Citation: | LIU Haiyong, ZENG Qinggao, WANG Yu, MAO Guozheng. Petrology, zircon U-Pb age and geochemical characteristics of the Lhaguo Tso ophiolitic melange in Tibet[J]. Geological Bulletin of China, 2020, 39(2-3): 164-176. |
Lhaguo Tso ophiolite is one of the most complete ophiolite combinations in the Shiquanhe-Namco-Lhari suture zone in central Tibetan Plateau, and has great significance for restoring the evolution of ocean.This paper reports petrology, zircon U-Pb chronology and geochemical characteristics of the diabases and plagiogranites to confirm the genesis and tectonic setting of Lhaguo Tso ophiolites.The zircon U-Pb dating of plagiogranite yielded an age of 167.8±1.7 Ma (n=24, MSWD=0.22), which indicates that the Lhaguo Tso ophiolite was formed in Late Jurassic.Geochemically, the gabbros and the diabases are similar to the island arc rocks and E-MORB, suggesting a continental back-arc basin environment setting.
[1] | Dewey J F, Bird J M.Origin and Emplacement of the Ophiolite Suite:Appalachian Ophiolites in Newfoundland[J].Journal of Geophysical Research, 1971, 76:3179-3206. |
[2] | Nicolas A.Structures of Ophiolites and Dynamics of Oceanic Lithosphere[M].Kluwer Academic Publishers, 1989. |
[3] | Dilek Y, Flower M F J.Arc-trench rollback and forearc accretion:2.A model template for ophiolites in Albania, Cyprus, and Oman[J].Geological Society London Special Publications, 2003, 218:43-68. |
[4] | Dilek Y, Furnes H.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J].Geological Society of America Bulletin, 2011, 123:387-411. |
[5] | Lister G, Forster M.Tectonic mode switches and the nature of orogenesis[J].Lithos, 2009, 113:274-291. |
[6] | Xu M, Li C, Zhang X, et al.Nature and evolution of the Neo-Tethys in central Tibet:synthesis of ophiolitic petrology, geochemistry, and geochronology[J].International Geology Review, 2014, 56(9):1072-1096. |
[7] | Zhu D C, Zhao Z D, Niu Y, et al.The origin and pre-Cenozoic evolution of the Tibetan Plateau[J].Gondwana Research, 2013, 23:1429-1454. |
[8] | 西藏自治区地质调查院.1/25万改则县幅区域地质调查报告[M].北京:地质出版社, 2012. |
[9] | 张玉修, 张开均, 黎兵, 等.西藏改则南拉果错蛇绿岩中斜长花岗岩锆石SHRIMP U-Pb年代学及其成因研究[J].科学通报, 2007, 52(1):100-106. |
[10] | 樊帅权, 史仁灯, 丁林, 等.西藏改则蛇绿岩中斜长花岗岩地球化学特征、锆石U-Pb年龄及构造意义[J].岩石矿物学杂志, 2010, 29(5):467-478. |
[11] | 西藏自治区地质矿产局.西藏自治区区域地质志[M].北京:地质出版社, 1993. |
[12] | 王保弟, 许继峰, 曾庆高, 等.西藏改则地区拉果错蛇绿岩地球化学特征及成因[J].岩石学报, 2007, 23(6):1521-1530. |
[13] | Liu Y S, Hu Z C, Gao S, et al.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J].Chemical Geology, 2008, 257:34-43. |
[14] | Winchester J A, Floyd P A.Geochemical discrimination of different magma series and their differentiation products using immobile elements[J].Chemical Geology, 1977, 20:325-343. |
[15] | Miyashiro A.Volcanic rock series in island arcs and active continental margins[J].American Journal of Science, 1974, 274(4):321-355. |
[16] | Boynton W V.Geochemistry of the rare earth elements: Meteorite studies[C]//Henderson P.Rare Earth Elements Geochemistry, Elsevier, Amsterdam, 1984: 63-114. |
[17] | Sun W D, McDonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J].Geological Society, London, Special Publications, 1989, 42(1):313-345. |
[18] | Yuan Y J, Yin Z X, Liu W L, et al.Tectonic Evolution of the Meso·Tethys in the Western Segment of Bangonghu-Nujiang Suture Zone:Insights from Geochemistry and Geochronology of the Lagkor Tso Ophiolite[J].Acta Geologica Sinica(English Edition), 2015, 89(2):369-388. |
[19] | Pearce J A, Stern R J.Origin of back-arc basin magmas:Trace element and isotope perspectives, Back-arc spreading systems:Geological, Biological, Chemical, and Physical Interactions[M].Washington, DC, AGU, 2006:63-86. |
[20] | Fretzdorff S, Livermore R A, Devey C W, et al.Petrogenesis of the Back-arc East Scotia Ridge, South Atlantic Ocean[J].Journal of Petrology, 2002, 43:1435-1467. |
[21] | Hawkins J W.Geology of supra-subduction zones: Implications for the origin of ophiolites[C]//Dilek Y, Newcomb S.Ophiolite concept and the evolution of geological thought, 2003. |
[22] | Sinton J M, Ford L L, Chappell B, et al.Magma Genesis and Mantle Heterogeneity in the Manus Back-Arc Basin, Papua New Guinea[J].Journal of Petrology, 2003, 44:159-195. |
[23] | Pearce J A, Cann J R.Tectonic Setting of Basic Volcanic Rocks determined using Trace Element Analyse[J].Earth & Planetary Science Letters, 1973, 19(2):290-300. |
[24] | Stolper E, Newman S.The role of water in the petrogenesis of Mariana trough magmas[J].Earth & Planetary Science Letters, 1994, 121:293-325. |
[25] | Pearce J A, Peate D W.Tectonic Implications of the Composition of Volcanic ARC Magmas[J].Annual Review of Earth & Planetary Sciences, 1995, 23:251-285. |
[26] | Geng H, Sun M, Yuan C, et al.Geochemical and geochronological study of early Carboniferous volcanic rocks from the West Junggar:Petrogenesis and tectonic implications[J].Journal of Asian Earth Sciences, 2011, 42:854-866. |
[27] | Jung C, Jung S, Hoffer E, et al.Petrogenesis of Tertiary Mafic Alkaline Magmas in the Hocheifel, Germany[J].Journal of Petrology, 2006, 47:1637-1671. |
[28] | Zhao J H, Zhou M F.Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district(Sichuan Province, SW China):Implications for subduction-related metasomatism in the upper mantle[J].Precambrian Research, 2007, 152:27-47. |
[29] | Aldanmaz E, Pearce J A, Thirlwall M F, et al.Petrogenetic evolution of late Cenozoic, post-collision volcanism in western Anatolia, Turkey[J].Journal of Volcanology & Geothermal Research, 2000, 102:67-95. |
[30] | Brophy J G.La-SiO2 and Yb-SiO2 systematics in mid-ocean ridge magmas:implications for the origin of oceanic plagiogranite[J].Contrib. Mineral. Petrol., 2009, 158:99-111. |
[31] | Frey F A, Green D H, Roy S D.Integrated models of basalt petrogenesis:a study of quartz tholeiites to olivine melilitites from South Eastern Australia utilizing geochemical and experimental petrological data[J].Journal of Petrology, 1978, 19:463-513. |
[32] | Hess P C.Phase equilibria constraints on the origin of ocean floor basalts[C]//Morgan J P, Blackman D K, Sinton J M.Mantle Flow and Melt Generation at Mid-Ocean Ridges.Geophysical Monograph 71, American Geophysical Union.1992: 67-102. |
[33] | Wilson M.Igneous Petrogenesis[M].London:Unwin Hyman, 1989:1-466. |
[34] | Jung S, Mesberg P.Major and trace-element systematics and isotope geochemistry of Cenozoic mafic volcanic rocks from the Vogelsberg(central Germany)Constraints on the origin of continental alkaline and tholeiitic basalts and their mantle sources[J].Journal of Volcanology and Geothermal Research, 1998, 86:151-177. |
[35] | 徐建鑫.西藏改则县拉果错蛇绿岩的构造属性[D].吉林大学博士学位论文, 2015. |
[36] | Cabanis B, Lecolle M.Le diagramme La/10-Y/15-Nb/8:Un outil pour la discrimination des series volcaniques et la mise en evidence des processus de mélange et/ou de contamination crustale[J].Comptes Rendus de l'Academie des Sciences Series Ⅱ, 1989, 309:2023-2029. |
[37] | Shervais J W.Ti-V plots and the petrogenesis of modern and ophiolitic lavas[J].Earth & Planetary Science Letters, 1982, 59(1)101-118. |
[38] | Metzger E P, Miller R B, Harper G D.Geochemistry and Tectonic Setting of the Ophiolitic Ingalls Complex, North Cascades, Washington:Implications for Correlations of Jurassic Cordilleran Ophiolites[J].The Journal of Geology, 2002, 110(5):543-560. |
[39] | Gribble R F, Stern R J, Bloomer S H, et al.MORB mantle and subduction components interact to generate basalts in the southern Mariana Trough back-arc basin[J].Geochimica Et Cosmochimica Acta, 1996, 60(12):2153-2166. |
[40] | Shinjo R, Chung S L, Kato Y, et al.Geochemical and Sr-Nd isotopic characteristics of volcanic rocks from the Okinawa Trough and Ryukyu Arc:Implications for the evolution of a young, intracontinental back arc basin[J].Journal of Geophysical Research Solid Earth, 1999, 104(B5):10591-10608. |
[41] | Xu J F, Castillo P R, Chen F R, et al.Geochemistry of late Paleozoic mafic igneous rocks from the Kuerti area, Xinjiang, northwest China:implications for backarc mantle evolution[J].Chemical Geology, 2003, 193:137-154. |
[42] | Ghazi J M, Moazzen M, Rahgoshay M, et al.Geochemical characteristics of basaltic rocks from the Nain ophiolite(Central Iran); constraints on mantle wedge source evolution in an oceanic back arc basin and a geodynamical model[J].Tectonophysics, 2012, 574/575:92-104. |
Simplified geological map of Lhaguo Tso area, central Tibet
Nb/Yb-Zr/TiO2*0.0001 diagram(a)and SiO2-TFeO/MgO diagram(b)
Chondrite-normalized REE patterns(a, c)and primitive mantle-normalized trace element diagrams(b, d)
Or-Ab-An diagram(a)and SiO2-K2O diagram(b)
CL images, U-Pb concordia plots(a)and age distribution for zircons(b)
Zr-Nb diagram(a)and Dy/Yb-La/Yb diagram(b)
Cr-Ni diagram
Ti/1000-V diagram(a)and triangular Y/15-La/10-Nb/8 diagram(b)