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地质通报  2007 

西藏拉萨地块MORB型榴辉岩的岩石地球化学特征

, PP. 1327-1339

Keywords: 松多榴辉岩大洋玄武岩超高压变质带拉萨地块青藏高原

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[1]  Chopin C. Coesite and pure pyrope in high-grade blueschists of the Western Alps: A first record and some consequences[J]. Contributions to Mineralogy and Petrology, 1984, 86:107-118.
[2]  XU Shutong, Okey A I, Ji S, et al. Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting[J]. Science, 1992, 256:80-82.
[3]  Chopin C. Ultrahigh-pressure metamorphism: Tracing continental crust into the mande [J]. Earth and Planetary Science Letters, 2003, 212:1-14.
[4]  杨经绥 Shigenori Maruyama 等.柴达木盆地北缘早古生代高压――超高压变质带中发现典型超高压矿物――柯石英[J].地质学报,:.
[5]  张建新 杨经绥 等.阿尔金榴辉岩中超高压变质作用证据[J].科学通报,:.
[6]  Jang B M. Sm-Nd isotope tracer study of UHP metamorphic rocks: implications for continental subduction and collisional tectonics [J].International Geology Review, 1999, 41:859-885.
[7]  Zhang R Y, Liou J G, Cong B L. Petrogenesis of garnet-bearing ultramafic rocks and associated eclogites in Su-Lu ultrahigh-P metamorphic terane, eastern China[J]. Journal of Metamorphic Geology, 1994, 12:169-186.
[8]  Cong B L, Zhai M G, Caeswell D A. Petrogenesis of the ultrahigh- pressure rocks and their country rocks at Shuanghe in Dabieshan, central China[J]. European Journal of Mineralogy, 1995, 7:119-138.
[9]  Bryan W B. Inferred geological settings and differentiation in basaltfrom the Deep Sea Drilling Project[J]. Jour. Geophy. Res., 1976,81: 4285-4304.
[10]  徐向珍 杨经绥 李天福 等.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[J].地质通报,2007,26(10):1340-1355.
[11]  潘桂棠 王立全 朱弟成.青藏高原区域地质调查中几个重大科学问题的思考[J].地质通报,:.
[12]  朱同兴 潘桂棠 等.藏南喜马拉雅北坡色龙地区二叠系基性火山岩的发现及其构造意义[J].地质通报,:.
[13]  翟庆国 李才 程立人 张以春.西藏羌塘角木日地区二叠纪蛇绿岩的地质特征及意义[J].地质通报,2004,23(12):1228-1230.
[14]  李才 翟庆国 程立人 徐峰 黄小鹏.青藏高原羌塘地区几个关键地质问题的思考[J].地质通报,2005,24(4):295-301.
[15]  吴根耀.藏东左贡地区碧土蛇绿岩:古特提斯主洋盆的地质记录[J].地质通报,2006,25(6):685-693.
[16]  吴根耀.藏东碧土地区古特提斯主洋盆中的亚速尔型洋岛玄武岩[J].地质通报,2006,25(7):772-781.
[17]  朱同兴 张启跃 董瀚 等.藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩[J].地质通报,2006,25(12):1413-1418.
[18]  李才 翟庆国 董永胜 等.青藏高原龙木错-双湖板块缝合带与古特提斯洋演化记录[J].地质通报,2007,26(1):13-21.
[19]  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.
[20]  Hong-Feng Tang, Cong-Qiang Liu, Shunichi Nakai, et al. Geochemistry of eclogites from the Dabie-Sulu terrane, eastern China: New insights into protoliths and trace element behaviour during UHP metamorphism[J]. Lithos, 2007, 95:441-457.
[21]  Yatsmi Y, Eggins S. Subduction zone magmatism[M]. Oxford: Blackwell, 1995:211.
[22]  Hofinann A W. Chemical differentiation of the Earth: the relationship between mande, contirtental crust, and oceanic crust[J]. Earth Planet. Sci. Lett., 1988, 90:297-314.
[23]  McDonough W F. Constraints on the composition of the continental lithospheric mantle[J]. Earth Planet. Sci. Lett., 1990,101:1-18.
[24]  McDonough W F. Partial melting of subducted oceanic crust and isolation of its residual eclogitic lithology [J]. Phil. Trans. R. Soc. London Set., 1991, A 335:407-418.
[25]  Jochum K P, Seufert H M, Spettel B, et al. The solar system abundances of Nb, Ta and Y, and the relative abundances of refractory lithophile elementS in diferentiated planetary bodies[J]. Geochim. Cosmochim. Acta, 1986, 50:1173-1183.
[26]  Jorg A Pfander, Carsten Munker, Andreas Stracke, et al. Nb/Ta and Zr/Hf in ocean island basalts-lmplications for crust - mantle differ entiation and the fate of Niobium[J]. Earth and Planetary Science Letters, 2007, 254:158-172.
[27]  Jochum K P, Stolz J. High-precision Nb, Ta, Zr, and Y data for carbonaceous chondrites: constraints on solar system Nb/Ta and Zr/ Nb ratios, Meteorit[J]. Planet. Sci., 1997,32:67.
[28]  Jochum K P, Hofmann A W. Nb/Ta in MORB and continental crust implications for a superchondritic Nb/Ta reservoir in the mantle[J]. EOS, 1998, 79:354.
[29]  Bodinier J L, Merlet C, Bedini R M, et al. Distribution of niobium, tantalum, and other highly incompatible trace elements in the lithospheric mande: the spinel paradox[J]. Geochim. Cosmochim. Acta, 1996, 60:545-550.
[30]  Rudnick R L, Barth M, Horn I, et al. Rutile-bearing refractory eclogites missing link between continents and depleted mantle[J]. Science, 2000, 287:278-281.
[31]  西藏地质矿产局.1:20万沃卡幅区域地质调查报告[R].,1994..
[32]  Smith D C. Coesite in clinopyroxene in the caledonides and its implications for geodynamics[J]. Nature, 1984, 310:641-644.
[33]  刘良 肖培喜 等.阿尔金发现超高压(〉3.8GPa)石榴二辉橄榄岩[J].科学通报,:.
[34]  O\\'Brien P J, Zotov N, Law R, et al. Coesite in Himalayan eclogite and implications for models of India-Asia collision[J]. Geology, 2001, 29:435-438.
[35]  Kaneko Y, Katayama I, Yamamoto H, et al. Timing of Himalayan ultrahigh-pressure metamorphism: Sinking rate and subduction angle of the Indian continental crust beneath Asia[J]. Journal of Metamorphic Geology, 2003, 21:589-599.
[36]  Sachan H, Mucherjee B K, Ishida H, et al. New discovery of coesite from the Indian Himalaya[C]//Fluid/slab/mantle interactions and ultrahigh-P minerals. UHPM Workshop 2001, Waseda, Japan, 2001:124-128.
[37]  Mukherjee B K, Sachan H K, Ogasawara Y, et al. Carbonate-bearing UHPM rocks from the Tso-Morari region, Ladakh, India: Petrological implications[J]. International Geology Review, 2003, 45: 49-69.
[38]  Li Cai, Zhai Qingguo, Dong Yongsheng, et al. Discovery of eclogite and its geological significance in Qiangtang area, central Tibet[J]. Chinese Science Bulletin, 2006, 51 (9): 1095-1100.
[39]  杨经绥 许志琴 耿全如 等.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[J].地质学报,2006,80(20):1787-1792.
[40]  Jahn B M. Geochemical and isotopic characteristics of UHP eclogites and ultramafic rocks of the Dabie orogen: collisional tectonics [C]//Hacker, Liou. When Continents Collide: Geodynamics and Geochemistry of Ultra-high pressure Rocks. Kluwer: Academic Publishers, 1998:203 -240.
[41]  Ye Kai, Hirajima T. High-pressure marble at Yangguantun, Rongcheng County , Shandong Province, eastern China[J]. Mineral Petrol., 1996, 57:151-165.
[42]  王希斌 郑海翔 曹佑功 李光芩 等.西藏雅鲁藏布江(中段)蛇绿岩组合层序及特提斯洋壳演化的模式[C].李光芩,等.中法喜马拉雅考察成果[C].北京:地质出版社,1984.181-207.
[43]  Allege C J, CourtiUot V, Tapponnier P, et al. Structure and evolu- tion of the Himalaya-Tibet orogenic belt[J]. Nature, 1984, 307:17- 22.
[44]  吴新国 贾建称 崔邢涛 等.雅鲁藏布江缝合带开合演化模式的探讨[J].现代地质,2005,19(4):488-494.
[45]  Girardeau J, Marcoux J, Allege C J, et al. Tectonic environment and geodynamic significance of the Neo-Cimmerian Dongqiao ophiolite, Bangong-Nujiang suture zone, Tibet [J]. Nature, 1984, 307:27-31.
[46]  张旗 杨瑞英.西藏丁青蛇绿岩中玻镁安山岩类的深成岩及其地质意义[J].科学通报,1985,16:1243-1245.
[47]  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,1993.264-477.
[48]  杨经绥 许志琴 李天福 等.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?[J].地质通报,2007,26(10):1277-1287.
[49]  中国地质科学院成都地质矿产研究所.青藏高原及其邻区地质图 1:1500000[M].成都:成都地图出版社,1988..
[50]  中国地质调查局成都地质矿产研究所.青藏高原及其邻区地质图 1:1500000[M].成都:成都地图出版社,2004..
[51]  Jahn B M, Rumble D, Liou J G. Geochemistry and isotope tracer study of UHP metamorphic rocks[J]. EMU Notes in Mineralogy, 2003, 5(12) :365 -414.
[52]  Griffin W L, Brueckner H K. REE,Rb-Sr and Sm-Nd studies of Norwegian eclogites[J]. Chemical Geology, 1985, 52(2):249-271.
[53]  凌文黎 贾望鲁.大别超高压变质过程中流体作用的微量元素效应及其地球化学意义[J].地球化学,2000,29(6):532-541.
[54]  周汉文 李献华.南大别花凉亭冷榴辉岩退变质作用过程的元素地球化学变异[J].地球化学,:.
[55]  侯增谦 莫宣学 朱勤文 等.“三江”古特提斯地幔热柱-洋中脊玄武岩证据[J].地球学报,1996,17(4):362-375.
[56]  Bernard-Criffiths J, Peucat Jean-Jacques, Cornichet J. U-Pb, Nd isotope and REE geochemistry in eclogues from the Cabo Ortegal Complex, Galicia Spain: an example of REE immobility conserving MORB-like patterns during high-grade metamorphism[J]. Chemical Geology, 1985,52(2):217-22.
[57]  Shatsky V S, Kozmenko O A , Snholev N V . Behaviour of rare earth elements during high-pressure metamorphism[J]. Lithos, 1990, 25:219-226.
[58]  李昌年.火成岩微量元素岩石学[M].武汉:中国地质大学出版社,1992.1-195.
[59]  赵振华.微量元素地球化学原理[M].北京:科学出版社,1997..
[60]  Pearce J A. Role of sub-continental lithosphere in magma genesis at active continental margins[C]//Hawkesworth C J, Norry M J. Continental Basalt.s and Mantle Xenoliths. 1983:230-249.

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