17 Williams I S. U-Th-Pb geochronology by ion microprobe. In: McKibben M A, Shanks W C, Ridley W I, eds. Applications ofMicroanalytical Techniques to Understanding Mineralizing Processes. Rev Econ Geol, 1998, 7: 1–35
[5]
18 Wan Y S, Li R W, Wilde S A, et al. UHP metamorphism and exhumation of the Dabie Orogen: Evidence from SHRIMP dating of zirconand monazite from a UHP granitic gneiss cobble from the Hefei Basin. Geochim Cosmochim Acta, 2005, 69: 4333–4348??
[6]
19 Black L P, Kamo S L, Allen C M, et al. TEMORA 1: A new zircon standard for Phanerozoic U-Pb geochronology. Chem Geol, 2003, 200:155–170??
[7]
20 Ludwig K R. Squid 1.02: A user’s manual. Berkeley Geochronol Centre Spec Publ, 2001, 2: 1–19
[8]
21 Black L P, Kamo S L, Williams I S, et al. The application of SHRIMP to Phanerozoic geochronology: A critical appraisal of four zirconstandards. Chem Geol, 2003, 200: 171–188??
[9]
22 Yuan H L, Gao S, Dai M N, et al. Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon byexcimer laser ablation quadrupole and multiple collector ICP-MS. Chem Geol, 2008, 247: 100–117??
[10]
23 Bievre D P, Taylor P D. Table of the isotopic compositions of the elements. Int J Mass Spectrom Ion Process, 1993, 123: 149–166??
[11]
24 Chu N C, Taylor R N, Chavagnac V, et al. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: Anevaluation of isobaric interference corrections. J Anal At Spectrom, 2002, 17: 1567–1574??
[12]
25 Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. ChemGeol, 2006, 234: 105–126
[13]
26 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, 70(Suppl): A158, doi: 10.1016/j.gca.2006.06.1383
[14]
27 Scherer E, Muenker C, Mezger K. Calibration of the lutetium-hafnium clock. Science, 2001, 293: 683–687??
[15]
28 Blichert-Toft J, Albarede F. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth Planet SciLett, 1997, 148: 243–258??
[16]
29 Vervoort J D, Blichert-Toft J. Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time. GeochimCosmochim Acta, 1999, 63: 533–556??
31 Rubatto D. Zircon trace element geochemistry: Partitioning with garnet and the link between U-Pb ages and metamorphism. Chem Geol,2002, 184: 123–138??
[19]
32 Zheng Y F, Wu Y B, Zhao Z F, et al. Metamorphic effect on zircon Lu-Hf and U-Pb isotope systems in ultrahigh-pressure eclogite-faciesmetagranite and metabasite. Earth Planet Sci Lett, 2005, 240: 378–400??
[20]
33 Zheng Y F, Zhao Z F, Wu Y B, et al. Zircon U-Pb age, Hf and O isotope constraints on protolith origin of ultrahigh-pressure eclogite andgneiss in the Dabie orogen. Chem Geol, 2006, 231: 135–158??
[21]
34 Kapp P, Yin A, Manning C E, et al. Tectonic evolution of the early Mesozoic blueschist-bearing Qiangtang metamorphic belt, central Tibet.Tectonics, 2003, 22: 1043–1068??
[22]
35 Pullen A, Kapp P, Gehrels G E, et al. Triassic continental subduction in central Tibet and Mediterranean-style closure of the Paleo-TethysOcean. Geology, 2008, 36: 351–354??
[23]
36 Gehrels G E, DeCelles P G, Ojha T P, et al. Geologic and U-Pb geochronologic evidence for early Paleozoic tectonism in the Dadeldhurathrust sheet, far-west Nepal Himalaya. J Asian Earth Sci, 2006, 28: 385–408??
[24]
37 Cenki B, Braun I, Brocher M. Evolution of the continental crust in the Kerala Khondalite Belt, southernmost India: Evidence from Ndisotope mapping, U-Pb and Rb-Sr geochronology. Precambrian Res, 2004, 134: 275–292??
[25]
38 Collins A S, Santosh M, Braun I, et al. Age and sedimentary provenance of the Southern Granulites, South India: U-Th-Pb SHRIMPsecondary ion mass spectrometry. Precambrian Res, 2007, 155: 125–138??
[26]
39 Burg J P, Chen G M. Tectonics and structural formation of southern Tibet, China. Nature, 1984, 311: 219–223??
[27]
40 Miller C, Th?ni M, Frank W, et al. The early Palaeozoic magmatic event in the Northwest Himalaya, India: Source, tectonic setting and ageof emplacement. Geol Mag, 2001, 138: 237–251
43 Liu W C, Zhou Z H, Zhang X X, et al. SHRIMP zircon geochronological constraints on a Pan-African orogeny in the Yadong area, southernTibet. Goldschmidt Conference Abstracts, 2006. A365
[31]
44 Cawood P A, Johnson M R W, Nemchin A A. Early Palaeozoic orogenesis along the Indian margin of Gondwana: Tectonic response toGondwana assembly. Earth Planet Sci Lett, 2007, 255: 70–84??
53 Yoshida M, Upreti B N. Neoproterozoic India within East Gondwana: Constraints from recent geochronologic data from Himalaya.Gondwana Res, 2006, 10: 349–356??
55 Leier A L, Kapp P, Gehrels G E, et al. Detrital zircon geochronology of Carboniferous-Cretaceous strata in the Lhasaterrane, Southern Tibet.Basin Res, 2007, 19: 361–378??
[43]
56 Gehrels G E, Kapp P, Pullen A, et al. U-Pb basement and detrital zircon geochronology of the southern Tibetan Plateau and TethyanHimalaya. Geol Soc Amer Abstract Programs, 2008, 40: 329
59 Wilde S A, Valley J W, Peck W H, et al. Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4Gyr ago. Science, 2001, 409: 175–179
[47]
60 Veevers J J. Pan-Gondwanaland post-collisional extension marked by 650–500 Ma alkaline rocks and carbonatites and related detritalzircons: A review. Earth-Sci Rev, 2007, 83: 1–47??
[48]
61 Veevers J J, Saeed A, Belousova E A, et al. U-Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zirconsin Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of theYilgarn Craton. Earth-Sci Rev, 2005, 68: 245–279
[49]
62 Veevers J J, Belousova E A, Saeed A, et al. Pan-Gondwanaland detrital zircons from Australia analysed for Hf-isotopes and trace elementsreflect an ice-covered Antarctic provenance of 700–500 Ma age, TDM of 2.0–1.0 Ga, and alkaline affinity. Earth-Sci Rev, 2006, 76:135–174
[50]
63 Li Z X, Bogdanov S V, Collins A S, et al. Assembly, configuration, and break-up history of Rodinia: A synthesis. Precambrian Res, 2008,160: 179–210??
[51]
64 Yang Z Y, Sun Z M, Yang T S, et al. A long connection (750–380 Ma) between South China and Australia: Paleomagnetic constraints.Earth Planet Sci Lett, 2004, 220: 423–434??
[52]
65 Zhou M F, Kennedy A K, Sun M, et al. Neoproterozoic arc-related mafic intrusions along the northern margin of South China: Implicationsfor the accretion of Rodinia. J Geol, 2002, 110: 611–618??
[53]
66 Li Z X, Li X H, Kinny P D, et al. Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China andcorrelations with other continents: Evidence for a mantle superplume that broke up Rodinia. Precambrian Res, 2003, 122: 85–109??
[54]
67 Wan Y S, Liu D Y, Xu M H, et al. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks innorthwestern Fujian, Cathaysia block, China: Tectonic implications and the need to redefine lithostratigraphic units. Gondwana Res, 2007,12: 166–183??
[55]
68 Li Z X, Li X H, Zhou H, et al. Grenville-aged continental collision in South China: New SHRIMP U-Pb zircon results and implications forRodinia configuration. Geology, 2002, 30: 163–166??
[56]
69 Li X H, Li Z X, Sinclair J A, et al. Revisiting the “Yanbian Terrane”: Implications for Neoproterozoic tectonic evolution of the westernYangtze Block, South China. Precambrian Res, 2006, 151: 14–30??
[57]
70 Li X H, Li W X, Li Z X, et al. 850–790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China: A major episode ofcontinental rift magmatism during the breakup of Rodinia. Lithos, 2008, 102: 341–357??
[58]
71 Ye M F, Li X H, Li W X, et al. SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early NeoproterozoicSibaoan magmatic arc along the southeastern margin of the Yangtze Block. Gondwana Res, 2007, 12: 144–156??
10 Garzanti E, Casnedi R, Jadoul F. Sedimentary evidence of a Cambro-Ordovician orogenic event in the northwestern Himalaya. SedimentGeol, 1986, 48: 237–265
[69]
11 Gehrels G E, DeCelles P G, Martin A, et al. Initiation of the Himalayan Orogen as an early Paleozoic thin-skinned thrust belt. GSA Today,2003, 13: 4–9