西藏狮泉河蛇绿岩中侏罗世晚期(ca.163Ma)OIB型辉绿岩及高镁闪长岩年代学及地球化学特征:早期洋壳俯冲产物?
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摘要
本文首次报道了侵位于狮泉河蛇绿岩(蛇纹石化超基性岩)中的具有OIB性质的辉绿岩以及赞岐岩型的高镁闪长岩。其中闪长岩具有较高的TiO_2、Y及Yb含量,较低的Sr/Y比值和La/Yb比值,与日本Setouchi火山岩带的赞岐岩以及前人报道的同期洋内初始俯冲成因相关的高镁安山岩性质一致。辉绿岩富LREE,高Zr/Y、TiO_2/Yb和Nb/Yb比值,Nb、Ti负异常,Pb正异常,表现出了俯冲带相关的OIB性质;采用LA-ICP-MS锆石U-Pb定年方法,测得辉绿岩脉的成岩年龄为163. 7±0. 54Ma(MSWD=3. 8),且该年龄与前人报道的160. 8±2. 3Ma的高镁安山岩年龄较为接近。综合分析本文及前人年代学与岩石地球化学相关数据,认为狮泉河辉绿岩和闪长岩同时形成于洋内俯冲的初始阶段。这种岩石组合与太平洋IBM岛链初始俯冲的岩石组合相似,但该OIB成因机制中俯冲作用与地幔柱之间的相互关系仍需进一步讨论。
This paper for the first time reports OIB-type diabase intruding into the Shiquanhe ophiolite,as well as diorite with high magnesium andesite( HMA) properties. The diorites have high TiO_2,Y and Yb contents,lower Sr/Y and La/Yb ratios,which is consistent with the high-magnesia andesite associated with the sanukite rock in the Setouchi volcanic rock belt in Japan and the initial inner-oceanic subduction reported by the predecessors. Based on LA-ICP-MS zircon U-Pb isotope dating,the OIB-type diabase yields a zircon U-Pb weighted mean age of 163. 7 ± 0. 54 Ma( MSWD = 3. 8). The measured samples have SiO_2 of 40. 93% ～ 49. 88% and Mg~# of 46. 3 ～ 60. 4,with the following geochemical characteristics: rich in LREE,with high Zr/YTiO_2/Yb and Nb/Yb ratios,Nb and Ti negative anomalies,and Pb positive anomalies,indicating OIB properties associated with a subduction zone. Putting the OIB-type diabase and associated HMA-type diorite back to the Shiquanhe ophiolite background,it is inferred that the Shiquanhe diabase and diorite are simultaneously formed in the initial stage of oceanic crust subduction. Besides,the timing of initial subduction associated with the Shiquanhe ophiolite is much later than that of the Bangong-Nujiang suture zone,suggesting that ophiolites from the two belts represent remnants of separate oceanic crusts. The rock assemblage of the studied samples is similar with the synchronous HMA-type diorite,while the OIB-type diabase from the Shiquanhe ophiolite is similar to the rock assemblage in the Izu-Bonin-Mariana island arc( Southwest Pacific) formed during the initial stage of oceanic subduction,suggesting the presence of an early stage oceanic subduction zone in the late Mid-Jurassic time,but the relationship between the subduction and the OIB genesis remains uncertainty and needs further studying.
This paper for the first time reports OIB-type diabase intruding into the Shiquanhe ophiolite,as well as diorite with high magnesium andesite( HMA) properties. The diorites have high TiO_2,Y and Yb contents,lower Sr/Y and La/Yb ratios,which is consistent with the high-magnesia andesite associated with the sanukite rock in the Setouchi volcanic rock belt in Japan and the initial inner-oceanic subduction reported by the predecessors. Based on LA-ICP-MS zircon U-Pb isotope dating,the OIB-type diabase yields a zircon U-Pb weighted mean age of 163. 7 ± 0. 54 Ma( MSWD = 3. 8). The measured samples have SiO_2 of 40. 93% ～ 49. 88% and Mg~# of 46. 3 ～ 60. 4,with the following geochemical characteristics: rich in LREE,with high Zr/YTiO_2/Yb and Nb/Yb ratios,Nb and Ti negative anomalies,and Pb positive anomalies,indicating OIB properties associated with a subduction zone. Putting the OIB-type diabase and associated HMA-type diorite back to the Shiquanhe ophiolite background,it is inferred that the Shiquanhe diabase and diorite are simultaneously formed in the initial stage of oceanic crust subduction. Besides,the timing of initial subduction associated with the Shiquanhe ophiolite is much later than that of the Bangong-Nujiang suture zone,suggesting that ophiolites from the two belts represent remnants of separate oceanic crusts. The rock assemblage of the studied samples is similar with the synchronous HMA-type diorite,while the OIB-type diabase from the Shiquanhe ophiolite is similar to the rock assemblage in the Izu-Bonin-Mariana island arc( Southwest Pacific) formed during the initial stage of oceanic subduction,suggesting the presence of an early stage oceanic subduction zone in the late Mid-Jurassic time,but the relationship between the subduction and the OIB genesis remains uncertainty and needs further studying.
引文
Abratis M and W9rner G.2001.Ridge collision,slab-window formation,and the flux of Pacific asthenosphere into the Caribbean realm.Geology,29(2):127-130
Aldanmaz E,Pearce JA,Thirlwall MF and Mitchell JG.2000.Petrogenetic evolution of Late Cenozoic,post-collision volcanism in western Anatolia,Turkey.Journal of Volcanology and Geothermal Research,102(1-2):67-95
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb.Chemical Geology,192(1-2):59-79
Bloomer SH and Hawkins JW.1987.Petrology and geochemistry of boninite series volcanic rocks from the Mariana trench.Contributions to Mineralogy and Petrology,97(3):361-377
Blundy J and Wood B.2003.Partitioning of trace elements between crystals and melts.Earth and Planetary Science Letters,210(3-4):383-397
Dai JG,Wang CS and Li YL.2012.Relicts of the Early Cretaceous seamounts in the central-western Yarlung Zangbo Suture Zone,southern Tibet.Journal of Asian Earth Sciences,53:25-37
Defant MJ,Jackson TE,Drummond MS,de Boer JZ,Bellon H,Feigenson MD,Maury RC and Stewart RH.1992.The geochemistry of young volcanism throughout western Panama and southeastern Costa Rica:An overview.Journal of the Geological Society,149(4):569-579
Deng JF,Liu C,Feng YF,Xiao QH,Su SG,Zhao GC,Kong WQ and Cao WY.2010.High magnesian andesitic/dioritic rocks(HMA)and magnesian andesitic/dioritic rocks(MA):Two igneous rock types related to oceanic subduction.Geology in China,37(4):1112-1118(in Chinese with English abstract)
Duggen S,Hoernle K,Van den Bogaard P,Rüpke L and Morgan JP.2003.Deep roots of the Messinian salinity crisis.Nature,422(6932):602-606
Faccenna C,Piromallo C,Crespo‐Blanc A,Jolivet L and Rossetti F.2004.Lateral slab deformation and the origin of the western Mediterranean arcs.Tectonics,23(1):TC1012
Faccenna C,Civetta L,D'Antonio M,Funiciello F,Margheriti L and Piromallo C.2005.Constraints on mantle circulation around the deforming Calabrian slab.Geophysical Research Letters,32(6):L06311
Faccenna C,Becker TW,Lallemand S,Lagabrielle Y,Funiciello F and Piromallo C.2010.Subduction-triggered magmatic pulses:A new class of plumes?Earth and Planetary Science Letters,299(1-2):54-68
Furukawa Y and Tatsumi Y.1999.Melting of a subducting slab and production of high-Mg andesite magmas:Unusual magmatism in SWJapan at 13~15Ma.Geophysical Research Letters,26(15):2271-2274
Girardeau J,Marcoux J,Fourcade E,Bassoullet JP and Youking T.1985.Xainxa ultramafic rocks,central Tibet,China:Tectonic environment and geodynamic significance.Geology,13(5):330
Gao S,Rudnick RL,Yuan HL,Liu XM,Liu YS,Xu WL,Ling WL,Ayers J,Wang XC and Wang QH.2004.Recycling lower continental crust in the North China craton.Nature,432(7019):892-897
Gao XY and Zheng YF.2011.On the Zr-in-rutile and Ti-in-zircon geothermometers.Acta Petrologica Sinica,27(2):417-432(in Chinese with English abstract)
Gehrels G,Kapp P,De Celles P,Pullen A,Blakey R,Weislogel A,Ding L,Guynn J,Martin A,Mc Quarrie N and Yin A.2011.Detrital zircon geochronology of pre-Tertiary strata in the Tibetan‐Himalayan orogen.Tectonics,30(5):TC5016
Gorring ML and Kay SM.2001.Mantle processes and sources of Neogene slab window magmas from Southern Patagonia,Argentina.Journal of Petrology,42(6):1067-1094
Green TH.1994.Experimental studies of trace-element partitioning applicable to igneous petrogenesis:Sedona 16 years later.Chemical Geology,117(1-4):1-36
Hanyu T,Tatsumi Y and Nakai S.2003.Evidence of slab melting for the formation of high-Mg andesite:A Hafnium isotope study of Setouchi volcanics,Japan.In:Geophysical Research Abstracts,Vol.5.Washington:EGS
Hanyu T,Tatsumi Y,Nakai S,Chang Q,Miyazaki T,Sato K,Tani K,Shibata T and Yoshida T.2006.Contribution of slab melting and slab dehydration to magmatism in the Japanese arc.Geochimica et Cosmochimica Acta,70(S18):A229
Hermann J and Rubatto D.2009.Accessory phase control on the trace element signature of sediment melts in subduction zones.Chemical Geology,265(3-4):512-526
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Hoskin PWO and Ireland TR.2000.Rare earth element chemistry of zircon and its use as a provenance indicator.Geology,28(7):627
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hoskin PWO.2005.Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills,Australia.Geochimica et Cosmochimica Acta,69(3):637-648
Hu J,Li Q,Fang NQ,Yang JY and Ge DS.2015.Geochemistry characteristics of the Low Permian sedimentary rocks from central uplift zone,Qiangtang Basin,Tibet:Insights into source-area weathering,provenance,recycling,and tectonic setting.Arabian Journal of Geosciences,8(8):5373-5388
Huang TT,Xu JF,Chen JL,Wu JB and Zeng YC.2017.Sedimentary record of Jurassic northward subduction of the Bangong-Nujiang Ocean:Insights from detrital zircons.International Geology Review,59(2):166-184
Huang XL,Niu YL,Xu YG,Ma JL,Qiu HN and Niu JW.2013.Geochronology and geochemistry of Cenozoic basalts from eastern Guangdong,SE China:Constraints on the lithosphere evolution beneath the northern margin of the South China Sea.Contributions to Mineralogy and Petrology,165(3):437-455
Johnson MC and Plank T.2000.Dehydration and melting experiments constrain the fate of subducted sediments.Geochemistry,Geophysics,Geosystems,1(12):1007
Kamei A,Owada M,Nagao T and Shiraki K.2004.High-Mg diorites derived from sanukitic HMA magmas,Kyushu Island,Southwest Japan arc:Evidence from clinopyroxene and whole rock compositions.Lithos,75(3-4):359-371
Kapp P,Murphy MA,Yin A,Harrison TM,Ding L and Guo JH.2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet.Tectonics,22(4):1029
Kapp P,Yin A,Harrison TM and Ding L.2005.Cretaceous-Tertiary shortening,basin development,and volcanism in central Tibet.Geological Society of America Bulletin,117(7-8):865-878
Kapp P,Decelles 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.Geological Society of America Bulletin,119(7-8):917-933
Kay RW.1978.Aleutian magnesian andesites:Melts from subducted Pacific Ocean crust.Journal of Volcanology and Geothermal Research,4(1-2):117-132
Kepezhinskas P,Defant MJ and Drummond MS.1996.Progressive enrichment of island arc mantle by melt-peridotite interaction inferred from Kamchatka xenoliths.Geochimica et Cosmochimica Acta,60(7):1217-1229
Labanieh S,Chauvel C,Germa A and Quidelleur X.2018.Martinique:A clear case for sediment melting and slab dehydration as a function of distance to the trench.Journal of Petrology,53(12):2441-2464
Lan JB,Xu YG,Yang QJ and Huang XL.2007.~40Ma OIB-type mafic magmatism in the Gaoligong belt:Results of break-off between subducting Tethyan slab and Indian Plate?Acta Petrologica Sinica,23(6):1334-1346(in Chinese with English abstract)
Li JX,Qin KZ,Li GM,Richards JP,Zhao JX and Cao MJ.2014a.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 SM,Zhu DC,Wang Q,Zhao ZD,Sui QL,Liu SA,Liu D and Mo XX.2014b.Northward subduction of Bangong-Nujiang Tethys:Insight from Late Jurassic intrusive rocks from Bangong Tso in western Tibet.Lithos,205:284-297
Li SM,Zhu DC,Wang Q,Zhao ZD,Zhang LL,Liu SA,Chang QS,Lu YH,Dai JG and Zheng YC.2016.Slab-derived adakites and subslab asthenosphere-derived OIB-type rocks at 156±2Ma from the north of Gerze,central Tibet:Records of the Bangong-Nujiang oceanic ridge subduction during the Late Jurassic.Lithos,262:456-469
Li SM.2018.Subduction polarity and processes of the Bangong-Nujiang Tethys:Insights from igneous rocks and detrial zircons.Ph.D.Dissertation.Beijing:China University of Geosciences(in Chinese with English summary)
Lin B,Chen YC,Tang JX,Wang Q,Song Y,Yang C,Wang WL,He W and Zhang LJ.2017.40Ar/39Ar and Rb-Sr ages of the Tiegelongnan porphyry Cu-(Au)deposit in the Bangong Co-Nujiang Metallogenic Belt of Tibet,China:Implication for generation of super-Large deposit.Acta Geologica Sinica,91(2):602-616
Liu B,Ma CQ,Guo P,Sun Y,Gao K and Guo YH.2016.Evaluation of late Permian mafic magmatism in the central Tibetan Plateau as a response to plume-subduction interaction.Lithos,264:1-16
Liu DL,Huang QS,Fan SQ,Zhang LY,Shi RD and Ding L.2014.Subduction of the Bangong-Nujiang Ocean:Constraints from granites in the Bangong Co area,Tibet.Geological Journal,49(2):188-206
Liu WL,Huang QT,Gu M,Zhong Y,Zhou RJ,Gu XD,Zheng H,Liu JN,Lu XX and Xia B.2018.Origin and tectonic implications of the Shiquanhe high-Mg andesite,western Bangong suture,Tibet.Gondwana Research,60:1-14
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
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig KR.2003.User’s manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,Berkeley,CA:Berkeley Geochronology Center,4:1-70
Martin H.1999.Adakitic magmas:Modern analogues of Archaean granitoids.Lithos,46(3):411-429
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Ydiagram.Chemical Geology,56(3-4):207-218
Miyashiro A.1974.Volcanic rock series in island arcs and active continental margins.American Journal of Science,274(4):321-355
Nebel O,Vroon PZ,van Westrenen W,Iizuka T and Davies GR.2011.The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust,Banda arc,Indonesia.Earth and Planetary Science Letters,303(3-4):240-250
Niu YL.2009.Some basic concepts and problems on the petrogenesis of Intra-Plate Ocean Island basalts.Chinese Science Bulletin,54(22):4148-4160
Niu YL,Wilson M,Humphreys ER and O'Hara MJ.2011.The origin of intra-plate ocean Island Basalts(OIB):The lid effect and its geodynamic implications.Journal of Petrology,52(7-8):1443-1468
Pearce JA and Cann JR.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth and Planetary Science Letters,19(2):290-300
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb variations in volcanic rocks.Contributions to Mineralogy and Petrology,69(1):33-47
Pearce JA and Deng W.1988.The Ophiolites of the Tibetan Geotraverses,Lhasa to Golmud(1985)and Lhasa to Kathmandu(1986).Philosophical Transactions of the Royal Society of London,327(1594):215-238
Pearce JA,van der Laan SR,Arculus RJ,Murton BJ,Ishii T,Peate DWand Parkinson IJ.1992.Boninite and harzburgite from Leg 125(Bonin-Mariana forearc):A case study of magma genesis during the initial stages of subduction.Proceedings of the Ocean Drilling Program,Scientific Results,125:623-659
Plank T and Langmuir CH.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle.Chemical Geology,145(3-4):325-394
Qian Q and Hermann J.2010.Formation of High-Mg diorites through assimilation of peridotite by monzodiorite magma at crustal depths.Journal of Petrology,51(7):1381-1416
Reagan MK and Gill JB.1989.Coexisting calcalkaline and high-niobium basalts from Turrialba Volcano,Costa Rica:Implications for residual titanates in arc magma sources.Journal of Geophysical Research:Solid Earth,94(B4):4619-4633
Reagan MK,Ishizuka O,Stern RJ,Kelley KA,Ohara Y,Blichert-Toft J,Bloomer SH,Cash J,Fryer P,Hanan BB,Hickey-Vargas R,Ishii T,Kimura JI,Peate DW,Rowe MC and Woods M.2013.Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system.Geochemistry,Geophysics,Geosystems,11(3):Q03X12
Rogers G,Saunders AD,Terrell DJ,Verma SP and Marriner GF.1985.Geochemistry of Holocene volcanic rocks associated with ridge subduction in Baja California,Mexico.Nature,315(6018):389-392
Rollinson HR.1993.Using Geochemical Data:Evaluation,Presentation,Interpretation.Longman Scientific&Technical,Longman Group UK Ltd.,1-352
Rudnick RL and Fountain DM.1995.Nature and composition of the continental crust:A lower crustal perspective.Reviews of Geophysics,33(3):267-310
Sajona FG,Maury RC,Bellon H,Cotton J and Defant M.1996.High field strength element enrichment of Pliocene-Pleistocene island arc basalts,Zamboanga Peninsula,Western Mindanao(Philippines).Journal of Petrology,37(3):693-726
Shimoda G,Tatsumi Y,Nohda S,Ishizaka K and Jahn BM.1998.Setouchi high-Mg andesites revisited:Geochemical evidence for melting of subducting sediments.Earth and Planetary Science Letters,160(3-4):479-492
Sisson TW.1994.Hornblende-melt trace-element partitioning measured by ion microprobe.Chemical Geology,117(1-4):331-344
Skora S and Blundy J.2010.High-pressure hydrous phase relations of radiolarian clay and implications for the involvement of subducted sediment in arc magmatism.Journal of Petrology,51(11):2211-2243
Smithies RH and Champion DC.2000.The Archaean High-Mg diorite suite:Links to tonalite-trondhjemite-granodiorite magmatism and implications for Early Archaean crustal growth.Journal of Petrology,41(12):1653-1671
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
Spandler C,Hermann J,Faure K,Mavrogenes JA and Arculus RJ.2008.The importance of talc and chlorite“hybrid”rocks for volatile recycling through subduction zones:Evidence from the high-pressure subduction mélange of New Caledonia.Contributions to Mineralogy and Petrology,155(2):181-198
Stern RA and Hanson GN.1991.Archean High-Mg granodiorite:Aderivative of light rare earth element-enriched monzodiorite of mantle origin.Journal of Petrology,32(1):201-238
Stern RJ.2002.Subduction zones.Reviews of Geophysics,40(4):1012
Stern RJ and Gerya T.2018.Subduction initiation in nature and models:A review.Tectonophysics,746:173-198
Straub SM,Gomez-Tuena A,Stuart FM,Zellmer GF,Espinasa-Perena R,Cai Y and Iizuka Y.2011.Formation of hybrid arc andesites beneath thick continental crust.Earth and Planetary Science Letters,303(3-4):337-347
Sun SS and Mcdonough 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 Publications,42(1):313-345
Tang GJ and Wang Q.2010.High-Mg andesites and their geodynamic implications.Acta Petrologica Sinica,26(8):2495-2512(in Chinese with English abstract)
Tang GJ,Wang Q,Wyman DA,Li ZX,Zhao ZH and Jia XH.2010.Ridge subduction and crustal growth in the Central Asian Orogenic Belt:Evidence from Late Carboniferous adakites and high-Mg diorites in the western Junggar region,northern Xinjiang(West China).Chemical Geology,277(3):281-300
Tang GJ,Wyman DA,Wang Q,Li J,Li ZX,Zhao ZH and Sun WD.2012.Asthenosphere-lithosphere interaction triggered by a slab window during ridge subduction:Trace element and Sr-Nd-Hf-Os isotopic evidence from Late Carboniferous tholeiites in the western Junggar area(NW China).Earth and Planetary Science Letters,329-330:84-96
Tatsumi Y and Hanyu T.2003.Geochemical modeling of dehydration and partial melting of subducting lithosphere:Toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt,SW Japan.Geochemistry,Geophysics,Geosystems,4(9):1081
Tatsumi Y.2006.High-Mg andesites in the Setouchi volcanic belt,southwestern Japan:Analogy to Archean Magmatism and Continental Crust Formation?Annual Review of Earth&Planetary Science,34(1):467-499
Thorkelson DJ,Madsen JK and Sluggett CL.2011.Mantle flow through the Northern Cordilleran slab window revealed by volcanic geochemistry.Geology,39(3):267-270
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 Q,Wyman DA,Xu JF,Wan YS,Li C,Zi F,Jiang ZQ,Qiu HN,Chu ZY,Zhao ZH and Dong YH.2008.Triassic Nb-enriched basalts,magnesian andesites,and adakites of the Qiangtang terrane(Central Tibet):Evidence for metasomatism by slab-derived melts in the mantle wedge.Contributions to Mineralogy and Petrology,155(4):473-490
Wang Q,Li ZX,Chung SL,Wyman DA,Sun YL,Zhao ZH,Zhu YTand Qiu HN.2011.Late Triassic high-Mg andesite/dacite suites from northern Hohxil,North Tibet:Geochronology,geochemical characteristics,petrogenetic processes and tectonic implications.Lithos,126(1-2):54-67
Watson EB and Harrison TM.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types.Earth and Planetary Science Letters,64(2):295-304
Weinberg RF and HasalováP.2015.Water-fluxed melting of the continental crust:A review.Lithos,212-215:158-188
Wilson BM.2007.Igneous Petrogenesis A Global Tectonic Approach.Netherlands:Springer Science&Business Media
Wilson M.1989.Igneous Petrogenesis:A Global Tectonic Approach.London:Unwin Hyman
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Wood BJ and Turner SP.2009.Origin of primitive high-Mg andesite:Constraints from natural examples and experiments.Earth and Planetary Science Letters,283(1-4):59-66
Xia Y,Zhu DC,Zhao ZD,Wang Q,Yuan SH,Chen Y and Mo XX.2012.Whole-rock geochemistry and zircon Hf isotope of the OIB-type mafic rocks from the Comei Large Igneous Province in southeastern Tibet.Acta Petrologica Sinica,28(5):1588-1602(in Chinese with English abstract)
Xu JF,Shinjo R,Defant MJ,Wang Q and Rapp RP.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:Partial melting of delaminated lower continental crust?Geology,30(12):1111-1114
Xu MJ,Li C,Zhang XZ and Wu YW.2014.Nature and evolution of the Neo-Tethys in central Tibet:Synthesis of ophiolitic petrology,geochemistry,and geochronology.International Geology Review,56(9):1072-1096
Xu YG,Chung SL,Jahn BM and Wu GY.2001.Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China.Lithos,58(3-4):145-168
Xu YG.2002.Mantle plumes,large igneous provinces and their geologic consequences.Earth Science Frontiers,9(4):341-353(in Chinese with English abstract)
Yang F,Huang XL and Li J.2018.Magma processes and petrogenesis of the Late Cretaceous plagioclase-phyric basalt in the Changchengling area,South China.Acta Petrologica Sinica,34(1):157-171(in Chinese with English abstract)
Yin A and Harrison TM.2000.Geologic evolution of the HimalayanTibetan Orogen.Annual Review of Earth and Planetary Sciences,28:211-280
Yogodzinski MG,Kay RW,Volynets ON,Koloskov AV and Kay SM.1995.Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge.GSA Bulletin,107(5):505-519
Zeng M,Zhang X,Cao H,Ettensohn FR,Cheng WB and Lang XH.2016a.Late Triassic initial subduction of the Bangong‐Nujiang Ocean beneath Qiangtang revealed:Stratigraphic and geochronological evidence from Gaize,Tibet.Basin Research,28(1):147-157
Zeng M,Chen JP and Wei CC.2017.The Mugagangri Group is an accretionary complex accreted onto the south margin of Qiangtang.Earth Science Frontiers,24(5):207-217(in Chinese with English abstract)
Zeng YC,Chen JL,Xu JF,Wang BD and Huang F.2016b.Sediment melting during subduction initiation:Geochronological and geochemical evidence from the Darutso high-Mg andesites within ophiolite melange,Central Tibet.Geochemistry,Geophysics,Geosystems,17(12):4859-4877
Zeng YC,Xu JF,Chen JL,Wang BD,Kang ZQ and Huang F.2018.Geochronological and geochemical constraints on the origin of the Yunzhug ophiolite in the Shiquanhe-Yunzhug-Namu Tso ophiolite belt,Lhasa Terrane,Tibetan Plateau.Lithos,300-301:250-260
Zhang KJ,Zhang YX,Tang XC and Xia B.2012.Late Mesozoic tectonic evolution and growth of the Tibetan Plateau prior to the Indo-Asian collision.Earth-Science Reviews,114(3-4):236-249
Zhang KJ,Xia B,Zhang YX,Liu WL,Zeng L,Li JF and Xu LF.2014.Central Tibetan Meso-Tethyan oceanic plateau.Lithos,210-211:278-288
Zhang RS and Zeng M.2018.Mapping lithologic components of ophiolitic mélanges based on ASTER spectral analysis:A case study from the Bangong-Nujiang Suture Zone(Tibet,China).ISPRS International Journal of Geo-Information,7(1):34
Zhang YX.2007.Tectonic evolution of the middle-western BangongNujiang suture,Tibet.Ph.D.Dissertation.Guangzhou:Guangzhou Institute of Geochemistry,Chinese Academy of Sciences(in Chinese with English summary)
Zhao JH and Zhou MF.2009.Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block,South China.Lithos,107(3-4):152-168
Zhao ZD,Liu D,Wang Q,Zhu DC,Dong GC,Zhou S and Mo XX.2018.Zircon trace elements and their use in probing deep processes.Earth Science Frontiers,25(6):124-135(in Chinese with English abstract)
Zheng YY,Xu RK,Ma GT,Gao SB,Zhang GY,Ma XM and Ci Q.2006.Ages of generation and subduction of Shiquan river ophiolite:Restriction from SHRIMP zircon dating.Acta Petrologica Sinica,22(4):895-904(in Chinese with English abstract)
Zhou MF,Zhao JH,Jiang CY,Gao JF,Wang W and Yang SH.2009.OIB-like,heterogeneous mantle sources of Permian basaltic magmatism in the western Tarim Basin,NW China:Implications for a possible Permian large igneous province.Lithos,113(3-4):583-594
Zhu DC,Pan GT,Mo XX,Wang LQ,Zhao ZD,Liao ZL,Geng QR and Dong GC.2006.Identification for the Mesozoic OIB-type basalts in Central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting.Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract)
Zhu DC,Mo XX,Pan GT,Zhao ZD,Dong GC,Shi YR,Liao ZL,Wang LQ and Zhou CY.2008.Petrogenesis of the earliest Early Cretaceous mafic rocks from the Cona area of the eastern Tethyan Himalaya in South Tibet:Interaction between the incubating Kerguelen plume and the eastern Greater India lithosphere?Lithos,100(1-4):147-173
Zhu DC,Zhao ZD,Niu Y,Dilek Y,Hou ZQ and Mo XX.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau.Gondwana Research,23(4):1429-1454
Zhu DC,Wang Q,Zhao ZD,Chung SL,Cawood PA,Niu Y,Liu SA,Wu FY and Mo XX.2015.Corrigendum:Magmatic record of IndiaAsia collision.Scientific Reports,5:17236
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
邓晋福,刘翠,冯艳芳,肖庆辉,苏尚国,赵国春,孔维琼,曹文燕.2010.高镁安山岩/闪长岩类(HMA)和镁安山岩/闪长岩类(MA):与洋俯冲作用相关的两类典型的火成岩类.中国地质,37(4):1112-1118
高晓英,郑永飞.2011.金红石Zr和锆石Ti含量地质温度计.岩石学报,27(2):417-432
蓝江波,徐义刚,杨启军,黄小龙.2007.高黎贡带~40Ma OIB型基性岩浆活动:消减特提斯洋片与印度板块断离的产物?岩石学报,23(6):1334-1346
李世民.2018.西藏班公湖-怒江特提斯洋的俯冲极性和过程:岩浆岩和碎屑锆石记录.博士学位论文.北京:中国地质大学
牛耀龄.2010.板内洋岛玄武岩(OIB)成因的一些基本概念和存在的问题.科学通报,55(2):103-114
唐功建,王强.2010.高镁安山岩及其地球动力学意义.岩石学报,26(8):2495-2512
夏瑛,朱弟成,赵志丹,王青,袁四化,陈越,莫宣学.2012.藏东南措美大火成岩省中OIB型镁铁质岩的全岩地球化学和锆石Hf同位素.岩石学报,28(5):1588-1602
徐义刚.2002.地幔柱构造、大火成岩省及其地质效应.地学前缘,9(4):341-353
杨帆,黄小龙,李洁.2018.华南长城岭晚白垩世斜斑玄武岩的岩浆作用过程与岩石成因制约.岩石学报,34(1):157-171
曾敏,陈建平,位冲冲.2017.木嘎岗日岩群是羌塘南缘的增生楔杂岩.地学前缘,24(5):207-217
张玉修.2007.班公湖-怒江缝合带中西段构造演化.博士学位论文.广州:中国科学院广州地球化学研究所
赵志丹,刘栋,王青,朱弟成,董国臣,周肃,莫宣学.2018.锆石微量元素及其揭示的深部过程.地学前缘,25(6):124-135
郑有业,许荣科,马国桃,高顺宝,张刚阳,马新民,茨邛.2006.锆石SHRIMP测年对狮泉河蛇绿岩形成和俯冲的时间约束.岩石学报,22(4):895-904
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境.地质学报,80(9):1312-1328
Aldanmaz E,Pearce JA,Thirlwall MF and Mitchell JG.2000.Petrogenetic evolution of Late Cenozoic,post-collision volcanism in western Anatolia,Turkey.Journal of Volcanology and Geothermal Research,102(1-2):67-95
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb.Chemical Geology,192(1-2):59-79
Bloomer SH and Hawkins JW.1987.Petrology and geochemistry of boninite series volcanic rocks from the Mariana trench.Contributions to Mineralogy and Petrology,97(3):361-377
Blundy J and Wood B.2003.Partitioning of trace elements between crystals and melts.Earth and Planetary Science Letters,210(3-4):383-397
Dai JG,Wang CS and Li YL.2012.Relicts of the Early Cretaceous seamounts in the central-western Yarlung Zangbo Suture Zone,southern Tibet.Journal of Asian Earth Sciences,53:25-37
Defant MJ,Jackson TE,Drummond MS,de Boer JZ,Bellon H,Feigenson MD,Maury RC and Stewart RH.1992.The geochemistry of young volcanism throughout western Panama and southeastern Costa Rica:An overview.Journal of the Geological Society,149(4):569-579
Deng JF,Liu C,Feng YF,Xiao QH,Su SG,Zhao GC,Kong WQ and Cao WY.2010.High magnesian andesitic/dioritic rocks(HMA)and magnesian andesitic/dioritic rocks(MA):Two igneous rock types related to oceanic subduction.Geology in China,37(4):1112-1118(in Chinese with English abstract)
Duggen S,Hoernle K,Van den Bogaard P,Rüpke L and Morgan JP.2003.Deep roots of the Messinian salinity crisis.Nature,422(6932):602-606
Faccenna C,Piromallo C,Crespo‐Blanc A,Jolivet L and Rossetti F.2004.Lateral slab deformation and the origin of the western Mediterranean arcs.Tectonics,23(1):TC1012
Faccenna C,Civetta L,D'Antonio M,Funiciello F,Margheriti L and Piromallo C.2005.Constraints on mantle circulation around the deforming Calabrian slab.Geophysical Research Letters,32(6):L06311
Faccenna C,Becker TW,Lallemand S,Lagabrielle Y,Funiciello F and Piromallo C.2010.Subduction-triggered magmatic pulses:A new class of plumes?Earth and Planetary Science Letters,299(1-2):54-68
Furukawa Y and Tatsumi Y.1999.Melting of a subducting slab and production of high-Mg andesite magmas:Unusual magmatism in SWJapan at 13~15Ma.Geophysical Research Letters,26(15):2271-2274
Girardeau J,Marcoux J,Fourcade E,Bassoullet JP and Youking T.1985.Xainxa ultramafic rocks,central Tibet,China:Tectonic environment and geodynamic significance.Geology,13(5):330
Gao S,Rudnick RL,Yuan HL,Liu XM,Liu YS,Xu WL,Ling WL,Ayers J,Wang XC and Wang QH.2004.Recycling lower continental crust in the North China craton.Nature,432(7019):892-897
Gao XY and Zheng YF.2011.On the Zr-in-rutile and Ti-in-zircon geothermometers.Acta Petrologica Sinica,27(2):417-432(in Chinese with English abstract)
Gehrels G,Kapp P,De Celles P,Pullen A,Blakey R,Weislogel A,Ding L,Guynn J,Martin A,Mc Quarrie N and Yin A.2011.Detrital zircon geochronology of pre-Tertiary strata in the Tibetan‐Himalayan orogen.Tectonics,30(5):TC5016
Gorring ML and Kay SM.2001.Mantle processes and sources of Neogene slab window magmas from Southern Patagonia,Argentina.Journal of Petrology,42(6):1067-1094
Green TH.1994.Experimental studies of trace-element partitioning applicable to igneous petrogenesis:Sedona 16 years later.Chemical Geology,117(1-4):1-36
Hanyu T,Tatsumi Y and Nakai S.2003.Evidence of slab melting for the formation of high-Mg andesite:A Hafnium isotope study of Setouchi volcanics,Japan.In:Geophysical Research Abstracts,Vol.5.Washington:EGS
Hanyu T,Tatsumi Y,Nakai S,Chang Q,Miyazaki T,Sato K,Tani K,Shibata T and Yoshida T.2006.Contribution of slab melting and slab dehydration to magmatism in the Japanese arc.Geochimica et Cosmochimica Acta,70(S18):A229
Hermann J and Rubatto D.2009.Accessory phase control on the trace element signature of sediment melts in subduction zones.Chemical Geology,265(3-4):512-526
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Hoskin PWO and Ireland TR.2000.Rare earth element chemistry of zircon and its use as a provenance indicator.Geology,28(7):627
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hoskin PWO.2005.Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills,Australia.Geochimica et Cosmochimica Acta,69(3):637-648
Hu J,Li Q,Fang NQ,Yang JY and Ge DS.2015.Geochemistry characteristics of the Low Permian sedimentary rocks from central uplift zone,Qiangtang Basin,Tibet:Insights into source-area weathering,provenance,recycling,and tectonic setting.Arabian Journal of Geosciences,8(8):5373-5388
Huang TT,Xu JF,Chen JL,Wu JB and Zeng YC.2017.Sedimentary record of Jurassic northward subduction of the Bangong-Nujiang Ocean:Insights from detrital zircons.International Geology Review,59(2):166-184
Huang XL,Niu YL,Xu YG,Ma JL,Qiu HN and Niu JW.2013.Geochronology and geochemistry of Cenozoic basalts from eastern Guangdong,SE China:Constraints on the lithosphere evolution beneath the northern margin of the South China Sea.Contributions to Mineralogy and Petrology,165(3):437-455
Johnson MC and Plank T.2000.Dehydration and melting experiments constrain the fate of subducted sediments.Geochemistry,Geophysics,Geosystems,1(12):1007
Kamei A,Owada M,Nagao T and Shiraki K.2004.High-Mg diorites derived from sanukitic HMA magmas,Kyushu Island,Southwest Japan arc:Evidence from clinopyroxene and whole rock compositions.Lithos,75(3-4):359-371
Kapp P,Murphy MA,Yin A,Harrison TM,Ding L and Guo JH.2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet.Tectonics,22(4):1029
Kapp P,Yin A,Harrison TM and Ding L.2005.Cretaceous-Tertiary shortening,basin development,and volcanism in central Tibet.Geological Society of America Bulletin,117(7-8):865-878
Kapp P,Decelles 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.Geological Society of America Bulletin,119(7-8):917-933
Kay RW.1978.Aleutian magnesian andesites:Melts from subducted Pacific Ocean crust.Journal of Volcanology and Geothermal Research,4(1-2):117-132
Kepezhinskas P,Defant MJ and Drummond MS.1996.Progressive enrichment of island arc mantle by melt-peridotite interaction inferred from Kamchatka xenoliths.Geochimica et Cosmochimica Acta,60(7):1217-1229
Labanieh S,Chauvel C,Germa A and Quidelleur X.2018.Martinique:A clear case for sediment melting and slab dehydration as a function of distance to the trench.Journal of Petrology,53(12):2441-2464
Lan JB,Xu YG,Yang QJ and Huang XL.2007.~40Ma OIB-type mafic magmatism in the Gaoligong belt:Results of break-off between subducting Tethyan slab and Indian Plate?Acta Petrologica Sinica,23(6):1334-1346(in Chinese with English abstract)
Li JX,Qin KZ,Li GM,Richards JP,Zhao JX and Cao MJ.2014a.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 SM,Zhu DC,Wang Q,Zhao ZD,Sui QL,Liu SA,Liu D and Mo XX.2014b.Northward subduction of Bangong-Nujiang Tethys:Insight from Late Jurassic intrusive rocks from Bangong Tso in western Tibet.Lithos,205:284-297
Li SM,Zhu DC,Wang Q,Zhao ZD,Zhang LL,Liu SA,Chang QS,Lu YH,Dai JG and Zheng YC.2016.Slab-derived adakites and subslab asthenosphere-derived OIB-type rocks at 156±2Ma from the north of Gerze,central Tibet:Records of the Bangong-Nujiang oceanic ridge subduction during the Late Jurassic.Lithos,262:456-469
Li SM.2018.Subduction polarity and processes of the Bangong-Nujiang Tethys:Insights from igneous rocks and detrial zircons.Ph.D.Dissertation.Beijing:China University of Geosciences(in Chinese with English summary)
Lin B,Chen YC,Tang JX,Wang Q,Song Y,Yang C,Wang WL,He W and Zhang LJ.2017.40Ar/39Ar and Rb-Sr ages of the Tiegelongnan porphyry Cu-(Au)deposit in the Bangong Co-Nujiang Metallogenic Belt of Tibet,China:Implication for generation of super-Large deposit.Acta Geologica Sinica,91(2):602-616
Liu B,Ma CQ,Guo P,Sun Y,Gao K and Guo YH.2016.Evaluation of late Permian mafic magmatism in the central Tibetan Plateau as a response to plume-subduction interaction.Lithos,264:1-16
Liu DL,Huang QS,Fan SQ,Zhang LY,Shi RD and Ding L.2014.Subduction of the Bangong-Nujiang Ocean:Constraints from granites in the Bangong Co area,Tibet.Geological Journal,49(2):188-206
Liu WL,Huang QT,Gu M,Zhong Y,Zhou RJ,Gu XD,Zheng H,Liu JN,Lu XX and Xia B.2018.Origin and tectonic implications of the Shiquanhe high-Mg andesite,western Bangong suture,Tibet.Gondwana Research,60:1-14
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
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig KR.2003.User’s manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,Berkeley,CA:Berkeley Geochronology Center,4:1-70
Martin H.1999.Adakitic magmas:Modern analogues of Archaean granitoids.Lithos,46(3):411-429
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Ydiagram.Chemical Geology,56(3-4):207-218
Miyashiro A.1974.Volcanic rock series in island arcs and active continental margins.American Journal of Science,274(4):321-355
Nebel O,Vroon PZ,van Westrenen W,Iizuka T and Davies GR.2011.The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust,Banda arc,Indonesia.Earth and Planetary Science Letters,303(3-4):240-250
Niu YL.2009.Some basic concepts and problems on the petrogenesis of Intra-Plate Ocean Island basalts.Chinese Science Bulletin,54(22):4148-4160
Niu YL,Wilson M,Humphreys ER and O'Hara MJ.2011.The origin of intra-plate ocean Island Basalts(OIB):The lid effect and its geodynamic implications.Journal of Petrology,52(7-8):1443-1468
Pearce JA and Cann JR.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth and Planetary Science Letters,19(2):290-300
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb variations in volcanic rocks.Contributions to Mineralogy and Petrology,69(1):33-47
Pearce JA and Deng W.1988.The Ophiolites of the Tibetan Geotraverses,Lhasa to Golmud(1985)and Lhasa to Kathmandu(1986).Philosophical Transactions of the Royal Society of London,327(1594):215-238
Pearce JA,van der Laan SR,Arculus RJ,Murton BJ,Ishii T,Peate DWand Parkinson IJ.1992.Boninite and harzburgite from Leg 125(Bonin-Mariana forearc):A case study of magma genesis during the initial stages of subduction.Proceedings of the Ocean Drilling Program,Scientific Results,125:623-659
Plank T and Langmuir CH.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle.Chemical Geology,145(3-4):325-394
Qian Q and Hermann J.2010.Formation of High-Mg diorites through assimilation of peridotite by monzodiorite magma at crustal depths.Journal of Petrology,51(7):1381-1416
Reagan MK and Gill JB.1989.Coexisting calcalkaline and high-niobium basalts from Turrialba Volcano,Costa Rica:Implications for residual titanates in arc magma sources.Journal of Geophysical Research:Solid Earth,94(B4):4619-4633
Reagan MK,Ishizuka O,Stern RJ,Kelley KA,Ohara Y,Blichert-Toft J,Bloomer SH,Cash J,Fryer P,Hanan BB,Hickey-Vargas R,Ishii T,Kimura JI,Peate DW,Rowe MC and Woods M.2013.Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system.Geochemistry,Geophysics,Geosystems,11(3):Q03X12
Rogers G,Saunders AD,Terrell DJ,Verma SP and Marriner GF.1985.Geochemistry of Holocene volcanic rocks associated with ridge subduction in Baja California,Mexico.Nature,315(6018):389-392
Rollinson HR.1993.Using Geochemical Data:Evaluation,Presentation,Interpretation.Longman Scientific&Technical,Longman Group UK Ltd.,1-352
Rudnick RL and Fountain DM.1995.Nature and composition of the continental crust:A lower crustal perspective.Reviews of Geophysics,33(3):267-310
Sajona FG,Maury RC,Bellon H,Cotton J and Defant M.1996.High field strength element enrichment of Pliocene-Pleistocene island arc basalts,Zamboanga Peninsula,Western Mindanao(Philippines).Journal of Petrology,37(3):693-726
Shimoda G,Tatsumi Y,Nohda S,Ishizaka K and Jahn BM.1998.Setouchi high-Mg andesites revisited:Geochemical evidence for melting of subducting sediments.Earth and Planetary Science Letters,160(3-4):479-492
Sisson TW.1994.Hornblende-melt trace-element partitioning measured by ion microprobe.Chemical Geology,117(1-4):331-344
Skora S and Blundy J.2010.High-pressure hydrous phase relations of radiolarian clay and implications for the involvement of subducted sediment in arc magmatism.Journal of Petrology,51(11):2211-2243
Smithies RH and Champion DC.2000.The Archaean High-Mg diorite suite:Links to tonalite-trondhjemite-granodiorite magmatism and implications for Early Archaean crustal growth.Journal of Petrology,41(12):1653-1671
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
Spandler C,Hermann J,Faure K,Mavrogenes JA and Arculus RJ.2008.The importance of talc and chlorite“hybrid”rocks for volatile recycling through subduction zones:Evidence from the high-pressure subduction mélange of New Caledonia.Contributions to Mineralogy and Petrology,155(2):181-198
Stern RA and Hanson GN.1991.Archean High-Mg granodiorite:Aderivative of light rare earth element-enriched monzodiorite of mantle origin.Journal of Petrology,32(1):201-238
Stern RJ.2002.Subduction zones.Reviews of Geophysics,40(4):1012
Stern RJ and Gerya T.2018.Subduction initiation in nature and models:A review.Tectonophysics,746:173-198
Straub SM,Gomez-Tuena A,Stuart FM,Zellmer GF,Espinasa-Perena R,Cai Y and Iizuka Y.2011.Formation of hybrid arc andesites beneath thick continental crust.Earth and Planetary Science Letters,303(3-4):337-347
Sun SS and Mcdonough 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 Publications,42(1):313-345
Tang GJ and Wang Q.2010.High-Mg andesites and their geodynamic implications.Acta Petrologica Sinica,26(8):2495-2512(in Chinese with English abstract)
Tang GJ,Wang Q,Wyman DA,Li ZX,Zhao ZH and Jia XH.2010.Ridge subduction and crustal growth in the Central Asian Orogenic Belt:Evidence from Late Carboniferous adakites and high-Mg diorites in the western Junggar region,northern Xinjiang(West China).Chemical Geology,277(3):281-300
Tang GJ,Wyman DA,Wang Q,Li J,Li ZX,Zhao ZH and Sun WD.2012.Asthenosphere-lithosphere interaction triggered by a slab window during ridge subduction:Trace element and Sr-Nd-Hf-Os isotopic evidence from Late Carboniferous tholeiites in the western Junggar area(NW China).Earth and Planetary Science Letters,329-330:84-96
Tatsumi Y and Hanyu T.2003.Geochemical modeling of dehydration and partial melting of subducting lithosphere:Toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt,SW Japan.Geochemistry,Geophysics,Geosystems,4(9):1081
Tatsumi Y.2006.High-Mg andesites in the Setouchi volcanic belt,southwestern Japan:Analogy to Archean Magmatism and Continental Crust Formation?Annual Review of Earth&Planetary Science,34(1):467-499
Thorkelson DJ,Madsen JK and Sluggett CL.2011.Mantle flow through the Northern Cordilleran slab window revealed by volcanic geochemistry.Geology,39(3):267-270
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 Q,Wyman DA,Xu JF,Wan YS,Li C,Zi F,Jiang ZQ,Qiu HN,Chu ZY,Zhao ZH and Dong YH.2008.Triassic Nb-enriched basalts,magnesian andesites,and adakites of the Qiangtang terrane(Central Tibet):Evidence for metasomatism by slab-derived melts in the mantle wedge.Contributions to Mineralogy and Petrology,155(4):473-490
Wang Q,Li ZX,Chung SL,Wyman DA,Sun YL,Zhao ZH,Zhu YTand Qiu HN.2011.Late Triassic high-Mg andesite/dacite suites from northern Hohxil,North Tibet:Geochronology,geochemical characteristics,petrogenetic processes and tectonic implications.Lithos,126(1-2):54-67
Watson EB and Harrison TM.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types.Earth and Planetary Science Letters,64(2):295-304
Weinberg RF and HasalováP.2015.Water-fluxed melting of the continental crust:A review.Lithos,212-215:158-188
Wilson BM.2007.Igneous Petrogenesis A Global Tectonic Approach.Netherlands:Springer Science&Business Media
Wilson M.1989.Igneous Petrogenesis:A Global Tectonic Approach.London:Unwin Hyman
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Wood BJ and Turner SP.2009.Origin of primitive high-Mg andesite:Constraints from natural examples and experiments.Earth and Planetary Science Letters,283(1-4):59-66
Xia Y,Zhu DC,Zhao ZD,Wang Q,Yuan SH,Chen Y and Mo XX.2012.Whole-rock geochemistry and zircon Hf isotope of the OIB-type mafic rocks from the Comei Large Igneous Province in southeastern Tibet.Acta Petrologica Sinica,28(5):1588-1602(in Chinese with English abstract)
Xu JF,Shinjo R,Defant MJ,Wang Q and Rapp RP.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:Partial melting of delaminated lower continental crust?Geology,30(12):1111-1114
Xu MJ,Li C,Zhang XZ and Wu YW.2014.Nature and evolution of the Neo-Tethys in central Tibet:Synthesis of ophiolitic petrology,geochemistry,and geochronology.International Geology Review,56(9):1072-1096
Xu YG,Chung SL,Jahn BM and Wu GY.2001.Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China.Lithos,58(3-4):145-168
Xu YG.2002.Mantle plumes,large igneous provinces and their geologic consequences.Earth Science Frontiers,9(4):341-353(in Chinese with English abstract)
Yang F,Huang XL and Li J.2018.Magma processes and petrogenesis of the Late Cretaceous plagioclase-phyric basalt in the Changchengling area,South China.Acta Petrologica Sinica,34(1):157-171(in Chinese with English abstract)
Yin A and Harrison TM.2000.Geologic evolution of the HimalayanTibetan Orogen.Annual Review of Earth and Planetary Sciences,28:211-280
Yogodzinski MG,Kay RW,Volynets ON,Koloskov AV and Kay SM.1995.Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge.GSA Bulletin,107(5):505-519
Zeng M,Zhang X,Cao H,Ettensohn FR,Cheng WB and Lang XH.2016a.Late Triassic initial subduction of the Bangong‐Nujiang Ocean beneath Qiangtang revealed:Stratigraphic and geochronological evidence from Gaize,Tibet.Basin Research,28(1):147-157
Zeng M,Chen JP and Wei CC.2017.The Mugagangri Group is an accretionary complex accreted onto the south margin of Qiangtang.Earth Science Frontiers,24(5):207-217(in Chinese with English abstract)
Zeng YC,Chen JL,Xu JF,Wang BD and Huang F.2016b.Sediment melting during subduction initiation:Geochronological and geochemical evidence from the Darutso high-Mg andesites within ophiolite melange,Central Tibet.Geochemistry,Geophysics,Geosystems,17(12):4859-4877
Zeng YC,Xu JF,Chen JL,Wang BD,Kang ZQ and Huang F.2018.Geochronological and geochemical constraints on the origin of the Yunzhug ophiolite in the Shiquanhe-Yunzhug-Namu Tso ophiolite belt,Lhasa Terrane,Tibetan Plateau.Lithos,300-301:250-260
Zhang KJ,Zhang YX,Tang XC and Xia B.2012.Late Mesozoic tectonic evolution and growth of the Tibetan Plateau prior to the Indo-Asian collision.Earth-Science Reviews,114(3-4):236-249
Zhang KJ,Xia B,Zhang YX,Liu WL,Zeng L,Li JF and Xu LF.2014.Central Tibetan Meso-Tethyan oceanic plateau.Lithos,210-211:278-288
Zhang RS and Zeng M.2018.Mapping lithologic components of ophiolitic mélanges based on ASTER spectral analysis:A case study from the Bangong-Nujiang Suture Zone(Tibet,China).ISPRS International Journal of Geo-Information,7(1):34
Zhang YX.2007.Tectonic evolution of the middle-western BangongNujiang suture,Tibet.Ph.D.Dissertation.Guangzhou:Guangzhou Institute of Geochemistry,Chinese Academy of Sciences(in Chinese with English summary)
Zhao JH and Zhou MF.2009.Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block,South China.Lithos,107(3-4):152-168
Zhao ZD,Liu D,Wang Q,Zhu DC,Dong GC,Zhou S and Mo XX.2018.Zircon trace elements and their use in probing deep processes.Earth Science Frontiers,25(6):124-135(in Chinese with English abstract)
Zheng YY,Xu RK,Ma GT,Gao SB,Zhang GY,Ma XM and Ci Q.2006.Ages of generation and subduction of Shiquan river ophiolite:Restriction from SHRIMP zircon dating.Acta Petrologica Sinica,22(4):895-904(in Chinese with English abstract)
Zhou MF,Zhao JH,Jiang CY,Gao JF,Wang W and Yang SH.2009.OIB-like,heterogeneous mantle sources of Permian basaltic magmatism in the western Tarim Basin,NW China:Implications for a possible Permian large igneous province.Lithos,113(3-4):583-594
Zhu DC,Pan GT,Mo XX,Wang LQ,Zhao ZD,Liao ZL,Geng QR and Dong GC.2006.Identification for the Mesozoic OIB-type basalts in Central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting.Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract)
Zhu DC,Mo XX,Pan GT,Zhao ZD,Dong GC,Shi YR,Liao ZL,Wang LQ and Zhou CY.2008.Petrogenesis of the earliest Early Cretaceous mafic rocks from the Cona area of the eastern Tethyan Himalaya in South Tibet:Interaction between the incubating Kerguelen plume and the eastern Greater India lithosphere?Lithos,100(1-4):147-173
Zhu DC,Zhao ZD,Niu Y,Dilek Y,Hou ZQ and Mo XX.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau.Gondwana Research,23(4):1429-1454
Zhu DC,Wang Q,Zhao ZD,Chung SL,Cawood PA,Niu Y,Liu SA,Wu FY and Mo XX.2015.Corrigendum:Magmatic record of IndiaAsia collision.Scientific Reports,5:17236
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
邓晋福,刘翠,冯艳芳,肖庆辉,苏尚国,赵国春,孔维琼,曹文燕.2010.高镁安山岩/闪长岩类(HMA)和镁安山岩/闪长岩类(MA):与洋俯冲作用相关的两类典型的火成岩类.中国地质,37(4):1112-1118
高晓英,郑永飞.2011.金红石Zr和锆石Ti含量地质温度计.岩石学报,27(2):417-432
蓝江波,徐义刚,杨启军,黄小龙.2007.高黎贡带~40Ma OIB型基性岩浆活动:消减特提斯洋片与印度板块断离的产物?岩石学报,23(6):1334-1346
李世民.2018.西藏班公湖-怒江特提斯洋的俯冲极性和过程:岩浆岩和碎屑锆石记录.博士学位论文.北京:中国地质大学
牛耀龄.2010.板内洋岛玄武岩(OIB)成因的一些基本概念和存在的问题.科学通报,55(2):103-114
唐功建,王强.2010.高镁安山岩及其地球动力学意义.岩石学报,26(8):2495-2512
夏瑛,朱弟成,赵志丹,王青,袁四化,陈越,莫宣学.2012.藏东南措美大火成岩省中OIB型镁铁质岩的全岩地球化学和锆石Hf同位素.岩石学报,28(5):1588-1602
徐义刚.2002.地幔柱构造、大火成岩省及其地质效应.地学前缘,9(4):341-353
杨帆,黄小龙,李洁.2018.华南长城岭晚白垩世斜斑玄武岩的岩浆作用过程与岩石成因制约.岩石学报,34(1):157-171
曾敏,陈建平,位冲冲.2017.木嘎岗日岩群是羌塘南缘的增生楔杂岩.地学前缘,24(5):207-217
张玉修.2007.班公湖-怒江缝合带中西段构造演化.博士学位论文.广州:中国科学院广州地球化学研究所
赵志丹,刘栋,王青,朱弟成,董国臣,周肃,莫宣学.2018.锆石微量元素及其揭示的深部过程.地学前缘,25(6):124-135
郑有业,许荣科,马国桃,高顺宝,张刚阳,马新民,茨邛.2006.锆石SHRIMP测年对狮泉河蛇绿岩形成和俯冲的时间约束.岩石学报,22(4):895-904
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境.地质学报,80(9):1312-1328
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