10 Lu S N, Li H K, Zhang C L, et al. Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton andsurrounding continental fragments. Precambrian Res, 2008, 160: 94–107??
[11]
11 Song B, Nutman A P, Liu D Y, et al. 3800 to 2500 Ma crustal evolution in the Anshan area of Liaoning Province, northern China.Precambrian Res, 1996, 78: 79–94??
[12]
12 Wan Y S, Zhang Z Q, Wu J S, et al. Geochemical and Nd isotopic characteristic of some rocks from the Paleoarchean Chentaigousupracrustal, Anshan area, NE China. Cont Dynam, 1997, 2: 39–46
16 Zhang S B, Zheng Y F, Wu Y B, et al. Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China.Precambrian Res, 2006, 151: 265–288??
[17]
17 Qiu Y M, Gao S, McNaughton N J, et al. First evidence of ≥3.2 Ga continental crust in the Yangtze craton of South China and itsimplications for Archean crustal evolution and Phanerozoic tectonics. Geology, 2000, 28: 11–14
28 Hu A Q, Jahn B M, Zhang G X, et al. Crustal evolution and Phanerozoic crustal growth in northern Xinjiang: Nd isotope evidence. 1.Isotopic characterization of basement rocks. Tectonophysics, 2000, 328: 15–51
[29]
29 Shu L S, Deng X L, Zhu W B, et al. Precambrian tectonic evolution of the Tarim Block, NW China: New geochronological insights fromthe Quruqtagh domain. J Asian Earth Sci, 2010, doi: 10.1016/j.jseaes.2010.08.018
[30]
30 Long X P, Yuan C, Sun M, et al, Archean crustal evolution of the northern Tarim Craton, NW China: Zircon U-Pb and Hf isotopicconstraints. Precambrian Res, 2010, 180: 272–284
[31]
31 Xu B, Jian P, Zheng H F, et al. U-Pb zircon geochronology and geochemistry of Neoproterozoic volcanic rocks in the Tarim Block ofnorthwest China: Implications for the breakup of Rodinia supercontinent and Neoproterozoic glaciations. Precambrian Res, 2005, 136:107–123??
[32]
32 Zhang C L, Li X H, Li Z X, et al. Neoproterozoic ultramafic-mafic-carbonatite complex and granitoids in Quruqtagh of northeastern TarimBlock, western China: Geochronology, geochemistry and tectonic implications. Precambrian Res, 2007, 152: 149–169??
[33]
33 Nasdala L, Norberg N, Schaltegger U, et al. Plesovice zircon—A new natural reference material for U-Pb and Hf isotopic microanalysis.Chem Geol, 2008, 249: 1–35??
[34]
34 Liu Y S, Hu Z C, Gao S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying aninternal standard. Chem Geol, 2008, 257: 34–43??
[35]
35 Ludwig K R. User’s Manual for Isoplot 3.00. A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Center,Special Publication No. 4a, 2003
38 Elhlou S, Belousova E, Griffin W L, et al. Trace element and isotopic composition of GJ-red zircon standard by laser ablation. GeochimCosmochim Acta, 2006, (Suppl): A158
[39]
39 Soderlund U, Patchett P J, Vervoort J D, et al. The 176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrianmafic intrusions. Earth Planet Sci Lett, 2004, 219: 311–324??
[40]
40 Blichert-Toft J, Albarède F. The Lu-Hf geochemistry of the chondrites and the evolution of the mantle-crust system, Earth Planet Sci Lett,1997, 148: 243–258??
[41]
41 Grifin W L, Pearson N J, Belousova E, et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zirconmegacrysts in kimberlites. Geochim Cosmochim Acta, 2000, 64: l33–147
[42]
42 Amelin Y, Lee D C, Halliday A N, et al. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons. Nature, 1999,399: 252–255??
[43]
43 DePaolo D J, Wasserburg G J. Nd isotopic variations and petrogenetic models. Geophys Res Lett, 1976, 3: 249–252??