2016 Vol. 35, No. 6
Article Contents

YANG Shuo, XIANG Shuyuan, ZHANG Xian, LI Zhixuan, LIU Zhenhe. LA-ICP-MS zircon U-Pb age and geochemical characteristics of Jiada potas-sic volcanic rocks in Zhongba terrane, Tibet[J]. Geological Bulletin of China, 2016, 35(6): 894-905.
Citation: YANG Shuo, XIANG Shuyuan, ZHANG Xian, LI Zhixuan, LIU Zhenhe. LA-ICP-MS zircon U-Pb age and geochemical characteristics of Jiada potas-sic volcanic rocks in Zhongba terrane, Tibet[J]. Geological Bulletin of China, 2016, 35(6): 894-905.

LA-ICP-MS zircon U-Pb age and geochemical characteristics of Jiada potas-sic volcanic rocks in Zhongba terrane, Tibet

  • Cenozoic potassic volcanic rocks are widely distributed in the Tibetan Plateau, mainly in northern Tibet and Lhasa block with a few reports in Zhongba terrane. The study of Jiada potassic volcanic rocks found in Zhongba terrane shows that the rocks are almost exclusively trachyte, and the magma erupted incessantly by overflowing and erupting. These rocks are also characterized by high potassium and high aluminum, rich LILE, LREE and Sr, and poor HFSE,Y and Yb, with Eu negative anomaly. Their geochemi-cal characteristicss are similar to those of typical adkite rocks. The LA-ICP-MS zircon U-Pb age of trachyandesites is 17.03±0.32Ma, which means that these volcanic rocks were formed in Miocene. The Jiada potassic magma was derived from partial melting of thickened crust. The rocks represent post-collisional tectonic setting and extension environment.
  • 加载中
  • [1] Turner S, Amaud N, Liu J, et al. Post-collision, shoshonitic volca-nism on the Tibetan Plateau:Implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Journal of Petrology, 1996, 37:45-71.

    Google Scholar

    [2] Chung S L, Liu D Y, Ji J Q, et al. Adakites from continental colli-sion zones:Melting of thickened lower crust beneanth southern Ti-bet[J]. Geology, 2003, 31:1021-1024.

    Google Scholar

    [3] Zhao Z D, Mo X X, Dilek Y, et al. Geochemical and Sr-Nd-Pb-O isotopic compositions of the post-collisional ultrapotassic mag-maatism in S W Tibet:Petrogenesis and implication for India intracontinental subduction beneath southern Tibet[J]. Lithos, 2009, 113:190-212.

    Google Scholar

    [4] 谭建政. 藏北布若错地区新生代火山岩及其成因探讨[J]. 桂林理工大学学报, 2013, 33(3):383-393.

    Google Scholar

    [5] 陈建林, 许继峰, 康志强, 等. 青藏高原西部措勤县中新世布嘎寺组钾质火山岩成因[J]. 岩石学报, 2006, 22(3):585-595.

    Google Scholar

    [6] 胡文洁, 田世洪, 杨竹森, 等. 拉萨地块西段中新世查加寺钾质火山岩岩石成因——岩石地球化学、年代学和Sr-Nd同位素约束[J]. 矿床地质, 2012, 31(4):813-830.

    Google Scholar

    [7] Lai S C, Liu C Y, Yi H S. Geochemistry and petrogenesis of Cenzo-ic and esite-dacite association from the Hoh Xil Region, Tibetan Plateau[J]. International Geology Reviews, 2003, 45(11):998-1019.

    Google Scholar

    [8] 刘栋, 赵志丹, 朱第成, 等. 青藏高原拉萨地块西部雄巴盆地后碰撞钾质-超钾质火山岩年代学与地球化学[J]. 岩石学报, 2011, 27(7):2045-2059.

    Google Scholar

    [9] 李才, 朱志勇, 迟效国. 藏北改则地区鱼鳞山组火山岩同位素年代学[J]. 地质通报, 2002, 21(11):732-734.

    Google Scholar

    [10] 李光明. 藏北羌塘地区新生代火山岩岩石特征及其成因探讨[J]. 地质地球化学, 2000, 28(2):38-44.

    Google Scholar

    [11] 黄勇, 牟世勇, 卢定彪, 等. 藏北鱼鳞山地区鱼鳞山组火山岩的特征及时代探讨[J]. 贵州地质, 2004, 21(3):148-151.

    Google Scholar

    [12] 西藏地矿局. 西藏自治区区域地质志[M]. 北京:地质出版社, 1993.

    Google Scholar

    [13] Yin A, Harrison T M. Geologic evolution of the Himalayan-Tibet-an orogen[J]. Annual Review of Earth and Planetary Sciences. 2000, 28(1):211-280.

    Google Scholar

    [14] 潘桂棠, 李兴振. 青藏高原及邻区大地构造单元初步划分[J]. 地质通报, 2002, 21(11):701-707.

    Google Scholar

    [15] 郭铁鹰. 西藏阿里地质[M]. 武汉:中国地质大学出版社, 1991.

    Google Scholar

    [16] 张振利, 专少鹏, 李广栋, 等. 藏南仲巴地层分区才巴弄组变质玄武质火山岩的发现及其意义[J]. 地质通报, 2007, 26(4):410-416.

    Google Scholar

    [17] Le Bas M J, Le Maitre R W, Streckeisen A, et al. A chemical classi-fication of volcanic rocks based on the total alkali-silica diagram[J]. J. Petrol., 1986, 27(3):745-750.

    Google Scholar

    [18] Turner S, A maud N, Liu J, et al.Post-collision shoshonitic volca-nism on the Tibetan plateau:Implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Petrolo-gy, 1996, 37(1):45-71.

    Google Scholar

    [19] Peccerillo A, Taylor S R. Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area,Northern Turkey[J]. Con-tributions to Mineralogy & Petrology, 1976, 58(1):63-81.

    Google Scholar

    [20] Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5):635-643.

    Google Scholar

    [21] Boynton, W V. Geochemistry of the rare earth elements:meteorite studies[J]. Rare Earth Element Geochemistry, 1984.

    Google Scholar

    [22] Mcdonough W F, Sun S S, Ringwood A E, et al. Potassium, rubid-ium, and cesium in the Earth and Moon and the evolution of the mantle of the Earth[J]. Geochimica Et Cosmochimica Acta, 1992, 56(3):1001-1012.

    Google Scholar

    [23] Vavra G, Schmid R, Gebauer D. Internal morphology, habit and U-Th-Pb microanalysis of amphibolite-to-granulite facies zir-cons:Geochronology of the ivrea zone (Southern Alps)[J]. Contri-butions to Mineralogy and Petrology, 1999, 134(4):380-404

    Google Scholar

    [24] Wu Y B, Zheng Y F. Genesis of zircon and its constraints on inter-pretation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(15):1554-1569.

    Google Scholar

    [25] 李再会, 郑来林, 李军敏, 等. 冈底斯中段林子宗火山岩岩石地球化学特征[J]. 矿物岩石地球化学通报, 2008, 27(1):20-27.

    Google Scholar

    [26] 陈德潜, 陈刚. 实用稀土地球化学[M]. 北京:冶金工业出版社, 1990.

    Google Scholar

    [27] Taylor S R, McLennan S M. The continental crust:its composition and evolution[J]. Physics of the Earth and Planetary Interiors, 1986, 42:196-197.

    Google Scholar

    [28] Sun S S, Mc Donough W F. Chemical and isotopic systematic of oce-anic basalts:Implication for mantle composition and processes[C]//Saunders A D, Norry M J (Magmatism in the Ocean Basins. Geologi-cal Society, London, Special Publication, 1989, 42(1):313-345.

    Google Scholar

    [29] Zhao Z, Mo X, Zhang S. Post-collisional magmatism in Wuyu ba-sin, central Tibet:evidence for recycling of subducted Tethyan oce-anic crust[J]. Science in China (series D), 2001, 44(supp.):27-34.

    Google Scholar

    [30] Ding L, Paul K, Zhong D L, et al. Cenozoic volcanism in Tibet:Evidence for a transition from oceanic to continental subduction[J]. J. Petrol., 2003, 44(10):1833-1865.

    Google Scholar

    [31] Miller C, Schuster R, Klotzli U, et al. Post-collisional potassic and ultrapotassic magmatism in SW Tibet:Geochemical and Sr-Nd-Pb-O isotopic constraints for mantle source characteristics and pet-rogenesis[J]. J. Petrol., 1999, 40(9):1399-1424.

    Google Scholar

    [32] Rollison H R. 杨学明, 杨晓勇, 等, 译.岩石地球化学[M]. 合肥:中国科技大学出版社, 2000.

    Google Scholar

    [33] Ding L, Kapp P, Yue Y H, et al. Postcollisional calc-alka-line la-vas and xenoliths from the southern Qiangtang terrane, central Ti-bet[J]. Earth and Planetary Science Letters, 2007, 254:28-38.

    Google Scholar

    [34] Hacker B R, Edwin G, Ratschbacher L, et al. Hot and dry deep crustal xenoliths from Tibet[J]. Science, 2000, 287:2463-2466.

    Google Scholar

    [35] Wyllie P J. Effects of H2O and CO2 on magma generation in the crust and mantle[J]. Journal of the Geological Society, 1977, 134:215-234.

    Google Scholar

    [36] 候增谦, 高永丰, 孟祥金, 等. 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[J]. 岩石学报, 2004, 20(2):239-248.

    Google Scholar

    [37] 莫宣学, 潘桂棠. 从特提斯到青藏高原形成:构造-岩浆事件的约束[J]. 地学前缘,2006,13(6):43-51.

    Google Scholar

    [38] Wang Q, McDcermott F, Xu J F, et al. Cenozoic K-rich adakitic volcanic rocks in the Hohxil area,northern Tibet:Lower-crustal melting in an intracontinental setting[J]. Geology, 2005, 33(6):465-468.

    Google Scholar

    [39] Defant M J, Drumond M S. Derivation of some modem arc mag-mas by melting of young subducted lithosphere[J]. Nature, 1990, 347:662-665.

    Google Scholar

    [40] 王焰, 张旗, 钱青. 埃达克岩(adakite)的地球化学特征及其构造意义[J]. 地质科学, 2000, 35(2):251-256.

    Google Scholar

    [41] 张旗, 王焰. 埃达克岩的特征及其意义[J]. 地质通报, 2002, 21(7):431-435.

    Google Scholar

    [42] Castillo P R. An overview of adakite petrogenesis[J]. Chinese Bulle-tin, 2006, 51(3):257-268

    Google Scholar

    [43] Drummond M S, Defant M J. A model for Trondhjemite-Tonal-ite-Dacite Genesis and crustal growth via slab melting:Archean to modern comparisons[J]. Journal of Geophysical Research, 1990, 95(B13):21503-21521.

    Google Scholar

    [44] Müller D, Groves D I. Direct and indirect associations between po-tassic igneous rocks, shoshonites and gold-copper deposits[J]. Ore Geology Reviews, 1993, 5:383-406.

    Google Scholar

    [45] Sylvester P J. Post-collisional strongly peraluminous granites[J]. Lithos, 1998, 45:29-44.

    Google Scholar

    [46] Harris N B W, Pearce J B, Tindle A G. Geochemicalcharacteristics of collision-zone magmatism[C]//Coward M P, Ries A C. Colli-sion tectonics. Geo. Soc. Spec.Publ., 1986, 19:67-81

    Google Scholar

    [47] Philip E, Le F P, Peter M, et al. Heat sources for the Teriary meta-morphism and anatexis in the Annapurna-Manaslu region, Central Nepal[J]. Journal of Geophysical Research Solid Earth, 1992, 97:2107-2128.

    Google Scholar

    [48] Bellieni G, Cavazzini G, Fioretti A M, et al. The Cima di Vila (Zin-snock) intrusion, eastern alps:Evidence for crustal melting, acidmafic magma mingling and wall-rock fluid effects[J]. Mineralogy and Petrology, 1996, 56(1/2):125-146.

    Google Scholar

    [49] Guillot S, Le Fort P. Geochemical constraints on the bimodal ori-gin of High Himalayan leucogranites[J]. Lithos, 1995, 35:221-234.

    Google Scholar

    [50] Armijo R, Tapponnier P, Mercier J L, et al. Quaternary extension in southern Tibet:Field observations and tectonic implications[J]. Journal of Geophysical Research Solid Earth, 1986, 91:13803-13872.

    Google Scholar

    [51] Colem M, Hodges K. Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimumage for east-west extension[J]. Na-ture, 1995, 374:49-52.

    Google Scholar

    [52] Hou Z Q, Gao Y F, Qu X M,et al. Origin of adakitic intrusive generated during mid-Miocene east-west extension in southern Tibet[J]. Earth and Planetary Science Letters, 2004, 220:139-155.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(1121) PDF downloads(85) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint