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.
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.
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.
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.
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.
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.