Research ArticleARTICLES
Precambrian crustal growth of Yangtze Craton as revealed by detrital zircon studies
Xiaoming Liu, Shan Gao, Chunrong Diwu and Wenli Ling
American Journal of Science April 2008, 308 (4) 421-468; DOI: https://doi.org/10.2475/04.2008.02
Xiaoming Liu
Shan Gao
Chunrong Diwu

REFERENCES
- ↵Amelin Y., Lee, D. C., Halliday, A. N., and Pidgeon, R. T., 1999, Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons: Nature, v. 399, p. 252–255, doi:10.1038/20426.
- ↵Ames L., Zhou, G. Z., and Xiong, B. C., 1996, Geochronology and isotopic characteristics of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons, central China: Tectonics, v. 15, p. 472–489, doi:10.1029/95TC02552.
- ↵Andersen T., 2002, Correction of common lead in U-Pb analyses that do not report 204Pb: Chemical Geology, v. 192, p. 59–79, doi:10.1016/S0009-2541(02)00195-X.
- ↵Barfod G. H., Albarède, F., Knoll, A. H., Xiao, S., Télouk, P., Robert, F. R., and Baker, L., 2002, New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils: Earth and Planetary Science Letters, v. 201, p. 203–212, doi:10.1016/S0012-821X(02)00687-8.
- ↵Belousova E. A., Griffin, W. L., O'Reilly, S. Y., and Fisher, N. I., 2002, Igneous zircon: trace element composition as an indicator of source rock type: Contributions to Mineralogy and Petrology, v. 143, p. 602–622.
- ↵Benus A. P., 1988, Sedimentological context of a deep-water Ediacaran fauna (Mistaken Point Formation, Avalon Zone, eastern Newfoundland), in Landing, E., Narbonne, G. M., Myrow, P., editors, Trace Fossils, Small Shelly Fossils and the Precambrian-Cambrian Boundary: Bulletin of the New York State Museum, p. 8–9.
- ↵Bichert-Toft J., and Albarède, F., 1997, The Lu–Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system: Earth and Planetary Science Letters, v. 148, p. 243–258, doi:10.1016/S0012-821X(97)00040-X.
- ↵Black L. P., Kamo, S. L., Allen, C. M., Aleinikoff, J. N., Davis, D. W., Korsch, R. J., and Foudoulis, C., 2003, TEMORA 1: A new zircon standard for Phanerozoic U-Pb geochronology: Chemical Geology, v. 200, p. 155–170, doi:10.1016/S0009-2541(03)00165-7.
- ↵Bruguier O., Lancelot, J. R., and Malavieille, J., 1997, U–Pb dating on single detrital zircon grains from the Triassic Songpan–Ganze flysch Central China: provenance and tectonic correlations: Earth and Planetary Science Letters, v. 152, p. 217–231, doi:10.1016/S0012-821X(97)00138-6.
- ↵
- ↵Condie K. C., Beyer, E., Belousova, E., Griffin, W. L., and O'Reilly, S. Y., 2005, U–Pb isotopic ages and Hf isotopic composition of single zircons: The search for juvenile Precambrian continental crust: Precambrian Research, v. 139, p. 42–100, doi:10.1016/j.precamres.2005.04.006.
- ↵Condon D., Zhu, M., Bowring, S., Wang, W., Yang, A., and Jin, Y., 2005, U-Pb Ages from the Neoproterozoic Doushantuo Formation, China: Science, v. 308, p. 95–98, doi:10.1126/science.1107765.
- ↵Cong B. L., 1996, Ultrahigh-pressure Metamorphic Rocks in the Dabieshan–Sulu Region of China: Beijing, Science Press, 224 p.
- ↵Coogan L. A., and Hinton, R. W., 2006, Do the trace element compositions of detrital zircons require Hadean continental crust?: Geology, v. 34, p. 633–636, doi:10.1130/G22737.1.
- ↵DeCelles P. G., Gehrels, G. E., Quade, J., LaReau, B., and Spurlin, M., 2000, Tectonic implications of U-Pb zircon ages of the Himalayan orogenic belt in Nepal: Science, v. 288, p. 497–499, doi:10.1126/science.288.5465.497.
- ↵Ferry J. M., and Watson, E. B., 2007, New thermodynamic model and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers: Contributions to Mineralogy and Petrology, doi:10.1007/s00410-007-0201-0.
- ↵Gao S., Zhang, B. R., Wang, D. P., Ouyang, J. P., and Xie, Q. L., 1996, Geochemical evidence for Proterozoic tectonic evolution of the Qinling orogenic belt and adjacent margins of the North China and Yangtze cratons: Precambrian Research v. 80, p. 23–48, doi:10.1016/0301-9268(95)00100-X.
- ↵Gao S., Ling, W. L., Qiu, Y., Zhou, L., Hartmann, G., and Simon, K., 1999, Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton: Evidence for cratonic evolution and redistribution of REE during crustal anatexis: Geochimica et Cosmochimica Acta, v. 63, p. 2071–2088, doi:10.1016/S0016-7037(99)00153-2.
- ↵Gao S., Rudnick, R. L., Yuan, H. L., Liu, X. M., Liu, Y. S., Xu, W. L., Ling, W. L., Ayers, J., Wang, X. C., and Wang, Q. H., 2004, Recycling lower continental crust in the North China craton: Nature, v. 432, p. 892–897, doi:10.1038/nature03162.
- ↵Goldschmidt V. M., 1933, Grundlagen der quantitativen Geochemie: Fortschritte der Mineralogie, Kirstllographie und Petrographie, v. 17, p. 112.
- ↵Greentree M. R., Li, Z. X., Li, X. H., and Wu, H. C., 2006, Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia: Precambrian Research, v. 151, p. 79–100, doi:10.1016/j.precamres.2006.08.002.
- ↵Griffin W. L., Pearson, N. J., Belousova, E., Jackson, S. E., Achterbergh, E. V., O'Reilly, S. Y., and Shee, S. R., 2000, The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites: Geochimica et Cosmochimica Acta, v. 64, p. 133–147, doi:10.1016/S0016-7037(99)00343-9.
- ↵Griffin W. L., Belousova, E. A., Shee, S. R., Pearson, N. J., and O'Reilly, S. Y., 2004, Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons: Precambrian Research, v. 131, p. 231–282, doi:10.1016/j.precamres.2003.12.011.
- ↵Hacker B. R., Ratschbacher, L., Webb, L., Ireland, T., Walker, D., and Dong, S., 1998, U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling–Dabie Orogen, China: Earth and Planetary Science Letters, v. 161, p. 215–230, doi:10.1016/S0012-821X(98)00152-6.
- ↵Hanchar J. M., and Hoskin, P. W. O., editors, 2003, Zircon: Reviews in Mineralogy and Geochemistry, v. 53, 500 p.
- ↵Hawkesworth C. J., and Kemp, A. I. S., 2006a, Evolution of the continental crust: Nature, v. 443, p. 811–817, doi:10.1038/nature05191.
- ↵––––2006b, Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution: Chemical Geology, v. 226, p. 144–162, doi:10.1016/j.chemgeo.2005.09.018.
- ↵Hoffman P. F., Kaufman, A. J., Halverson, G. P., and Schrag, D. P., 1998, A Neoproterozoic snowball Earth: Science, v. 281, p. 1342–1346, doi:10.1126/science.281.5381.1342.
- ↵Iizuka T., and Hirata, T., 2005, Improvements of precision and accuracy in in-situ Hf isotope microanalysis of zircon using the laser ablation-MC-ICPMS technique: Chemical Geology, v. 220, p. 121–137, doi:10.1016/j.chemgeo.2005.03.010.
- ↵Iizuka T., Hirata, T., Komiya, T., Rino, S., Katayama, I., Motoki, A., and Maruyama, S., 2005, U-Pb and Lu-Hf isotopic systematics of zircons from the Mississippi River sand: Implications for reworking and growth of continental crust: Geology, v. 33, p. 485–488, doi:10.1130/G21427.1.
- ↵Jahn B. M., Gallet, S., and Han, J. M., 2001, Geochemistry of the Xining, Xifeng, and Jixian sections, Loess Plateau of China: eolian dust provenance and paleosol evolution during the last 140 ka: Chemical Geology, v. 178, p. 71–94, doi:10.1016/S0009-2541(00)00430-7.
- ↵Kemp A. I. S., Hawkesworth, C. J., Paterson, B. A., and Kinny, P. D., 2006, Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon: Nature, v. 439, p. 580–583, doi:10.1038/nature04505.
- ↵Košler J., Fonneland, H., Sylvester, P., Tubrett, M., and Pedersen, R. B., 2002, U–Pb dating of detrital zircons for sediment provenance studies –a comparison of laser ablation ICPMS and SIMS techniques: Chemical Geology, v. 182, p. 605–618, doi:10.1016/S0009-2541(01)00341-2.
- ↵Krogh T. E., Strong, D. F., O'Brien, S. J., and Papezik, V., 1998, Precise U-Pb zircon dates from the Avalon Terrane in Newfoundland: Canadian Journal of Earth Sciences, v. 25, p. 442–453.
- ↵Li W. X., Li, X. H., and Li, Z. X., 2005, Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance: Precambrian Resarch, v. 136, p. 51–66, doi:10.1016/j.precamres.2004.09.008.
- ↵Li X. H., and McCulloch, M. T., 1996, Secular variation in the Nd isotopic composition of Neoproterozoic sediments from the southern margin of the Yangtze Block: Evidence for a Proterozoic continental collision in southeast China: Precambrian Research, v. 76, p. 67–76, doi:10.1016/0301-9268(95)00024-0.
- ↵Li X. H., Li, Z. X., Zhou, H. W., Liu, Y., and Kinny, P. D., 2002, U–Pb zircon geochronology, geochemistry and Nd isotopic study of Neoproterozoic bimodal volcanic rocks in the Kangdian Rift of South China: implications for the initial rifting of Rodinia: Precambrian Research, v. 113, p. 135–154, doi:10.1016/S0301-9268(01)00207-8.
- ↵Li X. H., Li, Z. X., Ge, W., Zhou, H., Li, W., Liu, Y., and Wingate, M. T. D., 2003, Neoproterozoic granitoids in South China: crustal melting above a mantle plume at 825 Ma?: Precambrian Research, v. 122, p. 45–83, doi:10.1016/S0301-9268(02)00207-3.
- ↵Li X. H., Li, Z. X., Sinclair, J. A., Li, W. X., and Carter, G., 2006, Revisiting the “Yanbian Terrane”: Implications for Neoproterozoic tectonic evolution of the western Yangtze Block, South China: Precambrian Research, v. 151, p. 14–30, doi:10.1016/j.precamres.2006.07.009.
- ↵Li X. H., Li, W. X., Li, Z. X., and Liu, Y., 2008, 850–790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China: A major episode of continental rift magmatism during the breakup of Rodinia: Precambrian Research.
- ↵Li Z. X., Li, X. H., Kinny, P. D., and Wang, J., 1999, The breakup of Rodinia: did it start with a mantle plume beneath South China?: Earth and Planetary Science Letters, v. 173, p. 171–181, doi:10.1016/S0012-821X(99)00240-X.
- ↵Li Z. X., Li, X. H., Kinny, P. D., Wang, J., Zhang, S., and Zhou, H., 2003, Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents: evidence for a mantle superplume that broke up Rodinia: Precambrian Research, v. 122, p. 85–109, doi:10.1016/S0301-9268(02)00208-5.
- ↵Ling W. L., Gao, S., Zhang, B. R., Zhou, L., and Xu, Q. D., 2001, The recognizing of ca. 1.95 Ga tectono-thermal event in Kongling nucleus and its significance for the evolution of Yangtze Block, South China: Chinese Science Bulletin, v. 46, p. 326–329.
- ↵Ling W. L., Gao, S., Zhang, B. R., and Li, H. M., 2003, Neoproterozoic tectonic evolution of Yangtze craton, South China: implications for amalgamation and beak-up of Rodinia Supercontinent: Precambrian Research, v. 122, p. 111–140, doi:10.1016/S0301-9268(02)00222-X.
- ↵Liu D. Y., Nutman, A. P., Compston, W., Wu, J. S., and Shen, Q. H., 1992, Remnants of >3800 Ma crust in the Chinese part of the Sino-Korean craton: Geology, v. 20, p. 339–342, doi:10.1130/0091-7613(1992)020<0339:ROMCIT>2.3.CO;2.
- ↵Liu X. M., Gao, S., Ling, W. L., Yuan, H. L., and Hu, Z. C., 2006, Identification of 3.5Ga detrital zircons from Yangtze craton in south China and the implication for Archean crust evolution: Progress in Natural Science, v. 16, p. 663–666, doi:10.1080/10020070612330050.
- ↵Ludwig K. R., 2003, ISOPLOT 3: a geochronological toolkit for Microsoft excel: Berkeley Geochronology Centre Special Publication, v. 4, 74 p.
- ↵Ma G., Li, H., and Zhang, Z., 1984, An investigation of the age limits of the Sinian System in South China: Yichang Institute of Geology and Mineral Resources Bulletin, v. 8, p. 1–29 (in Chinese with English abstract).
- ↵Maas R., Kinny, P. D., Williams, I. S., Froude, D. O., and Compston, W., 1992, The Earth's oldest known crust: A geochronological and geochemical study of 3900–4200 Ma old detrital zircons from Mt. Narryer and Jack Hills, Western Australia: Geochimica et Cosmochimica Acta, v. 56, p. 1281–1300, doi:10.1016/0016-7037(92)90062-N.
- ↵Machado N., and Simonetti, A., 2001, U–Pb dating and Hf isotopic composition of zircons by laser ablation-MC-ICP-MS, in Sylvester, P., editor, Laser-Ablation-ICPMS in the Earth Sciences: Principles, Applications: St. John's, Newfoundland, Short Course of Mineralogical Association of Canada, v. 29, p. 121–146.
- ↵McLennan S. M., 2001, Relationships between the trace element composition of sedimentary rocks and upper continental crust: Geochemistry Geophysics Geosystems, v. 2, article no. 2000GC000109.
- ↵Mojzsis S. J., Harrison, T. M., and Pidgeon, R. T., 2001, Oxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4300 Myr ago: Nature, v. 409, p. 178–181, doi:10.1038/35051557.
- ↵Nutman A. P., 2001, On the scarcity of >3900 Ma detrital zircons in 3500 Ma metasediments: Precambrian Research, v. 105, p. 93–114, doi:10.1016/S0301-9268(00)00106-6.
- ↵Qiu Y. M., Gao, S., McNaughton, N. J., Groves, D. I., and Ling, W. L., 2000, First evidence of >3.2 Ga continental crust in the Yangtze craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics: Geology, v. 28, p. 11–14, doi:10.1130/0091-7613(2000)028<0011:FEOGCC>2.0.CO;2.
- ↵Rudnick R. L., and Gao, S., 2003, Composition of the continental crust, in Rudnick, R. L. editor, The Crust: Elsevier, Treatise on Geochemistry, v. 3, p. 1–64.
- ↵Scherer E., Munker, C., and Mezger, K., 2001, Calibration of the lutetium–hafnium clock: Science, v. 293, p. 683–687, doi:10.1126/science.1061372.
- ↵
- ↵Taylor S. R., and McLennan, S. M., 1985, The Continental Crust: Its Composition and Evolution: Oxford, Blackwell, 311 p.
- ↵––––1995, The geochemical evolution of the continental crust: Reviews in Geophysics, v. 33, p. 241–265, doi:10.1029/95RG00262.
- ↵Taylor S. R., McLennan, S. M., and McCulloch, M. T., 1983, Geochemistry of loess, continental crustal composition and crustal model ages: Geochimica et Cosmochimica Acta, v. 47, p. 1897–1905, doi:10.1016/0016-7037(83)90206-5.
- ↵Thompson M. D., and Bowring, S. A., 2000, Age of the Squantum ‘tillite', Boston Basin, Massachusetts: U-Pb zircon constraints on terminal Neoproterozoic glaciation: American Journal of Science, v. 300, p. 630–655,doi:10.2475/ajs.300.8.630.
- ↵Veevers J. J., Saeed, A., Belousova, E. A., and Griffin, W. L., 2005, U–Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton: Earth and Science Reviews, v. 68, p. 245–279, doi:10.1016/j.earscirev.2004.05.005.
- ↵Vermeesch P., 2004, How many grains are needed for a provenance study?: Earth and Planetary Science Letters, v. 224, p. 441–451, doi:10.1016/j.epsl.2004.05.037.
- ↵Vervoort J. D., and Patchett, P. J., 1996, Behaviour of hafnium and neodymium isotopes in the crust: constraints from Precambrian crustally derived granites: Geochimica et Cosmochimica Acta, v. 60, p. 3717–3733, doi:10.1016/0016-7037(96)00201-3.
- ↵Wang J., and Li, Z. X., 2003, History of Neoproterozoic rift basins in South China: Implications for Rodinia break-up: Precambrian Research, v. 122, p. 141–158, doi:10.1016/S0301-9268(02)00209-7.
- ↵Watson E. B., and Harrison, T. M., 2005, Zircon thermometer reveals minimum melting conditions on earliest Earth: Science, v. 308, p. 841–844, doi:10.1126/science.1110873.
- ↵Watson E. B., Wark, D. A., and Thomas, J. B., 2006, Crystallization thermometers for zircon and rutile: Contributions to Mineralogy and Petrology, doi 10.1007/s00410-006-0068-5.
- ↵Weislogel A. L., Graham, S. A., Chang, E. Z., Wooden, J. L., Gehrels, G. E., and Yang, H., 2006, Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks: Geology, v. 34, p. 97–100, doi:10.1130/G21929.1.
- ↵Wilde S. A., Valley, J. W., Peck, W. H., and Grahams, C. M., 2001, Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago: Nature, v. 409, p. 175–178, doi:10.1038/35051550.
- ↵Woodhead J., Hergt, J., Shelley, M., Eggins, S., and Kemp, R., 2004, Zircon Hf-isotope analysis with an excimer laser, depth profiling, ablation of complex geometries, and concomitant age estimation: Chemical Geology, v. 209, p. 121–135, doi:10.1016/j.chemgeo.2004.04.026.
- ↵Wu F. Y., Zhao, G. C., Wilde, S. A., and Sun, D. Y., 2005, Nd isotopic constraints on crustal formation in the North China Craton: Journal of Asian Earth Sciences, v. 24, p. 523–545, doi:10.1016/j.jseaes.2003.10.011.
- ↵Wu F. Y., Yang, Y. H., Xie, L. W., Yang, J. H., and Xu, P., 2006a, Hf isotopic compositions of the standard zircons and baddeleyites used in U–Pb geochronology: Chemical Geology, v. 234, p. 105–126, doi:10.1016/j.chemgeo.2006.05.003.
- ↵Wu R. X., Zheng, Y. F., Wu, Y. B., Zhao, Z. F., Zhang, S. B., Liu, X. M., and Wu, F. Y., 2006b, Reworking of juvenile crust: Element and isotope evidence from Neoproterozoic granodiorite in South China: Precambrian Research, v. 146, p. 179–212, doi:10.1016/j.precamres.2006.01.012.
- ↵Xu P., Wu, F., Xie, L., and Yang, Y., 2004, Hf isotopic compositions of the standard zircons for U–Pb dating: Chinese Science Bulletin, v. 49, p. 1642–1648, doi:10.1360/04wd0128.
- ↵Yang J. H., Wu, F. Y., Zhang, Y. B., Zhang, Q., and Wilde, S. A., 2004, Identification of Mesoproterozoic zircons in a Triassic dolerite from the Liaodong Peninsula, Northeast China: Chinese Science Bulletin, v. 49, p. 1958–1962, doi:10.1360/04wd0248.
- ↵Yang J. H., Wu, F. Y., Shao, J. A., Wilde, S. A., Xie, L. W., and Liu, X. M., 2006, Constrains on the timing of the Yanshan fold and thrust belt, North China: Earth and Planetary Science Letters, v. 246, p. 336–352, doi:10.1016/j.epsl.2006.04.029.
- ↵Yuan H. L., Gao, S., Liu, X. M., Li, H. M., Günther, D., and Wu, F. Y., 2004, Accurate U–Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma mass spectrometry: Geostandards and Geoanalytical Research, v. 28, p. 353–370, doi:10.1111/j.1751-908X.2004.tb00755.x.
- ↵Zhang B. R., Gao, S., Zhang, H. F., and Han, Y. W., 2002, Geochemistry of the Qinling Orogenic Belt: Beijing, Science Press, 187 p.
- ↵Zhang S., Jiang, G., Zhang, J., Song, B., Kennedy, M. J., and Christie-Blick, N., 2005, U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in south China: Constraints on late Neoproterozoic glaciations: Geology, v. 33, p. 473–476, doi:10.1130/G21418.1.10.1130/G21418.1
- ↵Zhang S. B., Zheng, Y. F., Wu, Y. B., Zhao, Z. F., Gao, S., and Wu, F. Y., 2006a, Zircon U–Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China: Earth and Planetary Science Letters, v. 252, p. 56–71,doi:10.1016/j.epsl.2006.09.027.
- ↵––––2006b, Zircon isotope evidence for ≥3.5 Ga continental crust in the Yangtze craton of China: Precambrian Research, v. 146, p. 16–34, doi:10.1016/j.precamres.2006.01.002.
- ↵––––2006c, Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China: Precambrian Research, v. 151, p. 265–288, doi:10.1016/j.precamres.2006.08.009.
- ↵Zhao G. C., Cawood, P. A., Wilde, S. A., and Sun, M., 2000, Metamorphism of basement rocks in the Central Zone of the North China craton: implications for Paleoproterozoic tectonic evolution: Precambrian Research, v. 103, p. 55–88, doi:10.1016/S0301-9268(00)00076-0.
- ↵Zhao G. C., Wilde, S. A., Cawood, P. A., and Sun, M., 2001, Archean blocks and their boundaries in the North China craton: lithological, geochemical, structural and P–T path constraints and tectonic evolution: Precambrian Research, v. 107, p. 45–73, doi:10.1016/S0301-9268(00)00154-6.
- ↵Zhao G. C., Sun, M., Wilde, S. A., and Li, S. Z., 2005, Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited: Precambrian Research, v. 136, p. 177–202, doi:10.1016/j.precamres.2004.10.002.
- ↵Zheng J. P., Griffin, W. L., O'Reilly, S. Y., Lu, F. X., Wang, C. Y., Zhang, M., Wang, F. Z., and Li, H. M., 2004, 3.6 Ga lower crust in central China: New evidence on the assembly of the North China craton: Geology, v. 32, p. 229–232, doi:10.1130/G20133.1.
- ↵Zheng J. P., Griffin, W. L., O'Reilly, S. Y., Zhang, M., and Pearson, N., 2006, Widespread Archean basement beneath the Yangtze Craton: Geology, v. 34, p. 417–420, doi:10.1130/G22282.1.
- ↵
- Zheng Y. F., Fu, B., Gong, B., and Li, L., 2003, Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China: implications for geodynamics and fluid regime: Earth Science Reviews, v. 62, p. 105–161, doi:10.1016/S0012-8252(02)00133-2.
- ↵Zheng Y. F., Zhao, Z. F., Wu, Y. B., Zhang S. B., Liu, X. M., and Wu, F. Y., 2006, Zircon U-Pb age, Hf and O isotope constraints on protolith origin of ultrahigh-pressure eclogite and gneiss in the Dabie orogen: Chemical Geology, v. 231, p. 135–158, doi:10.1016/j.chemgeo.2006.01.005.
- ↵Zheng Y. F., Zhang, S. B., Zhao, Z. F., Wu, Y. B., Li, X. H, Li, Z. X., and Wu, F. Y., 2007, Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust: Lithos, doi:10.1016/j.lithos.2006.10.003.
- ↵Zhou C., Tucker, R., Xiao, S., Peng, Z., Yuan, X., and Chen, Z., 2004, New constraints on the ages of Neoproterozoic glaciations in south China: Geology, v. 32, p. 437–440, doi:10.1130/G20286.1.
In this issue
American Journal of Science
Vol. 308, Issue 4
April 2008
Precambrian crustal growth of Yangtze Craton as revealed by detrital zircon studies
Xiaoming Liu, Shan Gao, Chunrong Diwu, Wenli Ling
American Journal of Science Apr 2008, 308 (4) 421-468; DOI: 10.2475/04.2008.02
Jump to section
Related Articles
- No related articles found.
Cited By...
- A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formation: age constraint on the Weng'an biota
- Neoproterozoic backarc basin on the southeastern margin of the Yangtze block during Rodinia assembly: New evidence from provenance of detrital zircons and geochemistry of mafic rocks
- Continental igneous rock composition: A major control of past global chemical weathering
- The oldest crust in the Ukrainian Shield - Eoarchaean U-Pb ages and Hf-Nd constraints from enderbites and metasediments
- Intracontinental Eocene-Oligocene Porphyry Cu Mineral Systems of Yunnan, Western Yangtze Craton, China: Compositional Characteristics, Sources, and Implications for Continental Collision Metallogeny
- Detrital zircon evidence for the linkage of the South China block with Gondwanaland in early Palaeozoic time
- An Early Mesozoic transcontinental palaeoriver in South China: evidence from detrital zircon U-Pb geochronology and Hf isotopes
- Age and growth of the Archean Kongling terrain, South China, with emphasis on 3.3 ga granitoid gneisses
- Evolution of the Archaean Karelian Province in the Fennoscandian Shield in the light of U-Pb zircon ages and Sm-Nd and Lu-Hf isotope systematics
- Detrital zircon provenance from three turbidite depocenters of the Middle-Upper Triassic Songpan-Ganzi complex, central China: Record of collisional tectonics, erosional exhumation, and sediment production
- Permian-Triassic (260-220 Ma) crustal growth of Eastern Central Asian orogenic belt as revealed by detrital zircon studies