5 Liu L, Che Z C, Luo J H, et al. A discussion on the structure and tectonic evolution of the Altyn Tagh orogenic Zone. Earth Sci Fron, 2000,7(Suppl): 206
[6]
6 Zhang J X, Zhang Z M, Xu Z Q, et al. Petrology and geochronology of eclogite from the western segment of the Altyn Tagh, northwern China. Lithos, 2001, 56: 187-206？？
17 Chen X H, Yin A, George E, et al. Two phase of Mesozoic north-south extension in the eastern Altyn Tagh range, northern Tibetan Plateau. Tectonics, 2003, 22: 1-22
22 Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: Implication for mantle composition and processes. In: Saunder A D, Norry M J, eds. Magmatism in the Ocean Basins. Geol Soc Spe Publ London, 1989, 42: 313-345？？
[23]
23 McDonough W F, Sun S S. The composition of the Earth. Chem Geol, 1995, 120: 223-253？？
[24]
24 Flagler P A, Spray J G. Generation of plagiogranite by amphibolite anatexis in oceanic shear zones. Geology, 1991, 19: 70-73？？
[25]
25 Pedersen R B, Malpas J. The origin of oceanic plagiogranites from the Karmoy ophiolite, western Norway. Contrib Mineral Petrol, 1984, 88:36-52？？
[26]
26 Gao S, Liu X M, Yuan H L, et al. Analysis of forty-two major and trace elements of USGS and NISTSRM glasses by LA-ICP-MS. Geostand News Lett, 2002, 22: 181-195
28 Hermann J, Rubatto D, Korsakov A. Multiple zircon growth during fast exhumation of diamondiferous, deeply subducted continental crust (Kokchetav Massif, Kazakhstan). Contrib Mineral Petrol, 2001, 141: 66-82？？
[29]
29 Buick R, Thomett J R, Naughton N J, et al. Record of emergent continental crust similar to 3.5 billion years ago in the Pilbara craton of Australia. Nature, 1995, 375: 574-575
31 Li W X, Li X H. Adakitic granites within the NE Jiangxi ophiolites, South China: Geochemical and Nd isotopic evidence. Precambrian Res,2003, 122: 29-44？？
[32]
35 Whitehead J, Dunning G R, Spray J G. U-Pb geochronology and origin of granitoid rocks in the Thetford Mines ophiolite, Canadian Appalachians. Geol Soc Am Bull, 2000, 112: 915-928？？
[33]
36 Peters T, Kamber B S. Peraluminous, potassium-rich granitoids in the Semail Ophiolite. Contrib Mineral Petrol, 1994, 118: 229-238？？
[34]
37 Rapp R P, Watson E B, Miller C F. Partial melting of amphibolite/eclogite and the origin of Archean trondhjemite and tonalities. Precambrian Res, 1991, 51: 1-25？？
[35]
38 Rapp R P, Watson E B. Dehydration melting of metabasalt at 8-32 kbar: Implications for continental growth and crust-mantle recycling. J Petrol, 1995, 36: 891-931
[36]
39 Wilhelm S, Hans A S. Partial fusion of basic granulites at 5 to 15 kbar: Implications for the origin of TTG magmas. Contrib Mineral Petrol,1997, 127: 30-45？？
[37]
40 Guo F, Nakamura E, Fan W M, et al. Generation of Palaeoce
[38]
32 David C G, William P L, Hans G A L. Petrology and geochemistry of plagiogranite in the Canyon Mountain ophiolite, Oregon. Contrib Mineral Petrol, 1981, 77: 82-89？？
[39]
33 Claoue-long J C, Compston W, Roberts J, et al. Two carboniferous ages: A comparison of SHRIMP zircon dating with conventional zircon ages and 40Ar/39Ar analysis. In: Berggren W A, Kent D V, Aubry M P, et al, eds. Geochronology, Time Scales and Global Stratigraphic Correlation. SEPM Spec Publ, 1995, 4: 3-31
