31 Zhang S H, Jiang G Q, Zhang J M, et al. U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in SouthChina: Constraints on late Neoproterozoic glaciations. Geology, 2005, 33: 473-476??
[3]
32 Hawkesworth C J, van Calsteren P W C. Radiogenic isotopes--Some geological aplications. In: Henderson P, ed. Rare Earth ElementGeochemistry. Amsterdam: Elsevier, 1984. 375-421
[4]
33 DePaolo D J, Linn A M, Schubert G. The continental crustal age distribution: Methods of determining mantle separation ages from Sm-Ndisotopic data and application to the southwestern United States. J Geophys Res, 1991, 96: 2071-2088??
35 Wang W, Wang F, Chen F, et al. Detrital zircon ages and Hf-Nd isotopic composition of Neoproterozoic sedimentary rocks in the YangtzeBlock: Constraints on the deposition age and provenance. J Geol, 2010, 118: 79-94??
[7]
36 Li X H, Li Z X, Zhou H W, et al. U-Pb zircon geochronology, geochemistry and Nd isotopic study of Neoproterozoic bimodal volcanicrocks in the Kangdian rift of South China: Implications for the initial rifting of Rodinia. Precambrian Res, 2002, 113: 135-154??
[8]
37 Ling W L, Gao S, Zhang B R, et al. Neoproterozoic tectonic evolution of the northwestern Yangtze craton, South China: Implications foramalgamation and break-up of Rodinia Supercontinent. Precambrian Res, 2003, 122: 111-140??
[9]
38 Li W X, Li X H, Li Z X. Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance.Precambrian Res, 2005, 136: 51-66??
40 Wang X C, Li X H, Li W X, et al. Ca. 825 Ma komatitic basalts in South China: First evidence for >1500°C mantle melts by a Rodinianmantle plume. Geology, 2007, 35: 1103-1106
[12]
41 Li W X, Li X H, Li Z X. Middle Neoproterozoic syn-rifting volcanic rocks in Guangfeng, South China: Petrogenesis and tectonicsignificance. Geol Mag, 2008, 145: 475-489
[13]
42 Wang X C, Li X H, Li W X, et al. The Bikou basalts in the northwestern Yangtze Block, South China: Remnants of 820-810 Ma continentalflood basalts. Geol Soc Am Bull, 2008, 120: 1478-1492
[14]
43 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??
[15]
44 Li X H, Li W X, Li Q L. Petrogenesis and tectonic significance of the ~850 Ma Gangbian alkaline complex in South China: Evidence fromin situ zircon U-Pb dating, Hf-O isotopes and whole-rock geochemistry. Lithos, 2010, 114: 1-15??
48 Chen J F, Foland K A, Xing F M, et al. Magmatism along the south margin of the Yangtze block: Precambrian collision of the Yangtze andCathaysia blocks of China. Geology, 1991, 19: 815-818??
[20]
49 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??
[21]
50 Li Z X, Wartho J A, Occhipinti S, et al. Early history of the eastern Sibao Orogen (South China) during the assembly of Rodinia: New mica40Ar/39Ar dating and SHRIMP U-Pb detrital zircon provenance constraints. Precambrian Res, 2007, 159: 79-94??
[22]
51 Li W X, Li X H, Li Z X, et al. Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation betweenthe Yangtze and Cathaysia Blocks. Gondwana Res, 2008, 13: 288-301??
[23]
52 Li X H, Li W X, Li Z X, et al. Amalgamation between the Yangtze and Cathaysia blocks in South China: Constraints from SHRIMP U-Pbzircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks. Precambrian Res, 2009, 174: 117-128??
57 Liu L, Chen D L, Zhang A D, et al. Geochemical characteristics and LA-ICPMS zircon U-Pb dating of amphibolites in the Songshugouophiolite in the Eastern Qinling. Acta Geol Sin, 2004, 78: 137-145
59 Ratschbacher L, Hacker B R, Calvert A, et al. Tectonics of the Qinling (Central China): Tectonostratigraphy, geochronology, anddeformation history. Tectonophysics, 2003, 366: 1-53??
[31]
60 Huang W, Wu Z W. Evolution of the Qinling orogenic belt. Tectonics, 1992, 11: 371-380??
[32]
3 Taylor S R, McLennan S M. The geochemical evolution of the continental crust. Rev Geophys, 1995, 33: 241-265??
[33]
4 O’Nions R K, Hamilton P J, Hooker P J. A Nd isotope investigation of sediments related to crustal development in the British Isles. EarthPlanet Sci Lett, 1983, 63: 229-240??
15 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 and itsimplications for Archean crustal evolution and Phanerozoic tectonics. Geology, 2000, 28: 11-14
[36]
16 Zhang S B, Zheng Y F, Wu Y B, et al. Zircon U-Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking ofArchean crust in South China. Earth Planet Sci Lett, 2006, 252: 56-71
19 Sun W H, Zhou M F, Yan D P, et al. Provenance and tectonic setting of the Neoproterozoic Yanbian Group, western Yangtze Block (SWChina). Precambrian Res, 2008, 167: 213-236??
2 Zheng J P, Griffin W L, O’Reilly S Y, et al. Widespread Archean basement beneath the Yangtze Craton. Geology, 2006, 34: 417-420??
[46]
5 Allegre C J, Rousseau D. The growth of the continent through geological time studied by Nd isotope analysis of shales. Earth Planet SciLett, 1984, 67: 19-34??
[47]
6 Goldstein S J, Jacobsen S B. Nd and Sr isotopic systematics of river suspended material: Implications for crustal evolution. Earth Planet SciLett, 1988, 87: 249-265??
[48]
7 Miller J F, Harris N B W. Evolution of continental crust in the central Andes: Constraints from Nd isotope system. Geology, 1989, 17:615-617??
[49]
8 Zhao J X, McCulloch M T, Bennett V C. Sm-Nd and U-Pb zircon isotopic constraints on the provenance of sediments from the AmadeusBasin, Central Australia: Evidence for REE fractionation. Geochim Cosmochim Acta, 1992, 56: 921-940??
13 Li X H, McCulloch M T. Secular variation in the Nd isotopic composition of Neoproterozoic sediments from the southern margin of theYangtze Block: Evidence for a Proterozoic continental collision in southeast China. Precambrian Res, 1996, 76: 67-76??
[55]
24 Barfod G H, Albarède F, Knoll A H, et al. New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils. Earth Planet Sci Lett, 2002,201: 203-212??
[56]
25 Chen D F, Dong W Q, Zhu B Q, et al. Pb-Pb ages of Neoproterozoic Doushantuo phosphorites in South China: Constrains on earlymetazoan evolution and glaciations events. Precambrian Res, 2004, 132: 123-132??
[57]
26 Knoll A H, Xiao S H. On the age of the Doushantuo Formation. Acta Micropalaeontol Sin, 1999, 16: 225-236
28 Yin C Y, Tang F, Liu Y Q, et al. U-Pb zircon age from the base of the Ediacaran Doushantuo Formation in the Yangtze Gorges, SouthChina: Constraint on the age of Marinoan glaciations. Episodes, 2005, 28: 48-49
61 Xue F, Lerch F, Kr?ner A, et al. Tectonic evolution of the East Qinling Mountains, China, in the Paleozoic: A review and a new tectonicmodel. Tectonophysics, 1996, 253: 271-284??