西藏邦铺钼铜多金属矿床含矿斑岩的地球化学:对成岩源区与成矿机制的启示
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摘要
邦铺矿床是发育于冈底斯成矿带东段的大型斑岩型钼铜矿床。其含矿岩体的岩浆源区及成矿机制依然存在争议。本次研究从含矿岩体全岩主微量元素、锆石U-Pb定年、Hf-O同位素组成等方面做了进一步的探讨。含矿石英二长斑岩年龄为13.9±0.3Ma~14.0±0.2Ma,落在冈底斯带上的其他中新世斑岩型矿床含矿岩体成岩年龄范围内。含矿岩体锆石氧同位素组成比较均一,δ18O值为4.72‰~7.22‰(均值5.99‰);锆石εHf(t)值为-2.3~+5.6。锆石原位Hf-O同位素结果表明岩浆源区具有二端元混合的特点,且主要来自亏损地幔(如MORB)组分。与驱龙斑岩铜钼矿床相比,邦铺钼铜矿床Hf-O同位素更接近陆壳端元,表明在岩浆演化过程中遭受了更多富Mo的陆壳物质的混入,因此导致了驱龙是以铜为主要成矿元素的斑岩铜钼矿床,而邦铺矿床为具有更低Cu/Mo值的斑岩型钼铜矿床。
Bangpu porphyry Mo( Cu) deposit is a large Miocene Mo( Cu) deposit in Tibet. The petrogenesis of the ore-bearing Miocene intrusion and metallogenic mechanism has been debated. This study presents new results on whole rock major and trace elements,zircon U-Pb dating and Hf-O isotopic compositions of the Bangpu ore-bearing rocks. Magmatic zircons from these ore-bearing intrusions have U-Pb ages of 13. 9 ± 0. 3Ma ~ 14. 0 ± 0. 2Ma,which are within the range of other Miocene porphyry deposits in Gangdese belt. Zircons from the ore-bearing rocks have δ18O ranging from 4. 72‰ ~ 7. 22‰( average 5. 99‰) and εHf( t) from- 2. 3to + 5. 6. In situ zircon Hf-O isotopic measurements for the samples yield a binary mixing trend between mantle and continental crust,with depleted mantle-related( e. g. MORB) components as an important contributor. Compared to Qulong porphyry Cu( Mo) deposit,the zircon Hf-O isotopic measurements of Bangpu porphyry Mo( Cu) deposit plot closely to crustal end member,indicating that more continental crust melts enriched in Mo than that of Qulong deposit have been involved. These differences may be the main reason that Cu is the dominant exploitable metal( together with minor Mo) in Qulong,whereas Cu / Mo is lower than that of Qulong in Bangpu deposit.
Bangpu porphyry Mo( Cu) deposit is a large Miocene Mo( Cu) deposit in Tibet. The petrogenesis of the ore-bearing Miocene intrusion and metallogenic mechanism has been debated. This study presents new results on whole rock major and trace elements,zircon U-Pb dating and Hf-O isotopic compositions of the Bangpu ore-bearing rocks. Magmatic zircons from these ore-bearing intrusions have U-Pb ages of 13. 9 ± 0. 3Ma ~ 14. 0 ± 0. 2Ma,which are within the range of other Miocene porphyry deposits in Gangdese belt. Zircons from the ore-bearing rocks have δ18O ranging from 4. 72‰ ~ 7. 22‰( average 5. 99‰) and εHf( t) from- 2. 3to + 5. 6. In situ zircon Hf-O isotopic measurements for the samples yield a binary mixing trend between mantle and continental crust,with depleted mantle-related( e. g. MORB) components as an important contributor. Compared to Qulong porphyry Cu( Mo) deposit,the zircon Hf-O isotopic measurements of Bangpu porphyry Mo( Cu) deposit plot closely to crustal end member,indicating that more continental crust melts enriched in Mo than that of Qulong deposit have been involved. These differences may be the main reason that Cu is the dominant exploitable metal( together with minor Mo) in Qulong,whereas Cu / Mo is lower than that of Qulong in Bangpu deposit.
引文
Algeo TJ and Lyons TW.2006.Mo-total organic carbon covariation inmodern anoxic marine environments:Implications for analysis ofpaleoredox and paleohydrographic conditions.Paleoceanography,21(1):1-23
Ali JR and Aitchison JC.2008.Gondwana to Asia:Plate tectonics,paleogeography and the biological connectivity of the Indian subcontinent from the Middle Jurassic through latest Eocene(166~35Ma).Earth-Science Reviews,88(3-4):145-166
Black LP,Kamo SL,Allen CM,Aleinikoff JN,Davis DW,Korsch RJand Foudoulis C.2003.TEMORA 1:A new zircon standard forPhanerozoic U-Pb geochronology.Chemical Geology,200(1-2):155-170
Black LP,Kamo SL,Allen CM,Davis DW,Aleinikoff JN,Valley JW,Mundil R,Campbell IH,Korsch RJ,Williams IS and Foudoulis C.2004.Improved206Pb/238U microprobe geochronology by themonitoring of a trace-element-related matrix effect:SHRIMP,IDTIMS,ELA-ICP-MS and oxygen isotope documentation for a series ofzircon standards.Chemical Geology,205(1-2):115-140
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Ndisotopic composition of CHUR:Constraints from unequilibratedchondrites and implications for the bulk composition of terrestrialplanets.Earth and Planetary Science Letters,273(1-2):48-57
Chen SY,Yang JS,Li Y and Xu XZ.2009.Ultramafic blocks in Sumdoregion,Lhasa Block,eastern Tibet plateau:An ophiolite unit.Journal of Earth Science,20(2):332-347
Chen SY.2010.The development of Sumdo suture in the Lhasa Block,Tibet.Ph.D.Dissertation.Beijing:Chinese Academy of GeologicalScience,1-187(in Chinese)
Chen XC,Hu RZ,Bi XW,Zhong H,Lan JB,Zhao CH and Zhu JJ.2015.Petrogenesis of metaluminous A-type granitoids in theTengchong-Lianghe tin belt of southwestern China:Evidences fromzircon U-Pb ages and Hf-O isotopes,and whole-rock Sr-Nd isotopes.Lithos,212-215:93-110
Chu NC,Taylor RN,Chavagnac V,Nesbitt RW,Boella RM,Milton JA,German CR,Bayon G and Burton K.2002.Hf isotope ratio analysisusing multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections.Journal ofAnalytical Atomic Spectrometry,17(12):1567-1574
Chung SL,Liu DY,Ji JQ,Chu MF,Lee HY,Wen DJ,Lo CH,LeeTY,Qian Q and Zhang Q.2003.Adakites from continental collisionzones:Melting of thickened lower crust beneath southern Tibet.Geology,31(11):1021-1024
Chung SL,Chu MF,Ji J,O’Reilly SY,Pearson NJ,Liu D,Lee TY andLo CH.2009.The nature and timing of crustal thickening insouthern Tibet:Geochemical and zircon Hf isotopic constraints frompostcollisional adakites.Tectonophysics,477(1-2):36-48
Compston W,Williams IS,Kirschvink JL,Zichao Z and Guogan MA.1992.Zircon U-Pb ages for the Early Cambrian Time-Scale.Journalof the Geological Society,149(2):171-184
Feng Y,Wen ZH,Hou FH,Gao ZQ and Qi JH.2013.Tectonicevolution and paleocontinent reconstrucyion of Qinghai-Tibet Plateauand its adjacent since the Late Paleozoic.Marine Geology&Quaternary Geology,33(1):33-44(in Chinese with Englishabstract)
Gao YF,Hou ZQ and Wei RH.2003.Neogene porphyries fromGangdese:Petrological,geochemical characteristics and geodynamicsignificances.Acta Petrologica Sinica,19(3):418-428(inChinese with English abstract)
Gao YF,Hou ZQ,Kamber BS,Wei RH,Meng XJ and Zhao RS.2007.Adakite-like porphyries from the southern Tibetan continentalcollision zones:Evidence for slab melt metasomatism.Contributionsto Mineralogy and Petrology,153(1):105-120
Gao YF,Yang ZS,Santosh M,Hou ZQ,Wei RH and Tian SH.2010.Adakitic rocks from slab melt-modified mantle sources in thecontinental collision zone of southern Tibet.Lithos,119(3-4):651-663
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition ofcratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts inkimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin WL,Belousova EA,Shee SR,Pearson NJ and O’Reilly SY.2004.Archean crustal evolution in the northern Yilgarn Craton:UPb and Hf-isotope evidence from detrital zircons.PrecambrianResearch,131(3-4):231-282
Guo ZF,Wilson M and Liu JQ.2007.Post-collisional adakites in SouthTibet:Products of partial melting of subduction-modified lower crust.Lithos,96(1-2):205-224
Hou ZQ,Qu XM,Huang W and Gao YF.2001.Gangdise porphyrycopper metallogenic belt:The possible second“Yulong”copperbelt.Geology in China,28(10):27-29(in Chinese with Englishabstract)
Hou ZQ,Mo XX,Gao YF,Qu XM and Meng XJ.2003.Adakite,apossible host rock for porphyry copper deposits:Case studies ofporphyry copper belts in Tibetan Plateau and in Northern Chile.Mineral Deposits,22(1):1-12(in Chinese with Englishabstract)
Hou ZQ,Gao YF,Qu XM,Rui ZY and Mo XX.2004.Origin ofadakitic intrusives generated during Mid-Miocene east-west extensionin southern Tibet.Earth and Planetary Science Letters,220(1-2):139-155
Hou ZQ,Gao YF,Meng XJ,Qu XM and Huang W.2004.Genesis ofadakitic porphyry and tectonic controls on the Gangdese Mioceneporphyry copper belt in the Tibetan orogen.Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract)
Hou ZQ,Mo XX,Yang ZM,Wang AJ,Pan GT,Qu XM and Nie FJ.2006.Metallogeneses in the collisional orogen of the Qinghai-TibetPlateau:Tectonic setting,tempo-spatial distribution and ore deposittypes.Geology in China,33(2):340-351(in Chinese withEnglish abstract)
Hou ZQ,Yang ZM,Qu XM,Meng XJ,Li ZQ,Beaudoin G,Rui ZY,Gao YF and Zaw K.2009.The Miocene Gangdese porphyry copperbelt generated during post-collisional extension in the TibetanOrogen.Ore Geology Reviews,36(1-3):25-51
Hou ZQ,Zheng YC,Zeng LS,Gao LE,Huang KX,Li W,Li QY,FuQ,Liang W and Sun QZ.2012.Eocene-Oligocene granitoids insouthern Tibet:Constraints on crustal anatexis and tectonic evolutionof the Himalayan orogen.Earth and Planetary Science Letters,349-350:38-52
Hou ZQ,Zheng YC,Yang ZM,Rui ZY,Zhao ZD,Jiang SH,Qu XMand Sun QZ.2013.Contribution of mantle components withinjuvenile lower-crust to collisional zone porphyry Cu systems in Tibet.Mineralium Deposita,48(2):173-192
Hu YB,Liu JQ,Ling,MX,Ding W,Liu Y,Robert EZ,Ma XF,LiuDY,Zhang CC,Sun SJ,Zhang LP,Wu K and Sun WD.2015.The formation of Qulong adakites and their relationship with porphyrycopper deposit:Geochemical constraints.Lithos,220-223:60-80
Ickert RB,Hiess J,Williams IS,Holden P,Ireland TR,Lanc P,Schram N,Foster JJ and Clement SW.2008.Determining highprecision,in situ,oxygen isotope ratios with a SHRIMP II:Analysesof MPI-DING silicate-glass reference materials and zircon fromcontrasting granites.Chemical Geology,257(1-2):114-128
Kemp AI,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic andcrustal differentiation history of granitic rocks from Hf-O isotopes inzircon.Science,315(5814):980-983
Lee JKW,Williams IS and Ellis DJ.1997.Pb,U and Th diffusion innatural zircon.Nature,390(6656):159-162
Leng QF,Wang LQ,Ying LJ,Zheng WB,Luo MC,Chen W,Lin B andWang YY.2012.LA-ICP-MS Zircon U-Pb dating of allgovite in theBangpu molybdenum(copper)deposit in Tibet and its geologicalsignificance.Acta Geoscientia Sinica,33(4):559-568(inChinese with English abstract)
Li CY,Wang FY,Hao XL,Ding X,Zhang H,Ling MX,Zhou JB,LiYL,Fan WM and Sun WD.2012a.Formation of the world’s largestmolybdenum metallogenic belt:A plate-tectonic perspective on theQinling molybdenum deposits.International Geology Review,56(9):1093-1112
Li FQ,Liu W,Wang BD and Zhang SZ.2012.The continuation of thesubduction of Paleo-Tethys Ocean within Lhasa block in EarlyMiddle Triassic:Evidence from volcanic rocks and HP metamorphicrocks.Acta Petrologica et Mineralogica,31(2):119-132(inChinese with English abstract)
Li H,Ling MX,Li CY,Zhang H,Ding X,Yang XY,Fan WM,Li YLand Sun WD.2012b.A-type granite belts of two chemical subgroupsin central eastern China:Indication of ridge subduction.Lithos,150:26-36
Li XH,Li WX,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role ofmantle-derived magma in genesis of Early Yanshanian granites in theNanling Range,South China:In situ zircon Hf-O isotopicconstraints.Science in China(Series D),52(9):1262-1278
Li XH,Li WX,Li QL,Wang XC,Liu Y and Yang YH.2010.Petrogenesis and tectonic significance of the~850Ma Gangbianalkaline complex in South China:Evidence from in situ zircon U-Pbdating,Hf-O isotopes and whole-rock geochemistry.Lithos,114(1-2):1-15
Li JX,Qin KZ,Li GM and Yang LK.2007.K-Ar and40Ar/39Ar agedating of Nimu porphyry copper orefield in Central Gangdese:Constrains on magmatic-hydrothermal evolution and metallogenetictectonic setting.Acta Petrologica Sinica,23(5):953-966(inChinese with English abstract)
Li JX,Qin KZ,Li GM,Xiao B,Chen L and Zhao JX.2011.Postcollisional ore-bearing adakitic porphyries from Gangdese porphyrycopper belt,southern Tibet:Melting of thickened juvenile arc lowercrust.Lithos,126(3-4):265-277
Li TD.2002.New progress in the geoscience study of the Qinghai-Tibetplateau.Geological Bulletin of China,21(7):370-376(inChinese with English abstract)
Lin W,Liang HY,Zhang YQ and Xie YW.2004.Petrochemistry andSHRIMP U-Pb zircon age of the Chongjiang ore-bearing porphyry inthe Gangdese porphyry copper belt.Geochimica,33(6):585-592(in Chinese with English abstract)
Liu Y,Liu HC and Li XH.1996.Simultaneous and precisedetermination of 40 trace elements in rock samples using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract)
Liu YJ,Cao LM,Li ZL,Wang HN,Chu TQ and Zhang JR.1984.Element Geochemistry.Beijing:Science Press,1-548(inChinese)
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010a.Continental and oceanic crust recycling-induced melt-peridotiteinteractions in the Trans-North China Orogen:U-Pb dating,Hfisotopes and trace elements in zircons from mantle xenoliths.Journalof Petrology,51(1-2):537-571
Liu YS,Hu ZC,Zong KQ,Gao CG,Gao S,Xu JA and Chen HH.2010b.Reappraisement and refinement of zircon U-Pb isotope andtrace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546
Ludwig KR.2000.User’s manual for isoplot 3.00:A geochronologicaltoolkit for Microsoft excel.Berkeley Geochronology CenterSpecial Publication
Luo MC,Wang LQ,Leng QF and Chen W.2011.Zircon Hf isotope andCe4+/Ce3+ratio of the monzogranite porphyry and biotite monzoniticgranite in Bangpu Mo(Cu)deposit,Tibet.Mineral Deposits,30(2):266-278(in Chinese with English abstract)
Luo MC,Mao JW,Wang LW,Leng QF and Chen W.2012.Fluidinclusion evidence for magmatic-hydrothermal evolution in theBangpu porphyry molybdenum-copper deposit,Tibet.ActaGeoscientia Sinica,33(4):471-484(in Chinese with Englishabstract)
Mcdonough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
McM anus J,Berelson WM,Severmann S,Poulson RL,Hammond DE,Klinkhammer GP and Holm C.2006.Molybdenum and uraniumgeochemistry in continental margin sediments:Paleoproxy potential.Geochimica et Cosmochimica Acta,70(18):4643-4662
Meng XJ,Hou ZQ,Gao YF,Huang W,Qu XM and Qu WJ.2003.Development of porphyry copper-molybdenum-lead-zinc ore formingsystem in East Gangdese belt,Tibet:Evidence from Re-Os age ofmolybdenite in Bangpu copper polymetallic deposit.MineralDeposits,22(3):246-252(in Chinese with English abstract)
Mustard R,Ulrich T,Kamenetsky VS and Mernagh T.2006.Gold andmetal enrichment in natural granitic melts during fractionalcrystallization.Geology,34(2):85-88
Pan GT,Mo XX,Hou ZQ,Zhu DC,Wang LQ,Li GM,Zhao ZD,GengQR and Liao ZL.2006.Spatial-temporal framework of the GangdeseOrogenic Belt and its evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract)
Qu XM,Hou ZQ and Huang W.2001.Is Gangdese porphyry copper beltthe second“Yulong”copper belt?Mineral Deposits,20(4):355-366(in Chinese with English abstract)
Qu XM,Hou ZQ and Li YG.2004.Melt components derived from asubducted slab in late orogenic ore-bearing porphyries in theGangdese copper belt,southern Tibetan Plateau.Lithos,74(3-4):131-148
Qu XM,Hou ZQ,Guo LJ and Xu WY.2004.Source compositions andcrustal contaminations of adakitic ore-bearing porphyries in theGangdese copper belt:Nd,Sr,Pb and O isotope constraints.ActaGeologica Sinica,78(6):813-821(in Chinese with Englishabstract)
Rimmer SM.2004.Geochemical paleoredox indicators in DevonianMississippian black shales,central Appalachian basin(USA).Chemical Geology,206(3-4):373-391
Robb L.2005.Introduction to Ore-forming Processes.Oxford,UK:Blackwell Publication,1-373
Rudnick RL and Gao S.2003.Composition of the continental crust.In:Heinrich DH and Turekian KKE(eds.).Treatise on Geochemistry.Oxford:Elsevier-Pergamon,1-64
Rui ZY,Hou ZQ,Qu XM,Zhang LS,Wang LS and Liu YL.2003.Metallogenetic epoch of Gangdese porphyry copper belt and uplift ofQinghai-Tibet Plateau.Mineral Deposits,22(3):217-225(inChinese with English abstract)
Scott C,Lyons TW,Bekker A,Shen Y,Poulton SW,Chu X and AnbarAD.2008.Tracing the stepwise oxygenation of the Proterozoicocean.Nature,452(7186):456-459
Sun SS and McD onough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in OceanicBasins.Geological Society,London,Special Publications,42(1):313-345
Sun WD,Arculus RJ,Bennett VC,Eggins SM and Binns RA.2003a.Evidence for rhenium enrichment in the mantle wedge fromsubmarine arc-like volcanic glasses(Papua New Guinea).Geology,31(10):845-848
Sun WD,Bennett VC,Eggins SM,Arculus RJ and Perfit MR.2003b.Rhenium systematics in submarine MORB and back-arc basinglasses:Laser ablation ICP-MS results.Chemical Geology,196(1-4):259-281
Sun WD,Arculus RJ,Kamenetsky VS and Binns RA.2004a.Release ofgold-bearing fluids in convergent margin magmas prompted bymagnetite crystallization.Nature,431(7011):975-978
Sun WD,Bennett VC and Kamenetsky VS.2004b.The mechanism of Reenrichment in arc magmas:Evidence from Lau Basin basaltic glassesand primitive melt inclusions.Earth and Planetary Science Letters,222(1):101-114
Sun WD,Liang HY,Ling MX,Zhan MZ,Ding X,Zhang H,Yang XY,Li YL,Ireland TR,Wei QR and Fan WM.2013.The link betweenreduced porphyry copper deposits and oxidized magmas.Geochimicaet Cosmochimica Acta,103:263-275
Sun ZM,Jiang W,Pei JL and Li HB.2008.New Early Cretaceouspaleomagnetic data from volcanic of the eastern Lhasa Block and itstectonic implications.Acta Petrologica Sinica,24(7):1621-1626(in Chinese with English abstract)
Sun ZM,Jiang W,Li HB,Pei JL and Zhu ZM.2010.Newpaleomagnetic results of Paleocene volcanic rocks from the Lhasablock:Tectonic implications for the collision of India and Asia.Tectonophysics,490(3-4):257-266
Tang JX,Dor J,Liu HF,Lang XH,Zhang JS,Zheng WB and Ying LJ.2012.Minerogenetic series of ore deposits in the east part of theGangdise metallogenic belt.Acta Geoscientia Sinica,33(4):393-410(in Chinese with English abstract)
Tang XD,Huang BC,Yang LK,Yi ZY,Qiao QQ and Chen LW.2013.Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanicrocks in the middle Lhasa terrane,China and tectonic implications.Chinese Journal of Geophysics,56(1):136-149(in Chinese withEnglish abstract)
Tu XL,Zhang H,Deng WF,Ling MX,Liang HY,Liu Y and Sun WD.2011.Application of RESOlution in-situ laser ablation ICP-MS intrace element analyses.Geochimica,40(1):83-98(in Chinesewith English abstract)
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zirconmegacrysts from kimberlite:Oxygen isotope variability among mantlemelts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Valley JW,Lackey JS,Cavosie AJ,Clechenko CC,Spicuzza MJ,BaseiMAS,Bindeman IN,Ferreira VP,Sial AN,King EM,Peck WH,Sinha AK and Wei CS.2005.4.4 billion years of crustalmaturation:Oxygen isotope ratios of magmatic zircon.Contributionsto Mineralogy and Petrology,150(6):561-580
Wang LL,Mo XX,Li B,Dong GC and Zhao ZD.2006.Geochronologyand geochemistry of the ore-bearing porphyry in Qulong Cu(Mo)oredeposit,Tibet.Acta Petrologica Sinica,22(4):1001-1008(inChinese with English abstract)
Wang LQ,Tang JX,Chen YC,Luo MC,Leng QF,Chen W and WangH.2011.LA-ICP-MS zircon U-Pb dating of ore-bearingmonzogranite porphyry in Bangpu molybdenum(copper)deposit,Tibet and its significance.Mineral Deposits,30(2):349-360(inChinese with English abstract)
Wang LQ,Luo MC,Yuan ZJ,Chen W,Leng QF and Zhang XQ.2012.Sulfur,Lead,Carbon and Oxygen isotope composition and source ofore-forming materials of the Bangpu Pb-Zn ore deposit in Tibet.ActaGeoscientia Sinica,33(4):435-443(in Chinese with Englishabstract)
Wang LQ,Tang JX,Cheng WB,Chen W,Zhang Z,Lin X,Luo MCand Yang C.2014.Origin of the ore-forming fluids and metals of theBangpu porphyry Mo-Cu deposit of Tibet,China:Constraints fromHe-Ar,H-O,S and Pb isotopes.Journal of Asian Earth Sciences,103:276-287
Wang LQ,Tang JX,Chen W,Luo MC,Kang HR and Leng QF.2014.Mineralogical characteristics of skarn in the Bangpu Mo polymetallicdeposit,Tibet,and their geological significance.Geology in China,41(2):562-576(in Chinese with English abstract)
Wang QH,Wang BS,Li JG,Yao P,Li Z,Zhou ZY,Cheng LJ and LiuHF.2002.Basic features and ore prospect evaluation of theGangdise island arc,Tibet and its copper polymetallic ore belt.Geological Bulletin of China,21(1):35-40(in Chinese withEnglish abstract)
Wang ZH,Liu YL,Liu HF,Guo LS,Zhang JS and Xu KF.2012.Geochronology and geochemistry of the Bangpu Mo-Cu porphyry oredeposit,Tibet.Ore Geology Reviews,46:95-105
Wen Q,Duo J,Wen CQ,Zhang XQ,Zhou X,Hou Y and Fei CG.2011.Dating of monzonitic granite porphyry in the Bangpu Mo-Cudeposit,Tibet.Journal of Mineralogy and Petrology,31(2):48-53(in Chinese with English abstract)
Wu FY and Yang JH.2006.Zircon U-Pb and Hf isotopic constraints onthe multiple components in granites.Geochimica et CosmochimicaActa,70(18):A709
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints oninterpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xu WC,Zhang HF,Guo L and Yuan HL.2010.Miocene high Sr/Ymagmatism,south Tibet:Product of partial melting of subductedIndian continental crust and its tectonic implication.Lithos,114(3-4):293-306
Xu XZ,Yang JS,Li TF,Chen SY,Ren YF,Li ZL and Shi YR.2007.SHRIMP U-Pb ages and inclusions of zircons from the Sumdo eclogitein the Lhasa block,Tibet,China.Geological Bulletin of China,26(10):1340-1355(in Chinese with English abstract)
Xu ZQ,Yang JS,Li WC,Li HQ,Cai ZH,Yan Z and Ma CQ.2013.Paleo-Tethys system and accretionary orogen in the Tibet Plateau.Acta Petrologica Sinica,29(6):1847-1860(in Chinese withEnglish abstract)
Yang JS,Xu ZQ,Geng QR,Li ZL,Xu XZ,Li TF,Ren YF,Li HQ,Cai ZH,Liang FH and Chen SY.2006.A possible new HP/UHP(?)metamorphic belt in China:Discovery of eclogite in the LahsaTerrane,Tibet.Acta Geologica Sinica,80(12):1787-1792(inChinese with English abstract)
Yang JS,Xu ZQ,Li TF,Li HQ,Li ZL,Ren YF,Xu XZ and Chen SY.2007.Oceanic subduction-type eclogite in the Lhasa block,Tibet,China:Remains of the Paleo-Tethys ocean basin?Geological Bulletinof China,26(10):1277-1287(in Chinese with English abstract)
Yang JS,Xu ZQ,Li ZL,Xua XZ,Li TF,Ren YF,Li HQ,Chen SYand Robinson PT.2009.Discovery of an eclogite belt in the Lhasablock,Tibet:A new border for Paleo-Tethys?Journal of Asian EarthSciences,34(1):76-89
Yi ZY,Huang BC,Chen JS,Chen LW and Wang HL.2011.Paleomagnetism of Early Paleogene marine sediments in southernTibet,China:Implications to onset of the India-Asia collision andsize of Greater India.Earth and Planetary Science Letters,309(1-2):153-165
Zhang H,Sun WD,Yang XY,Liang HY,Wang BH,Wang RL andWang YX.2011.Geochronology and metallogenesis of theShapinggou giant porphyry molybdenum deposit in the Dabie orogenicbelt.Acta Geologica Sinica,85(12):2039-2059(in Chinese withEnglish abstract)
Zhang H,Li CY,Yang XY,Sun YL,Deng JH,Liang HY,Wang RL,Wang BH,Wang YX and Sun WD.2014.Shapinggou:The largestClimax-type porphyry Mo deposit in China.International GeologyReview,56(3):313-331
Zhang QL,Qu XM,Xu WY,Hou ZQ and Chen WS.2003.Study of thefluid inclusions from Nanmu porphyry Cu-Mo deposit in Tibet.ActaPetrologica Sinica,19(2):251-259(in Chinese with Englishabstract)
Zhao XY,Yang ZS,Hou ZQ,Zheng YC,Liu YC,Tian SH,Fu Q andFei F.2013.Petrogenesis of diabase porphyrite in Bangpu deposit ofTibet and its instructions to the regional tectonic and magmaticevolution.Acta Petrologica Sinica,29(11):3767-3778(inChinese with English abstract)
Zheng YC,Hou ZQ,Li QY,Sun QZ,Liang W,Fu Q,Li W and HuangKX.2012.Origin of Late Oligocene adakitic intrusives in thesoutheastern Lhasa terrane:Evidence from in situ zircon U-Pbdating,Hf-O isotopes,and whole-rock geochemistry.Lithos,148:296-311
Zheng YY,Xue YX,Cheng LJ,Fan ZH and Gao SB.2004.Finding,characteristics and significances of Qulong superlarge porphyrycopper(molybdenum)deposit,Tibet.Earth Science,29(1):103-108(in Chinese with English abstract)
Zhou X,Wen CQ,Fei CG,Cao SY,Wu PY and Huo Y.2010a.Geochemical characteristics of monzonite granite porphyry in Bangpuporphyry Mo deposit,Tibet,and its tectonic significance.Journal ofMineralogy and Petrology,30(4):48-54(in Chinese with Englishabstract)
Zhou X,Wen CQ,Huo Y,Fei GC and Wu PY.2010b.Characteristicsof ore-forming fluid of Bangpu molybdenum-copper polymetallicdeposit,Maizhokunggar area,Tibet,China.Geological Bulletin ofChina,29(7):1039-1048(in Chinese with English abstract)
Zhou X,Wen CQ,Wen Q,Wu PY,Cao SY,Fei CG,Huo Y and ZhouY.2010c.Zircon U-Pb SHRIMP dating of the monzonite graniteporphyry from the Bangpu large porphyry molybdenum-copperdeposits,Tibet,and its geological significance.Bulletin ofMineralogy,Petrology and Geochemistry,29(4):373-379(inChinese with English abstract)
Zhou X,Wen CQ,Zhang XQ,Cao SY,Wu PY,Zhou Y and Fei GC.2010d.Rb-Sr isochron age dating of the Bangpu large-scale Mo-Cupolymetallic deposit,Tibet and its geological significance.GeologicalJournal of China Universities,16(4):448-456(in Chinese withEnglish abstract)
Zhou X.2012.Genisis study of Mo-Cu polymetallic deposit from theBangpu,Tibet.Ph.D.Dissertation.Chengdu:Chengdu Universityof Technology(in Chinese with English summary)
Zhu DC,Pan GT,Mo XX,Wang LQ,Liao ZL,Zhao ZD,Dong GC andZhou CY.2006.Late Jurassic-Early Cretaceous geodynamic settingin middle-northern Gangdese;New insights from volcanic rocks.Acta Petrologica Sinica,22(3):534-546(in Chinese withEnglish abstract)
Zhu DC,Zhao ZD,Niu YL,Wang Q,Dilek Y,Dong GC and Mo XX.2012.Origin and Paleozoic tectonic evolution of the Lhasa Terrane.Geological Journal of China Universities,18(1):1-15(in Chinesewith English abstract)
Zhu DC,Zhao ZD,Niu YL,Dilek Y,Hou ZQ and Mo XX.2013.Theorigin and pre-Cenozoic evolution of the Tibetan Plateau.GondwanaResearch,23(4):1429-1454
陈松永.2010.西藏拉萨地块中古特提斯缝合带的厘定.博士学位论文.北京:中国地质科学院,1-187
冯岩,温珍河,侯方辉,高志清,祁江豪.2013.青藏高原及其邻区晚古生代以来构造演化与古大陆再造.海洋地质与第四纪地质,33(1):33-44
高永丰,侯增谦,魏瑞华.2003.冈底斯晚第三纪斑岩的岩石学、地球化学及其地球动力学意义.岩石学报,19(3):418-428
侯增谦,曲晓明,黄卫,高永丰.2001.冈底斯斑岩铜矿成矿带有望成为西藏第二条“玉龙”铜矿带.中国地质,28(10):27-29
侯增谦,莫宣学,高永丰,曲晓明,孟祥金.2003.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩(以西藏和智利斑岩铜矿为例).矿床地质,22(1):1-12
侯增谦,高永丰,孟祥金,曲晓明,黄卫.2004.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制.岩石学报,20(2):239-248
侯增谦,莫宣学,杨志明,王安建,潘桂棠,曲晓明,聂凤军.2006.青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型.中国地质,33(2):340-351
冷秋锋,王立强,应立娟,郑文宝,罗茂澄,陈伟,林彬,王艺云.2012.西藏邦铺钼(铜)矿床辉绿玢岩脉体LA-ICP-MS锆石UPb定年及其地质意义.地球学报,33(4):559-568
李奋其,刘伟,王保弟,张士贞.2012.拉萨地块内部古特提斯洋早中三叠世仍在俯冲———来自火山岩和高压变质岩的证据.岩石矿物学杂志,31(2):119-132
李金祥,秦克章,李光明,杨列坤.2007.冈底斯中段尼木斑岩铜矿田的K-Ar、40Ar/39Ar年龄:对岩浆-热液系统演化和成矿构造背景的制约.岩石学报,23(5):953-966
李廷栋.2002.青藏高原地质科学研究的新进展.地质通报,21(7):370-376
林武,梁华英,张玉泉,谢玉玲.2004.冈底斯铜矿带冲江含矿斑岩的岩石化学及锆石SHRIMP年龄特征.地球化学,33(6):585-592
刘颖,刘海臣,李献华.1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558
刘英俊,曹励明,李兆麟,王鹤年,储同庆,张景荣.1984.元素地球化学.北京:科学出版社,1-548
罗茂澄,王立强,冷秋锋,陈伟.2011.邦铺钼(铜)矿床二长花岗斑岩、黑云二长花岗岩锆石Hf同位素和Ce4+/Ce3+比值.矿床地质,30(2):266-278
罗茂澄,毛景文,王立强,冷秋锋,陈伟.2012.西藏邦铺斑岩钼铜矿床岩浆-热液流体演化:流体包裹体研究.地球学报,33(4):471-484
孟祥金,侯增谦,高永丰,黄卫,曲晓明,屈文俊.2003.西藏冈底斯带东段斑岩铜钼铅锌成矿系统的发育时限:帮浦铜多金属矿床辉钼矿Re-Os年龄证据.矿床地质,22(3):246-252
潘桂棠,莫宣学,侯增谦,朱弟成,王立全,李光明,赵志丹,耿全如,廖忠礼.2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533
曲晓明,侯增谦,黄卫.2001.冈底斯斑岩铜矿成矿带:西藏第二条玉龙铜矿带?矿床地质,20(4):355-366
曲晓明,侯增谦,国连杰,徐文艺.2004.冈底斯铜矿带埃达克质含矿斑岩的源区组成与地壳混染:Nd、Sr、Pb、O同位素约束.地质学报,78(6):813-821
芮宗瑶,侯增谦,曲晓明,张立生,王龙生,刘玉琳.2003.冈底斯斑岩铜矿成矿时代及青藏高原隆升.矿床地质,22(3):217-225
孙知明,江万,裴军令,李海兵.2008.青藏高原拉萨地块早白垩纪火山岩古地磁结果及其构造意义.岩石学报,24(7):1621-1626
唐菊兴,多吉,刘鸿飞,郎兴海,张金树,郑文宝,应立娟.2012.冈底斯成矿带东段矿床成矿系列及找矿突破的关键问题研究.地球学报,33(4):393-410
唐祥德,黄宝春,杨列坤,易治宇,乔庆庆,陈力为.2013.拉萨地块中部晚白垩世火山岩Ar-Ar年代学和古地磁研究结果及其构造意义.地球物理学报,56(1):136-149
涂湘林,张红,邓文峰,凌明星,梁华英,刘颖,孙卫东.2011.RESOlution激光剥蚀系统在微量元素原位微区分析中的应用.地球化学,40(1):83-98
王亮亮,莫宣学,李冰,董国臣,赵志丹.2006.西藏驱龙斑岩铜矿含矿斑岩的年代学与地球化学.岩石学报,22(4):1001-1008
王立强,唐菊兴,陈毓川,罗茂澄,冷秋锋,陈伟,王焕.2011.西藏邦铺钼(铜)矿床含矿二长花岗斑岩LA-ICP-MS锆石U-Pb定年及地质意义.矿床地质,30(2):349-360
王立强,罗茂澄,袁志洁,陈伟,冷秋锋,张学全.2012.西藏邦铺铅锌矿床S、Pb、C、O同位素组成及成矿物质来源研究.地球学报,33(4):435-443
王立强,唐菊兴,陈伟,罗茂澄,康浩然,冷秋锋.2014.西藏邦铺钼多金属矿床矽卡岩矿物学特征及其地质意义.中国地质,41(2):562-576
王全海,王保生,李金高,姚鹏,李志,周祖翼,程力军,刘鸿飞.2002.西藏冈底斯岛弧及其铜多金属矿带的基本特征与远景评估.地质通报,21(1):35-40
温泉,多吉,温春齐,张学全,周雄,霍艳,费光春.2011.西藏邦铺钼铜矿区花岗斑岩成岩年龄研究.矿物岩石,31(2):48-53
徐向珍,杨经绥,李天福,陈松永,任玉峰,李兆丽,石玉若.2007.青藏高原拉萨地块松多榴辉岩的锆石SHRIMP U-Pb年龄及锆石中的包裹体.地质通报,26(10):1340-1355
许志琴,杨经绥,李文昌,李化启,蔡志慧,闫臻,马昌前.2013.青藏高原中的古特提斯体制与增生造山作用.岩石学报,29(6):1847-1860
杨经绥,许志琴,耿全如,李兆丽,徐向珍,李天福,任玉峰,李化启,蔡志慧,梁凤华,陈松永.2006.中国境内可能存在一条新的高压/超高压(?)变质带———青藏高原拉萨地体中发现榴辉岩带.地质学报,80(12):1787-1792
杨经绥,许志琴,李天福,李化启,李兆丽,任玉峰,徐向珍,陈松永.2007.青藏高原拉萨地块中的大洋俯冲型榴辉岩:古特提斯洋盆的残留?地质通报,26(10):1277-1287
张红,孙卫东,杨晓勇,梁华英,王波华,王瑞龙,王玉贤.2011.大别造山带沙坪沟特大型斑岩钼矿床年代学及成矿机理研究.地质学报,85(12):2039-2059
张绮玲,曲晓明,徐文艺,侯增谦,陈伟十.2003.西藏南木斑岩铜钼矿床的流体包裹体研究.岩石学报,19(2):251-259
赵晓燕,杨竹森,侯增谦,郑远川,刘英超,田世洪,付强,费凡.2013.西藏邦铺矿区辉绿玢岩成因及对区域构造岩浆演化的指示.岩石学报,29(11):3767-3778
郑有业,薛迎喜,程力军,樊子珲,高顺宝.2004.西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义.地球科学,29(1):103-108
周雄,温春齐,费光春,曹盛远,吴鹏宇,霍艳.2010a.西藏邦铺斑岩型钼矿床二长花岗斑岩地球化学特征及构造意义.矿物岩石,30(4):48-54
周雄,温春齐,霍艳,费光春,吴鹏宇.2010b.西藏墨竹工卡地区邦铺钼铜多金属矿床成矿流体的特征.地质通报,29(7):1039-1048
周雄,温春齐,温泉,吴鹏宇,曹盛远,费光春,霍艳,周玉.2010c.西藏邦铺大型斑岩钼-铜矿床二长花岗斑岩锆石SHRIMP定年及其地质意义.矿物岩石地球化学通报,29(4):373-379
周雄,温春齐,张学全,曹盛远,吴鹏宇,周玉,费光春.2010d.西藏邦铺大型钼铜多金属矿床Rb-Sr等时线年龄及地质意义.高校地质学报,16(4):448-456
周雄.2012.西藏邦铺钼铜多金属矿床成因研究.博士学位论文.成都:成都理工大学
朱弟成,潘桂棠,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,赵志丹,牛耀龄,王青,Yildirim D,董国臣,莫宣学.2012.拉萨地体的起源和古生代构造演化.高校地质学报,18(1):1-15
①西藏自治区地勘局地热地质大队.2009.西藏自治区墨竹工卡县邦铺矿区钼(铜)多金属矿详查报告
Ali JR and Aitchison JC.2008.Gondwana to Asia:Plate tectonics,paleogeography and the biological connectivity of the Indian subcontinent from the Middle Jurassic through latest Eocene(166~35Ma).Earth-Science Reviews,88(3-4):145-166
Black LP,Kamo SL,Allen CM,Aleinikoff JN,Davis DW,Korsch RJand Foudoulis C.2003.TEMORA 1:A new zircon standard forPhanerozoic U-Pb geochronology.Chemical Geology,200(1-2):155-170
Black LP,Kamo SL,Allen CM,Davis DW,Aleinikoff JN,Valley JW,Mundil R,Campbell IH,Korsch RJ,Williams IS and Foudoulis C.2004.Improved206Pb/238U microprobe geochronology by themonitoring of a trace-element-related matrix effect:SHRIMP,IDTIMS,ELA-ICP-MS and oxygen isotope documentation for a series ofzircon standards.Chemical Geology,205(1-2):115-140
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Ndisotopic composition of CHUR:Constraints from unequilibratedchondrites and implications for the bulk composition of terrestrialplanets.Earth and Planetary Science Letters,273(1-2):48-57
Chen SY,Yang JS,Li Y and Xu XZ.2009.Ultramafic blocks in Sumdoregion,Lhasa Block,eastern Tibet plateau:An ophiolite unit.Journal of Earth Science,20(2):332-347
Chen SY.2010.The development of Sumdo suture in the Lhasa Block,Tibet.Ph.D.Dissertation.Beijing:Chinese Academy of GeologicalScience,1-187(in Chinese)
Chen XC,Hu RZ,Bi XW,Zhong H,Lan JB,Zhao CH and Zhu JJ.2015.Petrogenesis of metaluminous A-type granitoids in theTengchong-Lianghe tin belt of southwestern China:Evidences fromzircon U-Pb ages and Hf-O isotopes,and whole-rock Sr-Nd isotopes.Lithos,212-215:93-110
Chu NC,Taylor RN,Chavagnac V,Nesbitt RW,Boella RM,Milton JA,German CR,Bayon G and Burton K.2002.Hf isotope ratio analysisusing multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections.Journal ofAnalytical Atomic Spectrometry,17(12):1567-1574
Chung SL,Liu DY,Ji JQ,Chu MF,Lee HY,Wen DJ,Lo CH,LeeTY,Qian Q and Zhang Q.2003.Adakites from continental collisionzones:Melting of thickened lower crust beneath southern Tibet.Geology,31(11):1021-1024
Chung SL,Chu MF,Ji J,O’Reilly SY,Pearson NJ,Liu D,Lee TY andLo CH.2009.The nature and timing of crustal thickening insouthern Tibet:Geochemical and zircon Hf isotopic constraints frompostcollisional adakites.Tectonophysics,477(1-2):36-48
Compston W,Williams IS,Kirschvink JL,Zichao Z and Guogan MA.1992.Zircon U-Pb ages for the Early Cambrian Time-Scale.Journalof the Geological Society,149(2):171-184
Feng Y,Wen ZH,Hou FH,Gao ZQ and Qi JH.2013.Tectonicevolution and paleocontinent reconstrucyion of Qinghai-Tibet Plateauand its adjacent since the Late Paleozoic.Marine Geology&Quaternary Geology,33(1):33-44(in Chinese with Englishabstract)
Gao YF,Hou ZQ and Wei RH.2003.Neogene porphyries fromGangdese:Petrological,geochemical characteristics and geodynamicsignificances.Acta Petrologica Sinica,19(3):418-428(inChinese with English abstract)
Gao YF,Hou ZQ,Kamber BS,Wei RH,Meng XJ and Zhao RS.2007.Adakite-like porphyries from the southern Tibetan continentalcollision zones:Evidence for slab melt metasomatism.Contributionsto Mineralogy and Petrology,153(1):105-120
Gao YF,Yang ZS,Santosh M,Hou ZQ,Wei RH and Tian SH.2010.Adakitic rocks from slab melt-modified mantle sources in thecontinental collision zone of southern Tibet.Lithos,119(3-4):651-663
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition ofcratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts inkimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin WL,Belousova EA,Shee SR,Pearson NJ and O’Reilly SY.2004.Archean crustal evolution in the northern Yilgarn Craton:UPb and Hf-isotope evidence from detrital zircons.PrecambrianResearch,131(3-4):231-282
Guo ZF,Wilson M and Liu JQ.2007.Post-collisional adakites in SouthTibet:Products of partial melting of subduction-modified lower crust.Lithos,96(1-2):205-224
Hou ZQ,Qu XM,Huang W and Gao YF.2001.Gangdise porphyrycopper metallogenic belt:The possible second“Yulong”copperbelt.Geology in China,28(10):27-29(in Chinese with Englishabstract)
Hou ZQ,Mo XX,Gao YF,Qu XM and Meng XJ.2003.Adakite,apossible host rock for porphyry copper deposits:Case studies ofporphyry copper belts in Tibetan Plateau and in Northern Chile.Mineral Deposits,22(1):1-12(in Chinese with Englishabstract)
Hou ZQ,Gao YF,Qu XM,Rui ZY and Mo XX.2004.Origin ofadakitic intrusives generated during Mid-Miocene east-west extensionin southern Tibet.Earth and Planetary Science Letters,220(1-2):139-155
Hou ZQ,Gao YF,Meng XJ,Qu XM and Huang W.2004.Genesis ofadakitic porphyry and tectonic controls on the Gangdese Mioceneporphyry copper belt in the Tibetan orogen.Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract)
Hou ZQ,Mo XX,Yang ZM,Wang AJ,Pan GT,Qu XM and Nie FJ.2006.Metallogeneses in the collisional orogen of the Qinghai-TibetPlateau:Tectonic setting,tempo-spatial distribution and ore deposittypes.Geology in China,33(2):340-351(in Chinese withEnglish abstract)
Hou ZQ,Yang ZM,Qu XM,Meng XJ,Li ZQ,Beaudoin G,Rui ZY,Gao YF and Zaw K.2009.The Miocene Gangdese porphyry copperbelt generated during post-collisional extension in the TibetanOrogen.Ore Geology Reviews,36(1-3):25-51
Hou ZQ,Zheng YC,Zeng LS,Gao LE,Huang KX,Li W,Li QY,FuQ,Liang W and Sun QZ.2012.Eocene-Oligocene granitoids insouthern Tibet:Constraints on crustal anatexis and tectonic evolutionof the Himalayan orogen.Earth and Planetary Science Letters,349-350:38-52
Hou ZQ,Zheng YC,Yang ZM,Rui ZY,Zhao ZD,Jiang SH,Qu XMand Sun QZ.2013.Contribution of mantle components withinjuvenile lower-crust to collisional zone porphyry Cu systems in Tibet.Mineralium Deposita,48(2):173-192
Hu YB,Liu JQ,Ling,MX,Ding W,Liu Y,Robert EZ,Ma XF,LiuDY,Zhang CC,Sun SJ,Zhang LP,Wu K and Sun WD.2015.The formation of Qulong adakites and their relationship with porphyrycopper deposit:Geochemical constraints.Lithos,220-223:60-80
Ickert RB,Hiess J,Williams IS,Holden P,Ireland TR,Lanc P,Schram N,Foster JJ and Clement SW.2008.Determining highprecision,in situ,oxygen isotope ratios with a SHRIMP II:Analysesof MPI-DING silicate-glass reference materials and zircon fromcontrasting granites.Chemical Geology,257(1-2):114-128
Kemp AI,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic andcrustal differentiation history of granitic rocks from Hf-O isotopes inzircon.Science,315(5814):980-983
Lee JKW,Williams IS and Ellis DJ.1997.Pb,U and Th diffusion innatural zircon.Nature,390(6656):159-162
Leng QF,Wang LQ,Ying LJ,Zheng WB,Luo MC,Chen W,Lin B andWang YY.2012.LA-ICP-MS Zircon U-Pb dating of allgovite in theBangpu molybdenum(copper)deposit in Tibet and its geologicalsignificance.Acta Geoscientia Sinica,33(4):559-568(inChinese with English abstract)
Li CY,Wang FY,Hao XL,Ding X,Zhang H,Ling MX,Zhou JB,LiYL,Fan WM and Sun WD.2012a.Formation of the world’s largestmolybdenum metallogenic belt:A plate-tectonic perspective on theQinling molybdenum deposits.International Geology Review,56(9):1093-1112
Li FQ,Liu W,Wang BD and Zhang SZ.2012.The continuation of thesubduction of Paleo-Tethys Ocean within Lhasa block in EarlyMiddle Triassic:Evidence from volcanic rocks and HP metamorphicrocks.Acta Petrologica et Mineralogica,31(2):119-132(inChinese with English abstract)
Li H,Ling MX,Li CY,Zhang H,Ding X,Yang XY,Fan WM,Li YLand Sun WD.2012b.A-type granite belts of two chemical subgroupsin central eastern China:Indication of ridge subduction.Lithos,150:26-36
Li XH,Li WX,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role ofmantle-derived magma in genesis of Early Yanshanian granites in theNanling Range,South China:In situ zircon Hf-O isotopicconstraints.Science in China(Series D),52(9):1262-1278
Li XH,Li WX,Li QL,Wang XC,Liu Y and Yang YH.2010.Petrogenesis and tectonic significance of the~850Ma Gangbianalkaline complex in South China:Evidence from in situ zircon U-Pbdating,Hf-O isotopes and whole-rock geochemistry.Lithos,114(1-2):1-15
Li JX,Qin KZ,Li GM and Yang LK.2007.K-Ar and40Ar/39Ar agedating of Nimu porphyry copper orefield in Central Gangdese:Constrains on magmatic-hydrothermal evolution and metallogenetictectonic setting.Acta Petrologica Sinica,23(5):953-966(inChinese with English abstract)
Li JX,Qin KZ,Li GM,Xiao B,Chen L and Zhao JX.2011.Postcollisional ore-bearing adakitic porphyries from Gangdese porphyrycopper belt,southern Tibet:Melting of thickened juvenile arc lowercrust.Lithos,126(3-4):265-277
Li TD.2002.New progress in the geoscience study of the Qinghai-Tibetplateau.Geological Bulletin of China,21(7):370-376(inChinese with English abstract)
Lin W,Liang HY,Zhang YQ and Xie YW.2004.Petrochemistry andSHRIMP U-Pb zircon age of the Chongjiang ore-bearing porphyry inthe Gangdese porphyry copper belt.Geochimica,33(6):585-592(in Chinese with English abstract)
Liu Y,Liu HC and Li XH.1996.Simultaneous and precisedetermination of 40 trace elements in rock samples using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract)
Liu YJ,Cao LM,Li ZL,Wang HN,Chu TQ and Zhang JR.1984.Element Geochemistry.Beijing:Science Press,1-548(inChinese)
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010a.Continental and oceanic crust recycling-induced melt-peridotiteinteractions in the Trans-North China Orogen:U-Pb dating,Hfisotopes and trace elements in zircons from mantle xenoliths.Journalof Petrology,51(1-2):537-571
Liu YS,Hu ZC,Zong KQ,Gao CG,Gao S,Xu JA and Chen HH.2010b.Reappraisement and refinement of zircon U-Pb isotope andtrace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546
Ludwig KR.2000.User’s manual for isoplot 3.00:A geochronologicaltoolkit for Microsoft excel.Berkeley Geochronology CenterSpecial Publication
Luo MC,Wang LQ,Leng QF and Chen W.2011.Zircon Hf isotope andCe4+/Ce3+ratio of the monzogranite porphyry and biotite monzoniticgranite in Bangpu Mo(Cu)deposit,Tibet.Mineral Deposits,30(2):266-278(in Chinese with English abstract)
Luo MC,Mao JW,Wang LW,Leng QF and Chen W.2012.Fluidinclusion evidence for magmatic-hydrothermal evolution in theBangpu porphyry molybdenum-copper deposit,Tibet.ActaGeoscientia Sinica,33(4):471-484(in Chinese with Englishabstract)
Mcdonough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
McM anus J,Berelson WM,Severmann S,Poulson RL,Hammond DE,Klinkhammer GP and Holm C.2006.Molybdenum and uraniumgeochemistry in continental margin sediments:Paleoproxy potential.Geochimica et Cosmochimica Acta,70(18):4643-4662
Meng XJ,Hou ZQ,Gao YF,Huang W,Qu XM and Qu WJ.2003.Development of porphyry copper-molybdenum-lead-zinc ore formingsystem in East Gangdese belt,Tibet:Evidence from Re-Os age ofmolybdenite in Bangpu copper polymetallic deposit.MineralDeposits,22(3):246-252(in Chinese with English abstract)
Mustard R,Ulrich T,Kamenetsky VS and Mernagh T.2006.Gold andmetal enrichment in natural granitic melts during fractionalcrystallization.Geology,34(2):85-88
Pan GT,Mo XX,Hou ZQ,Zhu DC,Wang LQ,Li GM,Zhao ZD,GengQR and Liao ZL.2006.Spatial-temporal framework of the GangdeseOrogenic Belt and its evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract)
Qu XM,Hou ZQ and Huang W.2001.Is Gangdese porphyry copper beltthe second“Yulong”copper belt?Mineral Deposits,20(4):355-366(in Chinese with English abstract)
Qu XM,Hou ZQ and Li YG.2004.Melt components derived from asubducted slab in late orogenic ore-bearing porphyries in theGangdese copper belt,southern Tibetan Plateau.Lithos,74(3-4):131-148
Qu XM,Hou ZQ,Guo LJ and Xu WY.2004.Source compositions andcrustal contaminations of adakitic ore-bearing porphyries in theGangdese copper belt:Nd,Sr,Pb and O isotope constraints.ActaGeologica Sinica,78(6):813-821(in Chinese with Englishabstract)
Rimmer SM.2004.Geochemical paleoredox indicators in DevonianMississippian black shales,central Appalachian basin(USA).Chemical Geology,206(3-4):373-391
Robb L.2005.Introduction to Ore-forming Processes.Oxford,UK:Blackwell Publication,1-373
Rudnick RL and Gao S.2003.Composition of the continental crust.In:Heinrich DH and Turekian KKE(eds.).Treatise on Geochemistry.Oxford:Elsevier-Pergamon,1-64
Rui ZY,Hou ZQ,Qu XM,Zhang LS,Wang LS and Liu YL.2003.Metallogenetic epoch of Gangdese porphyry copper belt and uplift ofQinghai-Tibet Plateau.Mineral Deposits,22(3):217-225(inChinese with English abstract)
Scott C,Lyons TW,Bekker A,Shen Y,Poulton SW,Chu X and AnbarAD.2008.Tracing the stepwise oxygenation of the Proterozoicocean.Nature,452(7186):456-459
Sun SS and McD onough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in OceanicBasins.Geological Society,London,Special Publications,42(1):313-345
Sun WD,Arculus RJ,Bennett VC,Eggins SM and Binns RA.2003a.Evidence for rhenium enrichment in the mantle wedge fromsubmarine arc-like volcanic glasses(Papua New Guinea).Geology,31(10):845-848
Sun WD,Bennett VC,Eggins SM,Arculus RJ and Perfit MR.2003b.Rhenium systematics in submarine MORB and back-arc basinglasses:Laser ablation ICP-MS results.Chemical Geology,196(1-4):259-281
Sun WD,Arculus RJ,Kamenetsky VS and Binns RA.2004a.Release ofgold-bearing fluids in convergent margin magmas prompted bymagnetite crystallization.Nature,431(7011):975-978
Sun WD,Bennett VC and Kamenetsky VS.2004b.The mechanism of Reenrichment in arc magmas:Evidence from Lau Basin basaltic glassesand primitive melt inclusions.Earth and Planetary Science Letters,222(1):101-114
Sun WD,Liang HY,Ling MX,Zhan MZ,Ding X,Zhang H,Yang XY,Li YL,Ireland TR,Wei QR and Fan WM.2013.The link betweenreduced porphyry copper deposits and oxidized magmas.Geochimicaet Cosmochimica Acta,103:263-275
Sun ZM,Jiang W,Pei JL and Li HB.2008.New Early Cretaceouspaleomagnetic data from volcanic of the eastern Lhasa Block and itstectonic implications.Acta Petrologica Sinica,24(7):1621-1626(in Chinese with English abstract)
Sun ZM,Jiang W,Li HB,Pei JL and Zhu ZM.2010.Newpaleomagnetic results of Paleocene volcanic rocks from the Lhasablock:Tectonic implications for the collision of India and Asia.Tectonophysics,490(3-4):257-266
Tang JX,Dor J,Liu HF,Lang XH,Zhang JS,Zheng WB and Ying LJ.2012.Minerogenetic series of ore deposits in the east part of theGangdise metallogenic belt.Acta Geoscientia Sinica,33(4):393-410(in Chinese with English abstract)
Tang XD,Huang BC,Yang LK,Yi ZY,Qiao QQ and Chen LW.2013.Paleomagnetism and Ar-Ar geochronology of Cretaceous volcanicrocks in the middle Lhasa terrane,China and tectonic implications.Chinese Journal of Geophysics,56(1):136-149(in Chinese withEnglish abstract)
Tu XL,Zhang H,Deng WF,Ling MX,Liang HY,Liu Y and Sun WD.2011.Application of RESOlution in-situ laser ablation ICP-MS intrace element analyses.Geochimica,40(1):83-98(in Chinesewith English abstract)
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zirconmegacrysts from kimberlite:Oxygen isotope variability among mantlemelts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Valley JW,Lackey JS,Cavosie AJ,Clechenko CC,Spicuzza MJ,BaseiMAS,Bindeman IN,Ferreira VP,Sial AN,King EM,Peck WH,Sinha AK and Wei CS.2005.4.4 billion years of crustalmaturation:Oxygen isotope ratios of magmatic zircon.Contributionsto Mineralogy and Petrology,150(6):561-580
Wang LL,Mo XX,Li B,Dong GC and Zhao ZD.2006.Geochronologyand geochemistry of the ore-bearing porphyry in Qulong Cu(Mo)oredeposit,Tibet.Acta Petrologica Sinica,22(4):1001-1008(inChinese with English abstract)
Wang LQ,Tang JX,Chen YC,Luo MC,Leng QF,Chen W and WangH.2011.LA-ICP-MS zircon U-Pb dating of ore-bearingmonzogranite porphyry in Bangpu molybdenum(copper)deposit,Tibet and its significance.Mineral Deposits,30(2):349-360(inChinese with English abstract)
Wang LQ,Luo MC,Yuan ZJ,Chen W,Leng QF and Zhang XQ.2012.Sulfur,Lead,Carbon and Oxygen isotope composition and source ofore-forming materials of the Bangpu Pb-Zn ore deposit in Tibet.ActaGeoscientia Sinica,33(4):435-443(in Chinese with Englishabstract)
Wang LQ,Tang JX,Cheng WB,Chen W,Zhang Z,Lin X,Luo MCand Yang C.2014.Origin of the ore-forming fluids and metals of theBangpu porphyry Mo-Cu deposit of Tibet,China:Constraints fromHe-Ar,H-O,S and Pb isotopes.Journal of Asian Earth Sciences,103:276-287
Wang LQ,Tang JX,Chen W,Luo MC,Kang HR and Leng QF.2014.Mineralogical characteristics of skarn in the Bangpu Mo polymetallicdeposit,Tibet,and their geological significance.Geology in China,41(2):562-576(in Chinese with English abstract)
Wang QH,Wang BS,Li JG,Yao P,Li Z,Zhou ZY,Cheng LJ and LiuHF.2002.Basic features and ore prospect evaluation of theGangdise island arc,Tibet and its copper polymetallic ore belt.Geological Bulletin of China,21(1):35-40(in Chinese withEnglish abstract)
Wang ZH,Liu YL,Liu HF,Guo LS,Zhang JS and Xu KF.2012.Geochronology and geochemistry of the Bangpu Mo-Cu porphyry oredeposit,Tibet.Ore Geology Reviews,46:95-105
Wen Q,Duo J,Wen CQ,Zhang XQ,Zhou X,Hou Y and Fei CG.2011.Dating of monzonitic granite porphyry in the Bangpu Mo-Cudeposit,Tibet.Journal of Mineralogy and Petrology,31(2):48-53(in Chinese with English abstract)
Wu FY and Yang JH.2006.Zircon U-Pb and Hf isotopic constraints onthe multiple components in granites.Geochimica et CosmochimicaActa,70(18):A709
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints oninterpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xu WC,Zhang HF,Guo L and Yuan HL.2010.Miocene high Sr/Ymagmatism,south Tibet:Product of partial melting of subductedIndian continental crust and its tectonic implication.Lithos,114(3-4):293-306
Xu XZ,Yang JS,Li TF,Chen SY,Ren YF,Li ZL and Shi YR.2007.SHRIMP U-Pb ages and inclusions of zircons from the Sumdo eclogitein the Lhasa block,Tibet,China.Geological Bulletin of China,26(10):1340-1355(in Chinese with English abstract)
Xu ZQ,Yang JS,Li WC,Li HQ,Cai ZH,Yan Z and Ma CQ.2013.Paleo-Tethys system and accretionary orogen in the Tibet Plateau.Acta Petrologica Sinica,29(6):1847-1860(in Chinese withEnglish abstract)
Yang JS,Xu ZQ,Geng QR,Li ZL,Xu XZ,Li TF,Ren YF,Li HQ,Cai ZH,Liang FH and Chen SY.2006.A possible new HP/UHP(?)metamorphic belt in China:Discovery of eclogite in the LahsaTerrane,Tibet.Acta Geologica Sinica,80(12):1787-1792(inChinese with English abstract)
Yang JS,Xu ZQ,Li TF,Li HQ,Li ZL,Ren YF,Xu XZ and Chen SY.2007.Oceanic subduction-type eclogite in the Lhasa block,Tibet,China:Remains of the Paleo-Tethys ocean basin?Geological Bulletinof China,26(10):1277-1287(in Chinese with English abstract)
Yang JS,Xu ZQ,Li ZL,Xua XZ,Li TF,Ren YF,Li HQ,Chen SYand Robinson PT.2009.Discovery of an eclogite belt in the Lhasablock,Tibet:A new border for Paleo-Tethys?Journal of Asian EarthSciences,34(1):76-89
Yi ZY,Huang BC,Chen JS,Chen LW and Wang HL.2011.Paleomagnetism of Early Paleogene marine sediments in southernTibet,China:Implications to onset of the India-Asia collision andsize of Greater India.Earth and Planetary Science Letters,309(1-2):153-165
Zhang H,Sun WD,Yang XY,Liang HY,Wang BH,Wang RL andWang YX.2011.Geochronology and metallogenesis of theShapinggou giant porphyry molybdenum deposit in the Dabie orogenicbelt.Acta Geologica Sinica,85(12):2039-2059(in Chinese withEnglish abstract)
Zhang H,Li CY,Yang XY,Sun YL,Deng JH,Liang HY,Wang RL,Wang BH,Wang YX and Sun WD.2014.Shapinggou:The largestClimax-type porphyry Mo deposit in China.International GeologyReview,56(3):313-331
Zhang QL,Qu XM,Xu WY,Hou ZQ and Chen WS.2003.Study of thefluid inclusions from Nanmu porphyry Cu-Mo deposit in Tibet.ActaPetrologica Sinica,19(2):251-259(in Chinese with Englishabstract)
Zhao XY,Yang ZS,Hou ZQ,Zheng YC,Liu YC,Tian SH,Fu Q andFei F.2013.Petrogenesis of diabase porphyrite in Bangpu deposit ofTibet and its instructions to the regional tectonic and magmaticevolution.Acta Petrologica Sinica,29(11):3767-3778(inChinese with English abstract)
Zheng YC,Hou ZQ,Li QY,Sun QZ,Liang W,Fu Q,Li W and HuangKX.2012.Origin of Late Oligocene adakitic intrusives in thesoutheastern Lhasa terrane:Evidence from in situ zircon U-Pbdating,Hf-O isotopes,and whole-rock geochemistry.Lithos,148:296-311
Zheng YY,Xue YX,Cheng LJ,Fan ZH and Gao SB.2004.Finding,characteristics and significances of Qulong superlarge porphyrycopper(molybdenum)deposit,Tibet.Earth Science,29(1):103-108(in Chinese with English abstract)
Zhou X,Wen CQ,Fei CG,Cao SY,Wu PY and Huo Y.2010a.Geochemical characteristics of monzonite granite porphyry in Bangpuporphyry Mo deposit,Tibet,and its tectonic significance.Journal ofMineralogy and Petrology,30(4):48-54(in Chinese with Englishabstract)
Zhou X,Wen CQ,Huo Y,Fei GC and Wu PY.2010b.Characteristicsof ore-forming fluid of Bangpu molybdenum-copper polymetallicdeposit,Maizhokunggar area,Tibet,China.Geological Bulletin ofChina,29(7):1039-1048(in Chinese with English abstract)
Zhou X,Wen CQ,Wen Q,Wu PY,Cao SY,Fei CG,Huo Y and ZhouY.2010c.Zircon U-Pb SHRIMP dating of the monzonite graniteporphyry from the Bangpu large porphyry molybdenum-copperdeposits,Tibet,and its geological significance.Bulletin ofMineralogy,Petrology and Geochemistry,29(4):373-379(inChinese with English abstract)
Zhou X,Wen CQ,Zhang XQ,Cao SY,Wu PY,Zhou Y and Fei GC.2010d.Rb-Sr isochron age dating of the Bangpu large-scale Mo-Cupolymetallic deposit,Tibet and its geological significance.GeologicalJournal of China Universities,16(4):448-456(in Chinese withEnglish abstract)
Zhou X.2012.Genisis study of Mo-Cu polymetallic deposit from theBangpu,Tibet.Ph.D.Dissertation.Chengdu:Chengdu Universityof Technology(in Chinese with English summary)
Zhu DC,Pan GT,Mo XX,Wang LQ,Liao ZL,Zhao ZD,Dong GC andZhou CY.2006.Late Jurassic-Early Cretaceous geodynamic settingin middle-northern Gangdese;New insights from volcanic rocks.Acta Petrologica Sinica,22(3):534-546(in Chinese withEnglish abstract)
Zhu DC,Zhao ZD,Niu YL,Wang Q,Dilek Y,Dong GC and Mo XX.2012.Origin and Paleozoic tectonic evolution of the Lhasa Terrane.Geological Journal of China Universities,18(1):1-15(in Chinesewith English abstract)
Zhu DC,Zhao ZD,Niu YL,Dilek Y,Hou ZQ and Mo XX.2013.Theorigin and pre-Cenozoic evolution of the Tibetan Plateau.GondwanaResearch,23(4):1429-1454
陈松永.2010.西藏拉萨地块中古特提斯缝合带的厘定.博士学位论文.北京:中国地质科学院,1-187
冯岩,温珍河,侯方辉,高志清,祁江豪.2013.青藏高原及其邻区晚古生代以来构造演化与古大陆再造.海洋地质与第四纪地质,33(1):33-44
高永丰,侯增谦,魏瑞华.2003.冈底斯晚第三纪斑岩的岩石学、地球化学及其地球动力学意义.岩石学报,19(3):418-428
侯增谦,曲晓明,黄卫,高永丰.2001.冈底斯斑岩铜矿成矿带有望成为西藏第二条“玉龙”铜矿带.中国地质,28(10):27-29
侯增谦,莫宣学,高永丰,曲晓明,孟祥金.2003.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩(以西藏和智利斑岩铜矿为例).矿床地质,22(1):1-12
侯增谦,高永丰,孟祥金,曲晓明,黄卫.2004.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制.岩石学报,20(2):239-248
侯增谦,莫宣学,杨志明,王安建,潘桂棠,曲晓明,聂凤军.2006.青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型.中国地质,33(2):340-351
冷秋锋,王立强,应立娟,郑文宝,罗茂澄,陈伟,林彬,王艺云.2012.西藏邦铺钼(铜)矿床辉绿玢岩脉体LA-ICP-MS锆石UPb定年及其地质意义.地球学报,33(4):559-568
李奋其,刘伟,王保弟,张士贞.2012.拉萨地块内部古特提斯洋早中三叠世仍在俯冲———来自火山岩和高压变质岩的证据.岩石矿物学杂志,31(2):119-132
李金祥,秦克章,李光明,杨列坤.2007.冈底斯中段尼木斑岩铜矿田的K-Ar、40Ar/39Ar年龄:对岩浆-热液系统演化和成矿构造背景的制约.岩石学报,23(5):953-966
李廷栋.2002.青藏高原地质科学研究的新进展.地质通报,21(7):370-376
林武,梁华英,张玉泉,谢玉玲.2004.冈底斯铜矿带冲江含矿斑岩的岩石化学及锆石SHRIMP年龄特征.地球化学,33(6):585-592
刘颖,刘海臣,李献华.1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558
刘英俊,曹励明,李兆麟,王鹤年,储同庆,张景荣.1984.元素地球化学.北京:科学出版社,1-548
罗茂澄,王立强,冷秋锋,陈伟.2011.邦铺钼(铜)矿床二长花岗斑岩、黑云二长花岗岩锆石Hf同位素和Ce4+/Ce3+比值.矿床地质,30(2):266-278
罗茂澄,毛景文,王立强,冷秋锋,陈伟.2012.西藏邦铺斑岩钼铜矿床岩浆-热液流体演化:流体包裹体研究.地球学报,33(4):471-484
孟祥金,侯增谦,高永丰,黄卫,曲晓明,屈文俊.2003.西藏冈底斯带东段斑岩铜钼铅锌成矿系统的发育时限:帮浦铜多金属矿床辉钼矿Re-Os年龄证据.矿床地质,22(3):246-252
潘桂棠,莫宣学,侯增谦,朱弟成,王立全,李光明,赵志丹,耿全如,廖忠礼.2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533
曲晓明,侯增谦,黄卫.2001.冈底斯斑岩铜矿成矿带:西藏第二条玉龙铜矿带?矿床地质,20(4):355-366
曲晓明,侯增谦,国连杰,徐文艺.2004.冈底斯铜矿带埃达克质含矿斑岩的源区组成与地壳混染:Nd、Sr、Pb、O同位素约束.地质学报,78(6):813-821
芮宗瑶,侯增谦,曲晓明,张立生,王龙生,刘玉琳.2003.冈底斯斑岩铜矿成矿时代及青藏高原隆升.矿床地质,22(3):217-225
孙知明,江万,裴军令,李海兵.2008.青藏高原拉萨地块早白垩纪火山岩古地磁结果及其构造意义.岩石学报,24(7):1621-1626
唐菊兴,多吉,刘鸿飞,郎兴海,张金树,郑文宝,应立娟.2012.冈底斯成矿带东段矿床成矿系列及找矿突破的关键问题研究.地球学报,33(4):393-410
唐祥德,黄宝春,杨列坤,易治宇,乔庆庆,陈力为.2013.拉萨地块中部晚白垩世火山岩Ar-Ar年代学和古地磁研究结果及其构造意义.地球物理学报,56(1):136-149
涂湘林,张红,邓文峰,凌明星,梁华英,刘颖,孙卫东.2011.RESOlution激光剥蚀系统在微量元素原位微区分析中的应用.地球化学,40(1):83-98
王亮亮,莫宣学,李冰,董国臣,赵志丹.2006.西藏驱龙斑岩铜矿含矿斑岩的年代学与地球化学.岩石学报,22(4):1001-1008
王立强,唐菊兴,陈毓川,罗茂澄,冷秋锋,陈伟,王焕.2011.西藏邦铺钼(铜)矿床含矿二长花岗斑岩LA-ICP-MS锆石U-Pb定年及地质意义.矿床地质,30(2):349-360
王立强,罗茂澄,袁志洁,陈伟,冷秋锋,张学全.2012.西藏邦铺铅锌矿床S、Pb、C、O同位素组成及成矿物质来源研究.地球学报,33(4):435-443
王立强,唐菊兴,陈伟,罗茂澄,康浩然,冷秋锋.2014.西藏邦铺钼多金属矿床矽卡岩矿物学特征及其地质意义.中国地质,41(2):562-576
王全海,王保生,李金高,姚鹏,李志,周祖翼,程力军,刘鸿飞.2002.西藏冈底斯岛弧及其铜多金属矿带的基本特征与远景评估.地质通报,21(1):35-40
温泉,多吉,温春齐,张学全,周雄,霍艳,费光春.2011.西藏邦铺钼铜矿区花岗斑岩成岩年龄研究.矿物岩石,31(2):48-53
徐向珍,杨经绥,李天福,陈松永,任玉峰,李兆丽,石玉若.2007.青藏高原拉萨地块松多榴辉岩的锆石SHRIMP U-Pb年龄及锆石中的包裹体.地质通报,26(10):1340-1355
许志琴,杨经绥,李文昌,李化启,蔡志慧,闫臻,马昌前.2013.青藏高原中的古特提斯体制与增生造山作用.岩石学报,29(6):1847-1860
杨经绥,许志琴,耿全如,李兆丽,徐向珍,李天福,任玉峰,李化启,蔡志慧,梁凤华,陈松永.2006.中国境内可能存在一条新的高压/超高压(?)变质带———青藏高原拉萨地体中发现榴辉岩带.地质学报,80(12):1787-1792
杨经绥,许志琴,李天福,李化启,李兆丽,任玉峰,徐向珍,陈松永.2007.青藏高原拉萨地块中的大洋俯冲型榴辉岩:古特提斯洋盆的残留?地质通报,26(10):1277-1287
张红,孙卫东,杨晓勇,梁华英,王波华,王瑞龙,王玉贤.2011.大别造山带沙坪沟特大型斑岩钼矿床年代学及成矿机理研究.地质学报,85(12):2039-2059
张绮玲,曲晓明,徐文艺,侯增谦,陈伟十.2003.西藏南木斑岩铜钼矿床的流体包裹体研究.岩石学报,19(2):251-259
赵晓燕,杨竹森,侯增谦,郑远川,刘英超,田世洪,付强,费凡.2013.西藏邦铺矿区辉绿玢岩成因及对区域构造岩浆演化的指示.岩石学报,29(11):3767-3778
郑有业,薛迎喜,程力军,樊子珲,高顺宝.2004.西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义.地球科学,29(1):103-108
周雄,温春齐,费光春,曹盛远,吴鹏宇,霍艳.2010a.西藏邦铺斑岩型钼矿床二长花岗斑岩地球化学特征及构造意义.矿物岩石,30(4):48-54
周雄,温春齐,霍艳,费光春,吴鹏宇.2010b.西藏墨竹工卡地区邦铺钼铜多金属矿床成矿流体的特征.地质通报,29(7):1039-1048
周雄,温春齐,温泉,吴鹏宇,曹盛远,费光春,霍艳,周玉.2010c.西藏邦铺大型斑岩钼-铜矿床二长花岗斑岩锆石SHRIMP定年及其地质意义.矿物岩石地球化学通报,29(4):373-379
周雄,温春齐,张学全,曹盛远,吴鹏宇,周玉,费光春.2010d.西藏邦铺大型钼铜多金属矿床Rb-Sr等时线年龄及地质意义.高校地质学报,16(4):448-456
周雄.2012.西藏邦铺钼铜多金属矿床成因研究.博士学位论文.成都:成都理工大学
朱弟成,潘桂棠,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,赵志丹,牛耀龄,王青,Yildirim D,董国臣,莫宣学.2012.拉萨地体的起源和古生代构造演化.高校地质学报,18(1):1-15
①西藏自治区地勘局地热地质大队.2009.西藏自治区墨竹工卡县邦铺矿区钼(铜)多金属矿详查报告