle MC and Wones DR.1979.Characteristics and origin of anorogenic granites.Geological of Society of America,11(7):468
Ludwig KR.2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley,CA:Berkeley Geochronology Center,1-70
LüLN,Cui YB,Song L,Zhao YY,Qu XM and Wang JP.2011.Geochemical characteristics and zircon LA-ICP-MS U-Pb dating of Galale skarn gold(copper)deposit,Tibet and its significance.Earth Science Frontiers,18(5):224-242(in Chinese with English abstract)
Meng E,Liu FL,Liu PH,Liu CH,Yang H,Wang F,Shi JR and Cai J.2014.Petrogenesis and tectonic significance of Paleoproterozoic meta-mafic rocks from central Liaodong Peninsula,northeast China:Evidence from zircon U-Pb dating and in situ Lu-Hf isotopes,and whole-rock geochemistry.Precambrian Research,247:92-109
Middlemost EAK.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3-4):215-224
Murphy MA,Yin A,Harrison TM,Dürr SB,Chen Z,Ryerson FJ,Kidd WSF,Wang X and Zhou X.1997.Did the Indo-Asian collision alone create the Tibetan Plateau?Geology,25(8):719-722
Peccerillo A and Taylor SR.1976.Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81
Pitcher WS.1997.The Nature and Origin of Granite.2ndEdition.London:Chapman&Hall,1-386
Pullen A,Kapp P,Gehrels GE,Ding L and Zhang QH.2011.Metamorphic rocks in central Tibet:Lateral variations and implications for crustal structure.GSA Bulletin,123(3-4):585-600
Qu XM,Wang RJ,Xin HB,Zhao YY and Fan XT.2009.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523-535(in Chinese with English abstract)
Ran H,Wang GH,Liang X,Zheng YL and Jiumi DJ.2015.The Late Jurassic diorite in Rongma area,southern Qiangtang Terrane,Tibetan Plateau:Product of northward subduction of the Bangong CoNujiang River Tethys ocean.Geological Bulletin of China,34(5):815-825(in Chinese with English abstract)
Ravikant V,Wu FY and Ji WQ.2011.U-Pb age and Hf isotopic constraints of detrital zircons from the Himalayan foreland Subathu sub-basin on the Tertiary palaeogeography of the Himalaya.Earth and Planetary Science Letters,304(3-4):356-368
Shi RD.2007.SHRIMP dating of the Bangong Lake SSZ-type ophiolite:Constraints on the closure time of ocean in the Bangong Lake-Nujiang River,northwestern Tibet.Chinese Science Bulletin,52(7):936-941
Song Y,Yang C,Wei SG,Yang HH,Fang X and Lu HT.2018.Tectonic control,reconstruction and preservation of the Tiegelongnan porphyry and epithermal overprinting Cu(Au)deposit,Central Tibet,China.Minerals,8(9):398
S9derlund U,Patchett PJ,Vervoort JD and Isachsen CE.2004.The176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Tang JX,Song Y,Wang Q,Lin B,Yang C,Guo N,Fang X,Yang HH,Wang YY,Gao K,Ding S,Zhang Z,Duan JL,Chen HQ,Su DK,Feng J,Liu ZB,Wei SG,He W,Song JL,Li YB and Wei LJ.2016.Geological characteristics and exploration model of the Tiegelongnan Cu(Au-Ag)deposit:The first ten million tons metal resources of a porphyry-epithermal deposit in Tibet.Acta Geoscientica Sinica,37(6):663-690(in Chinese with English abstract)
Tang JX,Wang Q,Yang HH,Gao X,Zhang ZB and Zou B.2017.Mineralization,exploration and resource potential of porphyry-skarnepithermal copper polymetallic deposits in Tibet.Acta Geoscientica Sinica,38(5):571-613(in Chinese with English abstract)
van Achterbergh E,Ryan CG,Jackson SE and Griffin WL.2001.Data reduction software for LA-ICP-MS.In:Sylvester PJ(ed.).LaserAblation-ICPMS in the Earth Sciences:Principles and Applications.Ottawa,Ontario,Canada:Mineralogical Association of Canada,239-243
Wang BD,Wang LQ,Chung SL,Chen JL,Yin FG,Liu H,Li XB and Chen LK.2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the geochronology and geochemistry of mafic rocks within ophiolites.Lithos,245:18-33
Wang LQ,Wang Y,Danzhen WX,Li BL,Li Z,Li S,Fan Y,Li W and Gong FZ.2017.A tentative discussion on metallogeny of the main magmatic-hydrothermal ore deposits in the western Bangong CoNujiang metallogenic belt,Tibet.Acta Geoscientica Sinica,38(5):615-626(in Chinese with English abstract)
Wang Q,Zhu DC,Zhao ZD,Liu SA,Chung SL,Li SM,Liu D,Dai JG,Wang LQ and Mo XX.2014.Origin of the ca.90Ma magnesiarich volcanic rocks in SE Nyima,central Tibet:Products of lithospheric delamination beneath the Lhasa-Qiangtang collision zone.Lithos,198-199:24-37
Wang Y,Wang LQ,Danzhen WX,Li Z and Li S.2017.The discovery of Late Jurassic rhyolite porphyry in Geji area,southern Bangong CoNujiang suture zone,Tibet:Constraints from zircon U-Pb geochronology,geochemistry and Hf isotopes.Acta Geoscientica Sinica,38(5):723-733(in Chinese with English abstract)
Wang Y,Tang JX,Wang LQ,Duan JL,Danzhen WX,Li S and Li Z.2018.Petrogenesis of Jurassic granitoids in the west central Lhasa subterrane,Tibet,China:The Geji example.International Geology Review,60(9):1155-1171
Whalen JB.1985.Geochemistry of an island-arc plutonic suite:The Uasilau-yau Yau intrusive complex,New Britain,P.N.G.Journal of Petrology,26(3):603-632
Whalen JB,Currie KL and Chappell BW.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419
White AJR and Chappell BW.1983.Granitoid types and their distribution in the Lachlan Fold Belt,Southeastern Australia.Geological Society of America Memoirs,159:21-34
Wolf MB and Wyllie PJ.1994.Dehydratiom-melting of amphibolite at10kbar:The effects of temperature and time.Contributions to Mineralogy and Petrology,115(4):369-383
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Wu H,Li C,Xu MJ and Li XK.2015.Early Cretaceous adakitic magmatism in the Dachagou area,northern Lhasa terrane,Tibet:Implications for slab roll-back and subsequent slab break-off of the lithosphere of the Bangong-Nujiang Ocean.Journal of Asian Earth Sciences,97:51-66
Xia B,Xu LF,Wei ZQ,Zhang YQ,Wang R,Li JF and Wang YB.2008.SHRIMP zircon dating of gabbro from the Donqiao ophiolite in Tibet and its geological implication.Acta Geologica Sinica,82(4):528-531(in Chinese with English abstract)
Yan JJ.2016.Chronology and geochemistry of magmatic rocks of the Xuru Tso batholith in Central Lhasa Terrane,Tibet.Master Degree Thesis.Beijing:China University of Geosciences,1-60(in Chinese with English summary)
Yao XF,Tang JX,Li ZJ,Deng SL,Ding S,Hu ZH and Zhang Z.2012.Magma origin of two plutons from Gaerqiong copper-gold deposit and it’s geological significance,western Bangonghu-Nujiang metallogenic belt,Tibet:Implication from Hf isotope characteristics.Journal of Jilin University(Earth Science Edition),42(Suppl.2):188-197(in Chinese with English abstract)
Yao XF,Tang JX,Li ZJ,Deng SL,Ding S,Hu ZH and Zhang Z.2013.The redefinition of the ore-forming porphyry’s age in Gaerqiong skarn-type gold-copper deposit,western Bangong LakeNujiang River metallogenic belt,Xizang(Tibet).Geological Review,59(1):193-200(in Chinese with English abstract)
Zhang LL,Zhu DC,Zhao ZD,Dong GC,Mo XX,Guan Q,Liu M and Liu MH.2010.Petrogenesis of magmatism in the Baerda region of northern Gangdese,Tibet:Constraints from geochemistry,geochronology and Sr-Nd-Hf isotopes.Acta Petrologica Sinica,26(6):1871-1888(in Chinese with English abstract)
Zhang LL,Zhu DC,Zhao ZD,Liao ZL,Wang LQ and Mo XX.2011.Early Cretaceous granitoids in Xainza,Tibet:Evidence of slab break-off.Acta Petrologica Sinica,27(7):1938-1948(in Chinese with English abstract)
Zhang XQ,Zhu DC,Zhao ZD,Wang LQ,Huang JC and Mo XX.2010.Petrogenesis of the Nixiong pluton in Coqen,Tibet and its potential significance for the Nixiong Fe-rich mineralization.Acta Petrologica Sinica,26(6):1793-1804(in Chinese with English abstract)
Zhang Z,Tang JX,Yao XF,Song JL and He L.2013.The discovery and the tectonic implications of the Late Jurassic arc-related diorite in the Ga’erqiong-Galale copper-gold concentrated area,Tibet.Acta Mineralogica Sinica,33(S2):872-873(in Chinese)
Zhang ZC,Dong SY,Huang H,Ma LT,Zhang DY,Zhang S and Xue CJ.2009.Geology and geochemistry of the Permian intermediateacid intrusions in the southwestern Tianshan,Xinjiang,China:Implications for petrogenesis and tectonics.Geological Bulletin of China,28(12):1827-1839(in Chinese with English abstract)
Zhu DC,Pan GT,Mo XX,Wang LQ,Liao ZL,Zhao ZD,Dong GC and Zhou CY.2006.Late Jurassic-Early Cretaceous geodynamic setting in middle-northern Gangdese:New insights from volcanic rocks.Acta Petrologica Sinica,22(3):534-546(in Chinese with English abstract)
Zhu DC,Pan GT,Chung SL,Liao ZL,Wang LQ and Li GM.2008.SHRIMP zircon age and geochemical constraints on the origin of Lower Jurassic volcanic rocks from the Yeba Formation,southern Gangdese,south Tibet.International Geology Review,50(5):442-471
Zhu DC,Mo XX,Zhao ZD,Xu JF,Zhou CY,Sun CG,Wang LQ,Chen HH,Dong GC and Zhou S.2008.Zircon U-Pb geochronology of Zenong Group volcanic rocks in Coqen area of the Gangdese,Tibet and tectonic significance.Acta Petrologica Sinica,24(3):401-412(in Chinese with English abstract)
Zhu DC,Mo XX,Niu YL,Zhao ZD,Wang LQ,Liu YS and Wu FY.2009a.Geochemical investigation of Early Cretaceous igneous rocks along an east-west traverse throughout the central Lhasa Terrane,Tibet.Chemical Geology,268(3-4):298-312
Zhu DC,Chung SL,Mo XX,Zhao ZD,Niu YL,Song B and Yang YH.2009b.The 132Ma Comei-Bunbury large igneous province:Remnants identified in present-day southeastern Tibet and southwestern Australia.Geology,37(7):583-586
Zhu DC,Zhao ZD,Pan GT,Lee HY,Kang ZQ,Liao ZL,Wang LQ,Li GM,Dong GC and Liu B.2009c.Early Cretaceous subductionrelated adakite-like rocks of the Gangdese belt,southern Tibet:Products of slab melting and subsequent melt-peridotite interaction?Journal of Asian Earth Sciences,34(3):298-309
Zhu DC,Zhao ZD,Niu YL,Mo XX,Chung SL,Hou ZQ,Wang LQ and Wu FY.2011.The Lhasa terrane:Record of a microcontinent and its histories of drift and growth.Earth and Planetary Science Letters,301(1-2):241-255
Zhu DC,Li SM,Cawood PA,Wang Q,Zhao ZD,Liu SA and Wang LQ.2016.Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction.Lithos,245:7-17
Zorpi MJ,Coulon C and Orsini JB.1991.Hybridization between felsic and mafic magmas in calc-alkaline granitoids:A case study in northern Sardinia,Italy.Chemical Geology,92(1-3):45-86
陈越,朱弟成,赵志丹,张亮亮,刘敏,于枫,管琪,莫宣学.2010.西藏北冈底斯巴木错安山岩的年代学、地球化学及岩石成因.岩石学报,26(7):2193-2206
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报,27(7):1993-2002
杜德道.2012.西藏班公湖-怒江缝合带(中段和西段)的花岗岩地球化学特征及其构造环境.硕士学位论文.北京:中国地质大学,1-52
侯可军,李延河,邹天人,曲晓明,石玉若,谢桂青.2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10):2595-2604
姜昕,赵志丹,朱弟成,张凤琴,董国臣,莫宣学,郭铁鹰.2010.西藏冈底斯西部江巴、邦巴和雄巴岩体的锆石U-Pb年代学与Hf同位素地球化学.岩石学报,26(7):2155-2164
康志强,许继峰,董彦辉,王保弟.2008.拉萨地块中北部白垩纪则弄群火山岩:Slainajap洋南向俯冲的产物?岩石学报,24(2):303-314
康志强,许继峰,王保弟,陈建林.2010.拉萨地块北部去申拉组火山岩:班公湖-怒江特提斯洋南向俯冲的产物?岩石学报,26(10):3106-3116
李光明,段志明,刘波,张晖,董随亮,张丽.2011.西藏班公湖-怒江结合带北缘多龙地区侏罗纪增生杂岩的特征及意义.地质通报,30(8):1256-1260
李献华,李武显,王选策,李秋立,刘宇,唐国强.2009.幔源岩浆在南岭燕山早期花岗岩形成中的作用:锆石原位Hf-O同位素制约.中国科学(D辑),39(7):872-887
李艳广,汪双双,刘民武,孟恩,魏小燕,赵慧博,靳梦琪.2015.斜锆石LA-ICP-MS U-Pb定年方法及应用.地质学报,89(12):2400-2418
李志军,赵润东,何子轩,张志,李丕蓉,尤孟,何珊,郭奇奇,欧俊.2017.西藏嘎拉勒铜金矿床成矿物质来源探讨---来自硫、铅、碳和氢氧同位素地球化学特征的证据.地球学报,38(5):651-658
吕立娜,崔玉斌,宋亮,赵元艺,曲晓明,王江朋.2011.西藏嘎拉勒夕卡岩型金(铜)矿床地球化学特征与锆石的LA-ICP-MS定年及意义.地学前缘,18(5):224-242
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523-535
冉皞,王根厚,梁晓,郑艺龙,久米多吉.2015.青藏高原南羌塘荣玛晚侏罗世闪长岩:班公湖-怒江特提斯洋向北俯冲产物.地质通报,34(5):815-825
唐菊兴,宋扬,王勤,林彬,杨超,郭娜,方向,杨欢欢,王艺云,高轲,丁帅,张志,段吉琳,陈红旗,粟登逵,冯军,刘治博,韦少港,贺文,宋俊龙,李彦波,卫鲁杰.2016.西藏铁格隆南铜(金银)矿床地质特征及勘查模型---西藏首例千万吨级斑岩-浅成低温热液型矿床.地球学报,37(6):663-690
唐菊兴,王勤,杨欢欢,高昕,张泽斌,邹兵.2017.西藏斑岩-矽卡岩-浅成低温热液铜多金属矿成矿作用、勘查方向与资源潜力.地球学报,38(5):571-613
王立强,王勇,旦真王修,李宝龙,李壮,李申,范源,李威,龚福志.2017.班公湖-怒江成矿带西段主要岩浆热液型矿床成矿特征初探.地球学报,38(5):615-626
王勇,王立强,旦真王修,李壮,李申.2017.西藏班公湖-怒江结合带南缘革吉地区晚侏罗世流纹斑岩的成因---锆石U-Pb定年、地球化学和Hf同位素约束.地球学报,38(5):723-733
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
夏斌,徐力峰,韦振权,张玉泉,王冉,李建峰,王彦斌.2008.西藏东巧蛇绿岩中辉长岩锆石SHRIMP定年及其地质意义.地质学报,82(4):528-531
闫晶晶.2016.西藏中拉萨地块许如错岩体年代学和地球化学.硕士学位论文.北京:中国地质大学,1-60
姚晓峰,唐菊兴,李志军,邓世林,丁帅,胡正华,张志.2012.班怒带西段尕尔穷铜金矿两套侵入岩源区及其地质意义---来自Hf同位素特征的指示.吉林大学学报(地球科学版),42(增2):188-197
姚晓峰,唐菊兴,李志军,邓世林,丁帅,胡正华,张志.2013.班公湖-怒江带西段尕尔穷矽卡岩型铜金矿含矿母岩成岩时代的重新厘定及其地质意义.地质论评,59(1):193-200
张亮亮,朱弟成,赵志丹,董国臣,莫宣学,管琪,刘敏,刘美华.2010.西藏北冈底斯巴尔达地区岩浆作用的成因:地球化学、年代学及Sr-Nd-Hf同位素约束.岩石学报,26(6):1871-1888
张亮亮,朱弟成,赵志丹,廖忠礼,王立全,莫宣学.2011.西藏申扎早白垩世花岗岩类:板片断离的证据.岩石学报,27(7):1938-1948
张晓倩,朱弟成,赵志丹,王立全,黄建村,莫宣学.2010.西藏措勤尼雄岩体的岩石成因及其对富Fe成矿作用的潜在意义.岩石学报,26(6):1793-1804
张志,唐菊兴,姚晓峰,宋俊龙,何林.2013.西藏尕尔穷-嘎拉勒铜金矿集区中侏罗世晚期岛弧闪长岩的厘定及其构造意义.矿物学报,33(S2):872-873
张招崇,董书云,黄河,马乐天,张东阳,张舒,薛春纪.2009.西南天山二叠纪中酸性侵入岩的地质学和地球化学:岩石成因和构造背景.地质通报,28(12):1827-1839
朱弟成,潘桂堂,莫宣学,王立全,廖忠礼,赵志丹,董国臣,周长勇.2006.冈底斯中北部晚侏罗世-早白垩世地球动力学环境:火山岩约束.岩石学报,22(3):534-546
朱弟成,莫宣学,赵志丹,许继峰,周长勇,孙晨光,王立全,陈海红,董国臣,周肃.2008.西藏冈底斯带措勤地区则弄群火山岩锆石U-Pb年代学格架及构造意义.岩石学报,24(3):401-412
(1)四川省地质调查院.2003.1/250000革吉县幅区域地质调查报告
Blichert TJ and Albarède F.1997.The Lu-Hf geochemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148:243-258
Cao MJ,Qin KZ,Li GM,Li JX,Zhao JX,Evans NJ and Hollings P.2016.Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane,Tibet.Gondwana Research,39:386-400
Chappell BW and White AJR.1974.Two contrasting granite types.Pacific Geology,8(2):173-174
Chappell BW and White AJR.1992.I-and S-type granites in the Lachlan fold belt.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,83(1-2):1-26
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Chappell BW,Bryant CJ and Wyborn D.2012.Peraluminous I-type granites.Lithos,153:142-153
Chen Y,Zhu DC,Zhao ZD,Zhang LL,Liu M,Yu F,Guan Q and Mo XX.2010.Geochronology,geochemistry and petrogenesis of the Bamco andesites from the northern Gangdese,Tibet.Acta Petrologica Sinica,26(7):2193-2206(in Chinese with English abstract)
Chen Y,Zhu DC,Zhao ZD,Meng FY,Wang Q,Santosh M,Wang LQ,Dong GC and Mo XX.2014.Slab breakoff triggered ca.113Ma magmatism around Xainza area of the Lhasa Terrane,Tibet.Gondwana Research,26(2):449-463
Clemens JD.2003.S-type granitic magmas-petrogenetic issues,models and evidence.Earth-Science Reviews,61(1-2):1-18
Collins WJ,Beams SD,White AJR and Chappell BW.1982.Nature and origin of A-type granites with particular reference to southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200
Collins WJ and Richards SW.2008.Geodynamic significance of S-type granites in circum-Pacific orogens.Geology,36(7):559-562
Coney PJ and Reynolds SJ.1977.Cordilleran Benioff zones.Nature,270(5636):403-406
Coulon C,Maluski H,Bollinger C and Wang S.1986.Mesozoic and Cenozoic volcanic rocks from central and southern Tibet:30Ar-40Ar dating,petrological characteristics and geodynamical significance.Earth and Planetary Science Letters,79(3-4):281-302
Crosson RS and Owens TJ.1987.Slab geometry of the Cascadia subduction zone beneath Washington from earthquake hypocenters and teleseismic converted waves.Geophysical Research Letters,14(8):824-827
Defant MJ and Drummond MS.1990.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,347(6294):662-665
Ding L,Kapp P,Zhong DL and Deng WM.2003.Cenozoic volcanism in Tibet:Evidence for a transition from oceanic to continental subduction.Journal of Petrology,44(10):1833-1865
Du DD,Qu XM,Wang GH,Xin HB and Liu ZB.2011.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang suture,Tibet:Evidence from zircon U-Pb LAICPMS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993-2002(in Chinese with English abstract)
Du DD.2012.Geochemical characteristics and implications for tectonic settings of the middle segment and western segment of Bangong LakeNu River suture,the Tibet Plateau.Master Degree Thesis.Beijing:China University of Geosciences,1-52(in Chinese with English summary)
Geng QR,Zhang Z,Peng ZM,Guan JL,Zhu XP and Mao XC.2016.Jurassic-Cretaceous granitoids and related tectono-metallogenesis in the Zapug-Duobuza arc,western Tibet.Ore Geology Reviews,77:163-175
Griffin WL,Pearson NJ,Belousova E,Jackson SE,Achterbergh EV,O’Reilly SY and Shee SR.2000.The Hf isotope compositon of cratonic mantle:LAM-MC-ICP-MS analysis of zircon magacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin WL,Wang X,Jackson SE,Pearspm NJ,O’Reilly SY,Xu XSand Zhou XM.2002.Zircon chemistry and magma mixing,SEChina:In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269
Gutscher MA,Olivet JL,Aslanian D,Eissen JP and Maury R.1999.The“lost inca plateau”:Cause of flat subduction beneath Peru?Earth and Planetary Science Letters,171(3):335-341
Guynn JH,Kapp P,Pullen A,Heizler M,Gehrels G and Ding L.2006.Tibetan basement rocks near Amdo reveal“missing”Mesozoic tectonism along the Bangong suture,central Tibet.Geology,34(6):505-508
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hou KJ,Li YH,Zou TR,Qu XM,Shi YR and Xie GQ.2007.Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications.Acta Petrologica Sinica,23(10):2595-2604(in Chinese with English abstract)
Ji WQ,Wu FY,Chung SL,Li JX and Liu CZ.2009.Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith,southern Tibet.Chemical Geology,262(3-4):229-245
Jiang X,Zhao ZD,Zhu DC,Zhang FQ,Dong GC,Mo XX and Guo TY.2010.Zircon U-Pb geochronology and Hf isotopic geochemistry of Jiangba,Bangba,and Xiongba granitoids in western Gangdese,Tibet.Acta Petrologica Sinica,26(7):2155-2164(in Chinese with English abstract)
Kang ZQ,Xu JF,Dong YH and Wang BD.2008.Cretaceous volcanic rocks of Zenong Group in north-middle Lhasa block:Products of southward subducting of the Slainajap ocean?Acta Petrologica Sinica,24(2):303-314(in Chinese with English abstract)
Kang ZQ,Xu JF,Wang BD and Chen JL.2010.Qushenla formation volcanic rocks in north Lhasa block:Products of Bangong Co-Nujiang Tethy’s southward subduction.Acta Petrologica Sinica,26(10):3106-3116(in Chinese with English abstract)
Kapp P,De Celles PG,Gehrels GE,Heizler M and Ding L.2007.Geological records of the Lhasa-Qiangtang and Indo-Asian collisions in the Nima area of Central Tibet.GSA Bulletin,119(7-8):917-933
Karsli O,Chen B,Aydin F and爦en C.2007.Geochemical and Sr-NdPb isotopic compositions of the Eocene D9lek and Sari9i9ek Plutons,Eastern Turkey:Implications for magma interaction in the genesis of high-K calc-alkaline granitoids in a post-collision extensional setting.Lithos,98(1-4):67-96
Kaygusuz A and Aydn9akr E.2009.Mineralogy,whole-rock and Sr-Nd isotope geochemistry of mafic microgranular enclaves in Cretaceous Dagbasi granitoids,Eastern Pontides,NE Turkey:Evidence of magma mixing,mingling and chemical equilibration.Chemie der Erde-Geochemistry,69(3):247-277
Kemp AIS,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
Le Maitre RW.2002.Igneous Rocks:A Classification and Glossary of Terms:Recommendations of the International Union of Geological Sciences,Subcommission on the Systematics of Igneous Rocks.2nd Edition.Cambridge:Cambridge University Press,33-39
Li BL,Song Y,Peng B,Gong FZ,Yang SG and Zhou L.2018.Discovery of ophiolitic mélange in the north region of Geji County,Northwest Tibet and its zircon U-Pb age.Acta Geologica Sinica,92(5):2032-2033
Li GM,Duan ZM,Liu B,Zhang H,Dong SL and Zhang L.2011.The discovery of Jurassic accretionary complexes in Duolong area,northern Bangong Co-Nujiang suture zone,Tibet,and its geologic significance.Geological Bulletin of China,30(8):1256-1260(in Chinese with English abstract)
Li JX,Qin KZ,Li GM,Richards JP,Zhao JX and Cao MJ.2014.Geochronology,geochemistry,and zircon Hf isotopic compositions of Mesozoic intermediate-felsic intrusions in central Tibet:Petrogenetic and tectonic implications.Lithos,198-199:77-91
Li XH,Li WY,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role of mantle-derived magma in genesis of Early Yanshanian granites in the Nanling Range,South China:In situ zircon Hf-O isotopic constraints.Science in China(Series D),52(9):1262-1278
Li YG,Wang SS,Liu MW,Meng E,Wei XY,Zhao HB and Jin MQ.2015.U-Pb dating study of baddeleyite by LA-ICP-MS:Technique and application.Acta Geologica Sinica,89(12):2400-2418(in Chinese with English abstract)
Li ZJ,Zhao RD,He ZX,Zhang Z,Li PR,You M,He S,Guo QQ and Ou J.2017.Source of ore-forming materials in the Galale coppergold deposit of Tibet:Evidence from geochemical characteristics of sulfur,lead,carbon and hydrogen-oxygen isotopes.Acta Geoscientica Sinica,38(5):651-658(in Chinese with English abstract)
Lin B,Tang JX,Chen YC,Song Y,Hall G,Wang Q,Yang C,Fang X,Duan JL,Yang HH,Liu ZB,Wang YY and Feng J.2017.Geochronology and genesis of the Tiegelongnan porphyry Cu(Au)deposit in Tibet:Evidence from U-Pb,Re-Os dating and Hf,S,and H-O isotopes.Resource Geology,67(1):1-21
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Livaccari RF,Burke K and爦eng9r AMC.1981.Was the Laramide orogeny related to subduction of an oceanic plateau?Nature,289(5795):276-278
Loiselle MC and Wones DR.1979.Characteristics and origin of anorogenic granites.Geological of Society of America,11(7):468
Ludwig KR.2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley,CA:Berkeley Geochronology Center,1-70
LüLN,Cui YB,Song L,Zhao YY,Qu XM and Wang JP.2011.Geochemical characteristics and zircon LA-ICP-MS U-Pb dating of Galale skarn gold(copper)deposit,Tibet and its significance.Earth Science Frontiers,18(5):224-242(in Chinese with English abstract)
Meng E,Liu FL,Liu PH,Liu CH,Yang H,Wang F,Shi JR and Cai J.2014.Petrogenesis and tectonic significance of Paleoproterozoic meta-mafic rocks from central Liaodong Peninsula,northeast China:Evidence from zircon U-Pb dating and in situ Lu-Hf isotopes,and whole-rock geochemistry.Precambrian Research,247:92-109
Middlemost EAK.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3-4):215-224
Murphy MA,Yin A,Harrison TM,Dürr SB,Chen Z,Ryerson FJ,Kidd WSF,Wang X and Zhou X.1997.Did the Indo-Asian collision alone create the Tibetan Plateau?Geology,25(8):719-722
Peccerillo A and Taylor SR.1976.Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81
Pitcher WS.1997.The Nature and Origin of Granite.2ndEdition.London:Chapman&Hall,1-386
Pullen A,Kapp P,Gehrels GE,Ding L and Zhang QH.2011.Metamorphic rocks in central Tibet:Lateral variations and implications for crustal structure.GSA Bulletin,123(3-4):585-600
Qu XM,Wang RJ,Xin HB,Zhao YY and Fan XT.2009.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523-535(in Chinese with English abstract)
Ran H,Wang GH,Liang X,Zheng YL and Jiumi DJ.2015.The Late Jurassic diorite in Rongma area,southern Qiangtang Terrane,Tibetan Plateau:Product of northward subduction of the Bangong CoNujiang River Tethys ocean.Geological Bulletin of China,34(5):815-825(in Chinese with English abstract)
Ravikant V,Wu FY and Ji WQ.2011.U-Pb age and Hf isotopic constraints of detrital zircons from the Himalayan foreland Subathu sub-basin on the Tertiary palaeogeography of the Himalaya.Earth and Planetary Science Letters,304(3-4):356-368
Shi RD.2007.SHRIMP dating of the Bangong Lake SSZ-type ophiolite:Constraints on the closure time of ocean in the Bangong Lake-Nujiang River,northwestern Tibet.Chinese Science Bulletin,52(7):936-941
Song Y,Yang C,Wei SG,Yang HH,Fang X and Lu HT.2018.Tectonic control,reconstruction and preservation of the Tiegelongnan porphyry and epithermal overprinting Cu(Au)deposit,Central Tibet,China.Minerals,8(9):398
S9derlund U,Patchett PJ,Vervoort JD and Isachsen CE.2004.The176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Tang JX,Song Y,Wang Q,Lin B,Yang C,Guo N,Fang X,Yang HH,Wang YY,Gao K,Ding S,Zhang Z,Duan JL,Chen HQ,Su DK,Feng J,Liu ZB,Wei SG,He W,Song JL,Li YB and Wei LJ.2016.Geological characteristics and exploration model of the Tiegelongnan Cu(Au-Ag)deposit:The first ten million tons metal resources of a porphyry-epithermal deposit in Tibet.Acta Geoscientica Sinica,37(6):663-690(in Chinese with English abstract)
Tang JX,Wang Q,Yang HH,Gao X,Zhang ZB and Zou B.2017.Mineralization,exploration and resource potential of porphyry-skarnepithermal copper polymetallic deposits in Tibet.Acta Geoscientica Sinica,38(5):571-613(in Chinese with English abstract)
van Achterbergh E,Ryan CG,Jackson SE and Griffin WL.2001.Data reduction software for LA-ICP-MS.In:Sylvester PJ(ed.).LaserAblation-ICPMS in the Earth Sciences:Principles and Applications.Ottawa,Ontario,Canada:Mineralogical Association of Canada,239-243
Wang BD,Wang LQ,Chung SL,Chen JL,Yin FG,Liu H,Li XB and Chen LK.2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the geochronology and geochemistry of mafic rocks within ophiolites.Lithos,245:18-33
Wang LQ,Wang Y,Danzhen WX,Li BL,Li Z,Li S,Fan Y,Li W and Gong FZ.2017.A tentative discussion on metallogeny of the main magmatic-hydrothermal ore deposits in the western Bangong CoNujiang metallogenic belt,Tibet.Acta Geoscientica Sinica,38(5):615-626(in Chinese with English abstract)
Wang Q,Zhu DC,Zhao ZD,Liu SA,Chung SL,Li SM,Liu D,Dai JG,Wang LQ and Mo XX.2014.Origin of the ca.90Ma magnesiarich volcanic rocks in SE Nyima,central Tibet:Products of lithospheric delamination beneath the Lhasa-Qiangtang collision zone.Lithos,198-199:24-37
Wang Y,Wang LQ,Danzhen WX,Li Z and Li S.2017.The discovery of Late Jurassic rhyolite porphyry in Geji area,southern Bangong CoNujiang suture zone,Tibet:Constraints from zircon U-Pb geochronology,geochemistry and Hf isotopes.Acta Geoscientica Sinica,38(5):723-733(in Chinese with English abstract)
Wang Y,Tang JX,Wang LQ,Duan JL,Danzhen WX,Li S and Li Z.2018.Petrogenesis of Jurassic granitoids in the west central Lhasa subterrane,Tibet,China:The Geji example.International Geology Review,60(9):1155-1171
Whalen JB.1985.Geochemistry of an island-arc plutonic suite:The Uasilau-yau Yau intrusive complex,New Britain,P.N.G.Journal of Petrology,26(3):603-632
Whalen JB,Currie KL and Chappell BW.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419
White AJR and Chappell BW.1983.Granitoid types and their distribution in the Lachlan Fold Belt,Southeastern Australia.Geological Society of America Memoirs,159:21-34
Wolf MB and Wyllie PJ.1994.Dehydratiom-melting of amphibolite at10kbar:The effects of temperature and time.Contributions to Mineralogy and Petrology,115(4):369-383
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Wu H,Li C,Xu MJ and Li XK.2015.Early Cretaceous adakitic magmatism in the Dachagou area,northern Lhasa terrane,Tibet:Implications for slab roll-back and subsequent slab break-off of the lithosphere of the Bangong-Nujiang Ocean.Journal of Asian Earth Sciences,97:51-66
Xia B,Xu LF,Wei ZQ,Zhang YQ,Wang R,Li JF and Wang YB.2008.SHRIMP zircon dating of gabbro from the Donqiao ophiolite in Tibet and its geological implication.Acta Geologica Sinica,82(4):528-531(in Chinese with English abstract)
Yan JJ.2016.Chronology and geochemistry of magmatic rocks of the Xuru Tso batholith in Central Lhasa Terrane,Tibet.Master Degree Thesis.Beijing:China University of Geosciences,1-60(in Chinese with English summary)
Yao XF,Tang JX,Li ZJ,Deng SL,Ding S,Hu ZH and Zhang Z.2012.Magma origin of two plutons from Gaerqiong copper-gold deposit and it’s geological significance,western Bangonghu-Nujiang metallogenic belt,Tibet:Implication from Hf isotope characteristics.Journal of Jilin University(Earth Science Edition),42(Suppl.2):188-197(in Chinese with English abstract)
Yao XF,Tang JX,Li ZJ,Deng SL,Ding S,Hu ZH and Zhang Z.2013.The redefinition of the ore-forming porphyry’s age in Gaerqiong skarn-type gold-copper deposit,western Bangong LakeNujiang River metallogenic belt,Xizang(Tibet).Geological Review,59(1):193-200(in Chinese with English abstract)
Zhang LL,Zhu DC,Zhao ZD,Dong GC,Mo XX,Guan Q,Liu M and Liu MH.2010.Petrogenesis of magmatism in the Baerda region of northern Gangdese,Tibet:Constraints from geochemistry,geochronology and Sr-Nd-Hf isotopes.Acta Petrologica Sinica,26(6):1871-1888(in Chinese with English abstract)
Zhang LL,Zhu DC,Zhao ZD,Liao ZL,Wang LQ and Mo XX.2011.Early Cretaceous granitoids in Xainza,Tibet:Evidence of slab break-off.Acta Petrologica Sinica,27(7):1938-1948(in Chinese with English abstract)
Zhang XQ,Zhu DC,Zhao ZD,Wang LQ,Huang JC and Mo XX.2010.Petrogenesis of the Nixiong pluton in Coqen,Tibet and its potential significance for the Nixiong Fe-rich mineralization.Acta Petrologica Sinica,26(6):1793-1804(in Chinese with English abstract)
Zhang Z,Tang JX,Yao XF,Song JL and He L.2013.The discovery and the tectonic implications of the Late Jurassic arc-related diorite in the Ga’erqiong-Galale copper-gold concentrated area,Tibet.Acta Mineralogica Sinica,33(S2):872-873(in Chinese)
Zhang ZC,Dong SY,Huang H,Ma LT,Zhang DY,Zhang S and Xue CJ.2009.Geology and geochemistry of the Permian intermediateacid intrusions in the southwestern Tianshan,Xinjiang,China:Implications for petrogenesis and tectonics.Geological Bulletin of China,28(12):1827-1839(in Chinese with English abstract)
Zhu DC,Pan GT,Mo XX,Wang LQ,Liao ZL,Zhao ZD,Dong GC and Zhou CY.2006.Late Jurassic-Early Cretaceous geodynamic setting in middle-northern Gangdese:New insights from volcanic rocks.Acta Petrologica Sinica,22(3):534-546(in Chinese with English abstract)
Zhu DC,Pan GT,Chung SL,Liao ZL,Wang LQ and Li GM.2008.SHRIMP zircon age and geochemical constraints on the origin of Lower Jurassic volcanic rocks from the Yeba Formation,southern Gangdese,south Tibet.International Geology Review,50(5):442-471
Zhu DC,Mo XX,Zhao ZD,Xu JF,Zhou CY,Sun CG,Wang LQ,Chen HH,Dong GC and Zhou S.2008.Zircon U-Pb geochronology of Zenong Group volcanic rocks in Coqen area of the Gangdese,Tibet and tectonic significance.Acta Petrologica Sinica,24(3):401-412(in Chinese with English abstract)
Zhu DC,Mo XX,Niu YL,Zhao ZD,Wang LQ,Liu YS and Wu FY.2009a.Geochemical investigation of Early Cretaceous igneous rocks along an east-west traverse throughout the central Lhasa Terrane,Tibet.Chemical Geology,268(3-4):298-312
Zhu DC,Chung SL,Mo XX,Zhao ZD,Niu YL,Song B and Yang YH.2009b.The 132Ma Comei-Bunbury large igneous province:Remnants identified in present-day southeastern Tibet and southwestern Australia.Geology,37(7):583-586
Zhu DC,Zhao ZD,Pan GT,Lee HY,Kang ZQ,Liao ZL,Wang LQ,Li GM,Dong GC and Liu B.2009c.Early Cretaceous subductionrelated adakite-like rocks of the Gangdese belt,southern Tibet:Products of slab melting and subsequent melt-peridotite interaction?Journal of Asian Earth Sciences,34(3):298-309
Zhu DC,Zhao ZD,Niu YL,Mo XX,Chung SL,Hou ZQ,Wang LQ and Wu FY.2011.The Lhasa terrane:Record of a microcontinent and its histories of drift and growth.Earth and Planetary Science Letters,301(1-2):241-255
Zhu DC,Li SM,Cawood PA,Wang Q,Zhao ZD,Liu SA and Wang LQ.2016.Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction.Lithos,245:7-17
Zorpi MJ,Coulon C and Orsini JB.1991.Hybridization between felsic and mafic magmas in calc-alkaline granitoids:A case study in northern Sardinia,Italy.Chemical Geology,92(1-3):45-86
陈越,朱弟成,赵志丹,张亮亮,刘敏,于枫,管琪,莫宣学.2010.西藏北冈底斯巴木错安山岩的年代学、地球化学及岩石成因.岩石学报,26(7):2193-2206
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报,27(7):1993-2002
杜德道.2012.西藏班公湖-怒江缝合带(中段和西段)的花岗岩地球化学特征及其构造环境.硕士学位论文.北京:中国地质大学,1-52
侯可军,李延河,邹天人,曲晓明,石玉若,谢桂青.2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10):2595-2604
姜昕,赵志丹,朱弟成,张凤琴,董国臣,莫宣学,郭铁鹰.2010.西藏冈底斯西部江巴、邦巴和雄巴岩体的锆石U-Pb年代学与Hf同位素地球化学.岩石学报,26(7):2155-2164
康志强,许继峰,董彦辉,王保弟.2008.拉萨地块中北部白垩纪则弄群火山岩:Slainajap洋南向俯冲的产物?岩石学报,24(2):303-314
康志强,许继峰,王保弟,陈建林.2010.拉萨地块北部去申拉组火山岩:班公湖-怒江特提斯洋南向俯冲的产物?岩石学报,26(10):3106-3116
李光明,段志明,刘波,张晖,董随亮,张丽.2011.西藏班公湖-怒江结合带北缘多龙地区侏罗纪增生杂岩的特征及意义.地质通报,30(8):1256-1260
李献华,李武显,王选策,李秋立,刘宇,唐国强.2009.幔源岩浆在南岭燕山早期花岗岩形成中的作用:锆石原位Hf-O同位素制约.中国科学(D辑),39(7):872-887
李艳广,汪双双,刘民武,孟恩,魏小燕,赵慧博,靳梦琪.2015.斜锆石LA-ICP-MS U-Pb定年方法及应用.地质学报,89(12):2400-2418
李志军,赵润东,何子轩,张志,李丕蓉,尤孟,何珊,郭奇奇,欧俊.2017.西藏嘎拉勒铜金矿床成矿物质来源探讨---来自硫、铅、碳和氢氧同位素地球化学特征的证据.地球学报,38(5):651-658
吕立娜,崔玉斌,宋亮,赵元艺,曲晓明,王江朋.2011.西藏嘎拉勒夕卡岩型金(铜)矿床地球化学特征与锆石的LA-ICP-MS定年及意义.地学前缘,18(5):224-242
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523-535
冉皞,王根厚,梁晓,郑艺龙,久米多吉.2015.青藏高原南羌塘荣玛晚侏罗世闪长岩:班公湖-怒江特提斯洋向北俯冲产物.地质通报,34(5):815-825
唐菊兴,宋扬,王勤,林彬,杨超,郭娜,方向,杨欢欢,王艺云,高轲,丁帅,张志,段吉琳,陈红旗,粟登逵,冯军,刘治博,韦少港,贺文,宋俊龙,李彦波,卫鲁杰.2016.西藏铁格隆南铜(金银)矿床地质特征及勘查模型---西藏首例千万吨级斑岩-浅成低温热液型矿床.地球学报,37(6):663-690
唐菊兴,王勤,杨欢欢,高昕,张泽斌,邹兵.2017.西藏斑岩-矽卡岩-浅成低温热液铜多金属矿成矿作用、勘查方向与资源潜力.地球学报,38(5):571-613
王立强,王勇,旦真王修,李宝龙,李壮,李申,范源,李威,龚福志.2017.班公湖-怒江成矿带西段主要岩浆热液型矿床成矿特征初探.地球学报,38(5):615-626
王勇,王立强,旦真王修,李壮,李申.2017.西藏班公湖-怒江结合带南缘革吉地区晚侏罗世流纹斑岩的成因---锆石U-Pb定年、地球化学和Hf同位素约束.地球学报,38(5):723-733
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
夏斌,徐力峰,韦振权,张玉泉,王冉,李建峰,王彦斌.2008.西藏东巧蛇绿岩中辉长岩锆石SHRIMP定年及其地质意义.地质学报,82(4):528-531
闫晶晶.2016.西藏中拉萨地块许如错岩体年代学和地球化学.硕士学位论文.北京:中国地质大学,1-60
姚晓峰,唐菊兴,李志军,邓世林,丁帅,胡正华,张志.2012.班怒带西段尕尔穷铜金矿两套侵入岩源区及其地质意义---来自Hf同位素特征的指示.吉林大学学报(地球科学版),42(增2):188-197
姚晓峰,唐菊兴,李志军,邓世林,丁帅,胡正华,张志.2013.班公湖-怒江带西段尕尔穷矽卡岩型铜金矿含矿母岩成岩时代的重新厘定及其地质意义.地质论评,59(1):193-200
张亮亮,朱弟成,赵志丹,董国臣,莫宣学,管琪,刘敏,刘美华.2010.西藏北冈底斯巴尔达地区岩浆作用的成因:地球化学、年代学及Sr-Nd-Hf同位素约束.岩石学报,26(6):1871-1888
张亮亮,朱弟成,赵志丹,廖忠礼,王立全,莫宣学.2011.西藏申扎早白垩世花岗岩类:板片断离的证据.岩石学报,27(7):1938-1948
张晓倩,朱弟成,赵志丹,王立全,黄建村,莫宣学.2010.西藏措勤尼雄岩体的岩石成因及其对富Fe成矿作用的潜在意义.岩石学报,26(6):1793-1804
张志,唐菊兴,姚晓峰,宋俊龙,何林.2013.西藏尕尔穷-嘎拉勒铜金矿集区中侏罗世晚期岛弧闪长岩的厘定及其构造意义.矿物学报,33(S2):872-873
张招崇,董书云,黄河,马乐天,张东阳,张舒,薛春纪.2009.西南天山二叠纪中酸性侵入岩的地质学和地球化学:岩石成因和构造背景.地质通报,28(12):1827-1839
朱弟成,潘桂堂,莫宣学,王立全,廖忠礼,赵志丹,董国臣,周长勇.2006.冈底斯中北部晚侏罗世-早白垩世地球动力学环境:火山岩约束.岩石学报,22(3):534-546
朱弟成,莫宣学,赵志丹,许继峰,周长勇,孙晨光,王立全,陈海红,董国臣,周肃.2008.西藏冈底斯带措勤地区则弄群火山岩锆石U-Pb年代学格架及构造意义.岩石学报,24(3):401-412
(1)四川省地质调查院.2003.1/250000革吉县幅区域地质调查报告
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