[1] | 王希斌,鲍佩声,邓万明,王方国. 1987. 西藏蛇绿岩. 北京: 地质出版社.
|
[2] | 韦振权. 2007. 西藏澎湖西蛇绿岩岩石学、地球化学和榴辉岩中的出溶物及其构造意义.中国科学院广州地球化学研究所博士学位论文。西藏自治区地质调查院. 2003. 中华人民共和国1∶25万班戈县幅区域地质调查报告.
|
[3] | 张旗,周国庆. 2001. 中国蛇绿岩. 北京:科学出版社,1-15.
|
[4] | 钟立峰,夏斌,崔学军,周国庆,陈跟文,韦栋梁. 2006. 藏南罗布莎蛇绿岩壳层熔岩地球化学特征及成因. 大地构造与成矿学, 30(2):231-240.
|
[5] | Alabaster T, Pearce J A and Malpas J. 1982. The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex. Contrib Mineral Petrol, 81: 168-183.
|
[6] | Boynton W V. 1984. Geochemistry of the rare earth elements: Meteorite studies∥Henderson P(ed). Rare Earth Element Geochemistry. Amsterdam: Elsevier, 63-114.
|
[7] | Cameron W E. 1985. Petrology and origin of primitive lavas from the Troodos ophiolite. Contri Mineral Petrol, 89: 239-255.
|
[8] | 陈玉禄,张宽忠,杨志民,罗涛. 2006. 青藏高原班公湖-怒江结合带中段那曲觉翁地区发现完整蛇绿岩. 地质通报,25(6):694-699.
|
[9] | 邓万明, Pearce J A. 1990. 拉萨至格尔木(1985)和拉萨至加德曼都(1986)的蛇绿岩∥中-英青藏高原综合科学考察队. 青藏高原地质演化. 北京: 科学出版社, 218-241.
|
[10] | 李曙光. 1993. 蛇绿岩生成构造环境的Ba?Th?Nb?La判别图. 岩石学报, 9(2): 146-157.
|
[11] | 刘颖,刘海臣,李献华. 1996. ICP?MS准确测定岩石样品中的40余种微量元素. 地球化学,5(6):552-558.
|
[12] | 汤耀庆, 王方国. 1984. 藏北湖区蛇绿岩形成环境浅析∥喜马拉雅地质II. 北京: 地质出版社, 115-139.
|
[13] | Elthon D. 1991. Geochemical evidence for formation of the Bay of islands ophiolite above a subduction zone. Nature, 354: 140-143.
|
[14] | Hofmann A W. 1988. Chemical differentiation of the Earth: The relationship between mantle, continental crust, and oceanic crust. Earth Planet Sci Lett, 90: 297-314.
|
[15] | Janney P E and Castillo P R. 1996. Basalts from the Central Pacific basin: Evidence for the origin of Cretaceous igneous complexes in Jurassic western Pacific. J Geophys Res, 101: 2 875-2 893.
|
[16] | Meschede M. 1986. A method of discriminating between different types of mid?ocean ridge basalts and continental tholeiites with the Nb?Zr?Y diagram. Chem Geol, 56: 207-218.
|
[17] | Pearce J A and Cann J R. 1973. Tectonic setting of basic volcanic rocks determined using trace element analyses. Earth Planet Sci Lett, 19: 290-300.
|
[18] | Pearce J A and Deng Wanming. 1988. The ophiolites of the Tibet geotraverse (Lhasa to Golmud (1985) and Lhasa to Kathmandu (1986))∥Chang C et al. (eds). The Geological Evolution of Tibet. London: R Soc, 215-238.
|
[19] | Pearce J A, Lippard S J and Roberts S. 1984. Characteristics and tectonic significance of supra?subduction zone ophiolites∥Marginal Basin Geology. Geol Soc Lond Spec Publ, 16: 77-94.
|
[20] | Pearce J A. 1975. Basalt geochemistry used to investigate past tectonic environments on Cyprus. Tectonophysics, 25: 41-67.
|
[21] | Pearce J A. 1983. The role of sub?continental lithosphere in aga genesis at destructive plate margins∥Hawkesworth et al. (eds). Continental Basalts and Mantle Xenoliths. Nantwich Shiva, 230-249.
|
[22] | Pearce J A. 1991. Ocean floor comes ashore. Nature, 354: 110-111.
|
[23] | Pearce J A. 1996. A user′s guide to basalt discrimination diagrams∥Wyman D A(ed). Trace Element Geochemistry of Volcanic Rocks: Applications for Massive Sulphide Exploration. Geochem Short Course Notes?Geol Assoc Can, 12: 79-113.
|
[24] | Rollinson H R. 1993. Using Geochemical Data: Evaluation, Presentation, Interpretation. New York: John Wiley & Sons, 155.
|
[25] | Thy P and Moores E M. 1988. Crustal accretion and tectonic setting of the Troodos ophiolite, Cyprus. Tectonophysics, 147: 221-245.
|
[26] | Wilson M. 1989. Igneous Petrogenesis. London: Unwin Hyman, 1-25.
|
[27] | Wood D A. 1980. The application of a Th?Hf?Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province. Earth Planet Sci Lett, 50: 11-30.
|