• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 41 Issue 10
    Oct.  2016
    Turn off MathJax
    Article Contents
    Hu Rong, Li Shuangqing, Wang Wei, Chen Fukun, 2016. Source Characteristics of Tillite the Nantuo Formation in Three Gorges, Northern Yangtze Block: Evidences from Zircon Ages and Geochemical Composition. Earth Science, 41(10): 1630-1654. doi: 10.3799/dqkx.2016.121
    Citation: Hu Rong, Li Shuangqing, Wang Wei, Chen Fukun, 2016. Source Characteristics of Tillite the Nantuo Formation in Three Gorges, Northern Yangtze Block: Evidences from Zircon Ages and Geochemical Composition. Earth Science, 41(10): 1630-1654. doi: 10.3799/dqkx.2016.121

    Source Characteristics of Tillite the Nantuo Formation in Three Gorges, Northern Yangtze Block: Evidences from Zircon Ages and Geochemical Composition

    doi: 10.3799/dqkx.2016.121
    • Received Date: 2016-05-13
    • Publish Date: 2016-10-03
    • Neoproterozoic sedimentary sequences from the Yangtze block are completely developed and widely distributed. The Nantuo tillites in the Three Gorge area are glacial diamictites from the northern Yangtze block in the Nanhua period, which unconformably overlie the Neoproterozoic Huangling granites. The compositions of the Nantuo tillites are complicated, and the sedimentary time and components of source are rarely studied and remain in dispute. Zircon U-Pb dating results of the Nantuo tillite in this study yield youngest zircon age of 706±7 Ma. Combining with previous results about zircon U-Pb ages of the tuff from basal Doushantuo Formation and top of Datangpo Formation, the sedimentary ages of the Nantuo Formation are limited to 654-635 Ma, which can be equal to that of Marinoan. The peaks of zircon U-Pb age-spectrum are ~3.0 Ga, 2.5-2.3 Ga, 2.05-1.95 Ga and 900-700 Ma respectively, which indicate four crustal-reworking events in the Yangtze block. The ages of Paleoproterozoic and Archean are similar to that of the Kongling complex, meanwhile, 900-800 Ma and 800-700 Ma are the same as that of the Huangling granites nearby and the rocks from northern margin of the Yangtze block. The trace elements and isotope compositions of moraine sandstones show obvious differentiation, maybe due to the different degrees of mixture by materials from the northern margin of the Yangtze block, the Huangling granite and the Kongling Complex. Granitic conglomerates in the Nantuo tillites have different features of trace elements, low REE contents and depleted HREE. Associated with zircon U-Pb age and signature of Sr-Nd isotopes, these granitic conglomerates probably mainly came from the Huangling batholith and the Kongling Complex. The provenance characteristics of the Nantuo tillites reflect intensive rift related magma activities in the Yangtze block during the Neoproterozoic time, which causes the terrain featuring "lower in the south and higher in the north".

       

    • loading
    • Anbar, A.D., Knoll, A.H., 2002.Proterozoic Ocean Chemistry and Evolution:A Bioinorganic Bridge? Science, 297(5584):1137-1142.doi: 10.1126/science.1069651
      Andersen, T., 2002.Correction of Common Lead in U-Pb Analyses that Do Not Report 204Pb. Chemical Geology, 192(1-2):59-79.doi: 10.1016/S0009-2541(02)00195-X
      Barfod, G.H., Albarede, F., Knoll, A.H., et al., 2002.New Lu-Hf and Pb-Pb Age Constraints on the Earliest Animal Fossils. Earth and Planetary Science Letters, 201(1):203-212.doi: 10.1016/S0012-821X(02)00687-8
      Bouvier, A., Vervoort, J.D., Patchett, P.J., 2008.The Lu-Hf and Sm-Nd Isotopic Composition of CHUR:Constraints from Unequilibrated Chondrites and Implications for the Bulk Composition of Terrestrial Planets. Earth and Planetary Science Letters, 273(1-2):48-57.doi: 10.1016/j.epsl.2008.06.010
      Boynton, W.V., 1984.Cosmochemistry of the Rare Earth Elements:Meteorite Studies. Rare Earth Element Geochemistry, 19:63-114. http://inis.iaea.org/Search/search.aspx?orig_q=RN:16023201
      Chen, D.F., Dong, W.Q., Zhu, B.Q., et al., 2004.Pb-Pb Ages of Neoproterozoic Doushantuo Phosphorites in South China:Constraints on Early Metazoan Evolution and Glaciation Events. Precambrian Research, 132(1-2), 123-132.doi: 10.1016/j.precamres.2004.02.005
      Chen, F.K., Hegner, E., Todt, W., 2000.Zircon Ages and Nd Isotopic and Chemical Compositions of Othogneisses from the Black Forest, Germany:Evidence for a Cambrian Magmatic Arc. International Journal of Earth Sciences, 88:791-802. doi: 10.1007/s005310050306
      Chen, F.K., Siebel, W., Satir, M., et al., 2002.Geochronology of the Karadere Basement (NW Turkey) and Implications for the Geological Evolution of the Istanbul Zone. International Journal of Earth Sciences, 91(3):469-481.doi: 10.1007/s00531-001-0239-6
      Chen, J.F., Jahn, B.M., 1998.Crustal Evolution of Southeastern China:Nd and Sr Isotopic Evidence. Tectonophysics, 284(1-2):101-133.doi: 10.1016/S0040-1951(97)00186-8
      Chen, K., Gao, S., Wu, Y.B., et al., 2013.2.6-2.7 Ga Crustal Growth in Yangtze Craton, South China. Precambrian Research, 224:472-490.doi: 10.1016/j.precamres.2012.10.017
      Chu, X.L., Todt, W., Zhang, Q.R., et al., 2005.U-Pb Zircon Age for the Nanhua-Sinian Boundary. Chinese Science Bulletin, 50(7):716-718. doi: 10.1360/982005-155
      Condon, D., Zhu, M.Y., Bowring, S., et al., 2005.U-Pb Ages from the Neoproterozoic Doushantuo Formation, China. Science, 308(5718):95-98.doi: 10.1126/science.110776
      Crichton, J.G., Condie, K.C., 1993.Trace Elements As Source Indicators in Cratonic Sediments:A Case Study from the Early Proterozoic Libby Creek Group, Southeastern Wyoming. The Journal of Geology, 101(3):319-332. doi: 10.1086/648226
      Depaolo, D.J., 1981.A Neodymium and Strontium Isotopic Study of the Mesozoic Calc-Alkaline Granitic Batholiths of the Sierra Nevada and Peninsular Ranges, California. Journal of Geophysical Research, 86(B11):470-488. doi: 10.1029/JB086iB11p10470/pdf
      Evans, D.A., Li, Z., Kirschvink, J.L., et al., 2000.A High-Quality Mid-Neoproterozoic Paleomagnetic Pole from South China, with Implications for Ice Ages and the Breakup Configuration of Rodinia. Precambrian Research, 100(1-3):313-334.doi: 10.1016/S0301-9268(99)00079-0
      Feng, D.Y., Li, Z.C., Zhang, Z.C., 1991.Intrusive Ages and Isotopic Characteristics of Massives in the South of Huangling Granitoids. Hubei Geology, 5(2):1-12 (in Chinese with English abstract).
      Gao, F.H., Yang, Y., Wang, F., et al., 2014.Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province:Evidence from Field Geology and Detrital Zircon U-Pb Geochronology. Earth Science, 39(5):499-508(in Chinese with English abstract). https://www.researchgate.net/publication/287618885_Determination_of_the_early_Paleozoic_strata_in_eastern_Heilongjiang_Province_Evidence_from_field_geology_and_detrital_zircon_U-Pb_geochronology
      Gao, S., Ling, W.L., Qiu, Y.M., et al., 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, 63(13-14):2071-2088.doi: 10.1016/S0016-7037(99)00153-2
      Gao, S., Yang, J., Zhou,Zhou, et al., 2011.Age and Growth of the Archean Kongling Terrain, South China, with Emphasis on 3.3 Ga Granitoid Gneisses. American Journal of Science, 311(12):153-182.doi: 10.2475/02.2011.03
      Greentree, M.R., Li, Z.X., 2008.The Oldest Known Rocks in South-Western China:SHRIMP U-Pb Magmatic Crystallisation Age and Detrital Provenance Analysis of the Paleoproterozoic Dahongshan Group. Journal of Asian Earth Sciences, 33(5):289-302.doi: 10.1016/j.jseaes.2008.01.001
      Halverson, G.P., Hoffman, P.F., Schrag, D.P., et al., 2005.Toward a Neoproterozoic Composite Carbon-Isotope Record. Geological Society of America Bulletin, 117(9):1181-1207.doi: 10.1130/B25630.1
      Hu, J., Qiu, J.S., Wang, R.C., et al., 2007.Earliest Response of the Neoproterozoic Rodinia Break-up in the Northeastern Yangtze Craton:Constraints from Zircon U-Pb Geochronology and Nd Isotopes of the Gneissic Alkaline Granites in Donghai Area. Acta Petrologica Sinica, 23(6):1321-1333 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200706008.htm
      Hu, S.L., Wang, S.S., Sang, H.Q., et al., 1985.An Application of the Fast-Neutron Activation Dating Technique to Approach the Age of Early Emplacement of Jiuling Granodiorite Intrusion of Jiangxi Province. Acta Petrologica Sinica, 1(3):29-34 (in Chinese with English abstract).
      Hoffman, P.F., Kaufman, A.J., Halverson, G.P., et al., 1998.A Neoproterozoic Snowball Earth. Science, 281(5381), 1342-1346.doi: 10.1126/science.281.5381.1342
      Hoffman, P.F., 2009.Pan-Glacial—A Third State in the Climate System. Geology Today, 25(3):100-107.doi: 10.1111/j.1365-2451.2009.00716.x
      Hou, Z.H., Wang, C.X.2007.Determination of 35 Trace Elements in Geological Samples by Inductively Coupled Plasma Mass Spectrometry. Journal of University of Science and Technology of China, 37:940-944 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZKJD200708019.htm
      Jiao, W.F., Wu, Y.B., Yang, S.H., et al., 2009.The Oldest Basement Rock in the Yangtze Craton Revealed by Zircon U-Pb Age and Hf Isotope Composition. Science in China (Ser.D), (7):972-978.doi: 10.1007/s11430-009-0135-7
      Knoll, A., Xiao, S.H., 1999.On the Age of the Doushantuo Formation. Acta Micropalaeontologica Sinica, 16:225-236. https://www.researchgate.net/publication/259358982_On_the_age_of_the_Doushantuo_Formation
      Li, S.Q., Chen, F., Siebel, W., et al., 2012.Late Mesozoic Tectonic Evolution of the Songliao Basin, NE China:Evidence from Detrital Zircon Ages and Sr-Nd Isotopes. Gondwana Research, 22(S3-4):943-955.doi: 10.1016/j.gr.2012.04.002
      Li, X.H., Li, Z.X., Ge, W.C., et al., 2003a.Neoproterozoic Granitoids in South China:Crustal Melting above a Mantle Plume at ca.825 Ma? Precambrian Research, 122(S1-4):45-83.doi: 10.1016/S0301-9268(02)00207-3
      Li, X.H., Li, W.X., He, B.2012.Building of the South China Block and Its Relavance to Assembly and Breakup of Rodinia Supercontinent:Observations, Interpretations and Test. Bull Mineral Petrol. Geochem., 31(6):543-559 (in Chinese with English abstract).
      Li, Y.F., Lai, S.C., Qin, J.F., et al., 2007.Neoproterozoic Rifting of North Margin of Yangtze Block:Evidences from Geochemistry and Sr-Nd-Pb Isotopes of Bikou Volcanic Rocks. Science in China (Ser.D), 37(Suppl.1):295-306 (in Chinese with English abstract).
      Li, Y.L., Zhou, H.W., Li, X.H., et al., 2007.40Ar-39Ar Plateau Ages of Biotite and Amphibole from Tonalite of Huangling Granitoids and Their Cooling Curve. Acta Petrologica Sinica, 23(5):1067-1074 (in Chinese with English abstract).
      Li, Z.C., Wang, G.H., Zhang, Z.C., 2002.Isotopic Age Spectrum of the Huangling Granitic Batholith, Western Hubei. Geology and Mineral Resources of South China, 3:19-28 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200203003.htm
      Li, Z.X., Li, X., Kinny, P., et al., 2003b.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, 122(1-4):85-109.doi: 10.1016/S0301-9268(02)00208-5
      Liew, T.C., Hofmann, A.W., 1988.Precambrian Crustal Components, Plutonic Associations, Plate Environment of the Hercynian Fold Belt of Central Europe:Indications from a Nd and Sr Isotopic Study. Contributions to Mineralogy and Petrology, 98(2):129-138.doi: 10.1007/BF00402106
      Ling, W.L., 1996.Isotopic Geochronology and Crustal Growth of Proterozoic Basement along the Northern Margin of Yangtze Craton:Ⅰ.Houhe Group and Xixiang Group. Earth Science, 5 (in Chinese with English abstract).
      Ling, W.L., Gao, S., Zhang, B.R., Zhou, L., Zhang, H.F.1997.Early Precambrian Continental Crust Evolution at the Northern Margin of Yangtze Craton:Constrain from the Elemental and Isotopic Geochemical Study of Houhe Complex. Journal of Mineralogy and Petrology, 17(4):26-32 (in Chinese with English abstract). https://www.researchgate.net/publication/296128876_Early_Precambrian_continental_crust_evolution_at_the_northern_margin_of_Yangtze_craton_constrain_from_the_elemental_and_isotopic_geochemical_study_of_Houhe_complex
      Ling, W.L., Gao, S., Zhang, B.R., et al., 2000.Later Paleoproterozoic Tectonothermal Event and Evolution of Yangtze Craton. Chinese Science Bulletin, 45:2343-2348 (in Chinese with English abstract).
      Ling, W.L., Gao, S., Ouyang, J.P., et al., 2002.Time and Tectonic Setting of the Xixiang Group:Constraints from Zircon U-Pb Geochronology and Geochemistry. Science in China (Ser.D), 45(9):818-831.doi: 10.1007/BF02879516
      Ling, W.L., Gao, S., Zhang, B.R., et al., 2003.Neoproterozoic Tectonic Evolution of the Northwestern Yangtze Craton, South China:Implications for Amalgamation and Break-up of the Rodinia Supercontinent. Precambrian Research, 122(1):111-140.doi: 10.1016/S0301-9268(02)00222-X
      Ling, W.L., Gao, S., Cheng, J.P., et al., 2006.Neoproterozoic Magmatic Events within the Yangtze Continental Interior and along Its Northern Margin and Their Tectonic Implication:Constraint from the ELA-ICPMS U-Pb Geochronology of Zircons from the Huangling and Hannan Complexes. Acta Petrologica Sinica, 22(2):387-396 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200602011.htm
      Liu, X.M., Gao, S., Ling, W.L., et al., 2005.Evidence of 3.5 Ga Detrital Zircons in Yangtze Craton and Their Geological Significance. Progress in Natural Science, 15:1334-1337 (in Chinese with English abstract).
      Liu, X.M., Gao, S., Diwu, C.R., et al., 2008.Precambrian Crustal Growth of Yangtze Craton as Revealed by Detrital Zircon Studies. American Journal of Science, 308(4):421-468.doi: 10.2475/04.2008.02
      Ludwig, K.R., 2003.User's manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel.Geochronology Center Special Publication, Berkeley, 74.
      Ma, D.Q., Du, S.H., Xiao, Z.F., 2002.The Origin of Huangling Granite Batholith. Acta Petrologica et Mineralogica, 21(2):151-161 (in Chinese with English abstract).
      Ma, G.G., Li, H.Q., Zhang, Z.C., 1984.An Investigation of the Age Limits of the Sinian System in South China. Bulletin of Yichang Institute of Geology and Mineral Resources, 8:1-29 (in Chinese with English abstract).
      McFadden, K.A., Xiao, S.H., Zhou, C.M., et al., 2009.Quantitative Evaluation of the Biostratigraphic Distribution of Acanthomorphic Acritarchs in the Ediacaran Doushantuo Formation in the Yangtze Gorges Area, South China. Precambrian Research, 173(1-4):170-190.doi: 10.1016/j.precamres.2009.03.009
      Prudencio, M.J., Figueiredo, M.O., Cabral, J.M.P., 1989.Rare Earth Distribution and Its Correlation with Clay Mineralogy in the Clay-Sized Fraction of Cretaceous and Pliocene Sediments (Central Portugal). Clay Minerals, 24(1):67-74.doi: 10.1180/claymin.1989.024.1.06
      Qiu, Y.M., Gao, S., McNaughton, N.J., et al., 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, 28(1):11-14.doi:10.1130/0091-7613(2000)028<0011:FEOGCC>2.0.CO; 2
      Sha, Q.A., Liu, H.Y., Zhang, S.S., et al., 1963.Tillites of Nantuo Formation in East Yangtze Area. Scientia Geologica Sinic, 3:139-148 (in Chinese with English abstract).
      Sun, S.S., McDonough, W., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes. Geological Society, Special Publications, London, 42:313-345.
      Taylor, S.R., Mclennan, S.M., 1985.The Continental Crust:Its Composition and Evolution.Black-Well Scientific Publicaions, Oxford.
      Wang, J., Li, X.H., Duan, T.Z., et al., 2003.Zircon SHRIMP U-Pb Dating for the Cangshuipu Volcanic Rocks and Its Iimplications for the Lower Boundary Age of the Nanhua Strata in South China. Chinese Science Bulletin, 48(16):1663-1669.doi: 10.1360/03wd0168
      Wang, J., Li, Z.X., 2003.History of Neoproterozoic Rift Basins in South China:Implications for Rodinia Break-up. Precambrian Research, 122(1-4):141-158.doi: 10.1016/S0301-9268(02)00209-7
      Wang, M.X, Wang, C.Y., Sun, Y.L., 2013a.Mantle Source, Magma Differentiation and Sulfide Saturation of the ~637 Ma Zhouan Mafic-Ultramafic Intrusion in the Northern Margin of the Yangtze Block, Central China. Precambrian Research, 228:206-222.doi: 10.1016/j.precamres.2013.01.015
      Wang, W., Chen, F.K., Hu, R., et al., 2012.Provenance and Tectonic Setting of Neoproterozoic Sedimentary Sequences in the South China Block:Evidence from Detrital Zircon Ages and Hf-Nd Isotopes. International Journal of Earth Sciences, 101(7):1723-1744.doi: 10.1007/s00531-011-0746-z
      Wang, W., Zhou, M.F., Yan, D.P., et al., 2013b.Detrital Zircon Record of Neoproterozoic Active-Margin Sedimentation in the Eastern Jiangnan Orogen, South China. Precambrian Research, 235:1-19.doi: 10.1016/j.precamres.2013.05.013
      Wang, Y., Lu, S., Gao, Z., et al., 1981.Sinian Tillites of China. Earth's Pre-Pleistocene Glacial Record, 386:401.
      Wu, R.X., Zheng, Y.F., Wu, Y.B., et al., 2006.Reworking of Juvenile Crust:Element and Isotope Evidence from Neoproterozoic Granodiorite in South China. Precambrian Research, 146(S3-4):179-212.doi: 10.1016/j.precamres.2006.01.012
      Wu, Y.B., Chen, D.G., Xia, Q.K., et al., 2002.SIMS U-Pb Dating of Zircons in Granulite of Huangtuling from Northern Dabieshan. Acta Petrologica Sinica, 18(3):378-382 (in Chinese with English abstract).
      Wu, Y.B., Gao, S., Zhang, H.F., et al., 2012.Geochemistry and Zircon U-Pb Geochronology of Paleoproterozoic Arc Related Granitoid in the Northwestern Yangtze Block and Its Geological Implications. Precambrian Research, 200:26-37.doi: 10.1016/j.precamres.2011.12.015
      Wu, Y.B., Zheng, Y.F., Gao, S., et al., 2008.Zircon U-Pb Age and Trace Element Evidence for Paleoproterozoic Granulite-Facies Metamorphism and Archean Crustal Rocks in the Dabie Orogen. Lithos, 101(3):308-322.doi: 10.1016/j.lithos.2007.07.008
      Xiao, S.H., Bao, H.M., Wang, H.F., et al., 2004.The Neoproterozoic Quruqtagh Group in Eastern Chinese Tianshan:Evidence for a Post-Marinoan Glaciation. Precambrian Research, 130(1):1-26.doi: 10.1016/j.precamres.2003.10.013
      Xiao, S.H., McFadden, K.A., Peek, S., et al., 2012.Integrated Chemostratigraphy of the Doushantuo Formation at the Northern Xiaofenghe Section (Yangtze Gorges, South China) and Its Implication for Ediacaran Stratigraphic Correlation and Ocean Redox Models. Precambrian Research, 192-95(1), 125-141.doi: 10.1016/j.precamres.2011.10.021
      Xing, Y.S., Gao, Z.J., Wang, Z.Q., 1996.Stratigraphical Lexicon of China:Neoproterozoic.Geological Publishing House, Beijing (in Chinese with English abstract).
      Xiong, Q., Zheng, J.P., Yu, C.M., et al., 2008.Zircon U-Pb Age and Hf Isotope of Quanyishang A-Type Granite in Yichang:Signification for the Yangtze Continental Cratonization in Paleoproterozoic. Science in China Press, 53:2782-2792 (in Chinese with English abstract).
      Xu, B., Jian, P., Zheng, H.F., et al., 2005.U-Pb Zircon Geochronology and Geochemistry of Neoproterozoic Volcanic Rocks in the Tarim Block of Northwest China:Implications for the Breakup of Rodinia Supercontinent and Neoproterozoic Glaciations. Precambrian Research, 136(2):107-123.doi: 10.1016/j.precamres.2004.09.007
      Yang, J.D., Wang, Z.Z., Xue, Y.S., et al., 1997.Origin and Age of Mn Deposits of the Nantuo Formation in the Sinian System. Chinese Science Bulletin, 42(24):2072-2075.doi: 10.1007/BF02882949
      Yin, C.Y., Tang, F., Liu, Y.Q., et al., 2005.U-Pb Zircon Age from the Base of the Ediacaran Doushantuo Formation in the Yangtze Gorges, South China:Constraint on the Age of Marinoan Glaciation. Episodes, 28(1):48-49. https://www.researchgate.net/profile/Pengju_Liu/publication/268819356_U-Pb_zircon_age_from_the_base_of_the_Ediacaran_Doushantuo_Formation_in_the_Yangtze_Gorges_South_China_constraint_on_the_age_of_Marinoan_glaciation/links/5479b7350cf293e2da2b598f.pdf
      Yuan, H.H., Zhang, Z.L., Liu, W., et al., 1991.Direct Dating Method of Zircon Grains by 207Pb/206Pb. Mineral.Petrol., 11(2):72-79 (in Chinese with English abstract).
      Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry. Geostandards and Geoanalytical Research, 28:353-370. doi: 10.1111/ggr.2004.28.issue-3
      Zhang, C.J., 1990.Sedimentary Facies and Origin of Purplish Red Diamictites of Nantuo Formation (Lower Sinian) in Yunan. Journal of Chengdu College of Geology, 17(4):53-61 (in Chinese with English abstract).
      Zhang, Q.R., 1995.The Oringin of the Sinian Nantuo Formation in Yichang County, Hubei Province. Scientia Geologica Sinica, 30(2):147-152 (in Chinese with English abstract).
      Zhang, Q.R., Chu, X.L., Zhang, T.G., et al., 2002.From Global Glaciation to Snowball Earth:Recent Researches on the Neoproterozoic Glaciation Events. Geological Journal of China Universities, 8(4):473-481.
      Zhang, S.B., Zheng, Y.F., Wu, Y.B., et al., 2006a.Zircon Isotope Evidence for ≥3.5 Ga Continental Crust in the Yangtze Craton of China. Precambrian Research, 146(1-2):16-34.doi: 10.1016/j.precamres.2006.01.002
      Zhang, S.B., Zheng, Y.F., Wu, Y.B., et al., 2006b.Zircon U-Pb Age and Hf-O Isotope Evidence for Paleoproterozoic Metamorphic Event in South China. Precambrian Research, 151(3-4):265-288.doi: 10.1016/j.precamres.2006.08.009
      Zhang, S.B., Zheng, Y.F., Wu, Y.B., et al., 2006c.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, 252(1-2):56-71.doi: 10.1016/j.epsl.2006.09.027
      Zhang, S.B., Zheng, Y.F., Zhao, Z.F., et al., 2008a.Neoproterozoic Anatexis of Archean Lithosphere:Geochemical Evidence from Felsic to Mafic Intrusions at Xiaofeng in the Yangtze Gorge, South China. Precambrian Research, 163(3):210-238.doi: 10.1016/j.precamres.2007.12.003
      Zhang, S.B., Zheng, Y.F., Zhao, Z.F., et al., 2009.Origin of TTG-Like Rocks from Anatexis of Ancient Lower Crust:Geochemical Evidence from Neoproterozoic Granitoids in South China. Lithos, 113(3):347-368.doi: 10.1016/j.lithos.2009.04.024
      Zhang, S.H., Jiang, G.Q., Zhang, J.M., et al., 2005.U-Pb Sensitive High-Resolution Ion Microprobe Ages from the Doushantuo Formation in South China:Constraints on Late Neoproterozoic Glaciations. Geology, 33:473-476. doi: 10.1130/G21418.1
      Zhang, S.H, Jiang, G.Q., Han, Y.G., 2008b.The Age of the Nantuo Formation and Nantuo Glaciation in South China. Terra Nova, 20(4):289-294.doi: 10.1111/j.1365-3121.2008.00819.x
      Zhao, G.C., Sun, M., Wilde, S.A., et al., 2003.Assembly, Accretion and Breakup of the Paleo-Mesoproterozoic Columbia Supercontinent:Records in the North China Craton. Gondwana Research, 6:417-434. doi: 10.1016/S1342-937X(05)70996-5
      Zhao, G.C., Sun, M., Wilde, S.A., et al., 2004.A Paleo-Mesoproterozoic Supercontinent:Assembly, Growth and Breakup. Earth-Science Reviews, 67:91-123. doi: 10.1016/j.earscirev.2004.02.003
      Zhao, G.C., Cawood, P.A., 2012.Precambrian Geology of China. Precambrian Research, 222-223, 13-54.
      Zhao, J.H., Zhou, M.F., 2008.Neoproterozoic Adakitic Plutons in the Northern Margin of the Yangtze Block, China:Partial Melting of a Thickened Lower Crust and Implications for Secular Crustal Evolution. Lithos, 104:231-248. doi: 10.1016/j.lithos.2007.12.009
      Zhao, J.H., Zhou, M.F., Zheng, J.P., 2013.Neoproterozoic High-K Granites Produced by Melting of Newly Formed Mafic Crust in the Huangling Region, South China. Precambrian Research, 233:93-107. doi: 10.1016/j.precamres.2013.04.011
      Zhao, Z.Q., Xing, Y.S., Ma, G.G., Yu, W., Wang, Z.Q., 1980.Subdivision and Correlation of the Upper Precambrian in China.Tianjin Science and Technology Publishing House, Tianjin, 29-53 (in Chinese with English abstract).
      Zheng, J., Griffin, W., O'Reilly, S.Y., Zhang, M., Pearson, N., Pan, Y., 2006a.Widespread Archean Basement Beneath the Yangtze Craton. Geology, 34:417-420. doi: 10.1130/G22282.1
      Zheng, Y.F., 2003.Neoproterozoic Magmatic Activity and Global Change. Chinese Science Bulletin, 48(16):1639-1656 (in Chinese with English abstract). doi: 10.1360/03wd0342
      Zheng, Y.F., Fu, B., Gong, B., 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, 62:105-161. doi: 10.1016/S0012-8252(02)00133-2
      Zheng, Y.F., Wu, Y.B., Chen, F.K., et al., 2004.Zircon U-Pb and Oxygen Isotope Evidence for a Large-Scale 18O Depletion Event in Igneous Rocks during the Neoproterozoic. Geochimica et Cosmochimica Acta, 68:4145-4165. doi: 10.1016/j.gca.2004.01.007
      Zheng, Y.F., Zhao, Z.F., Wu, Y.B., et al., 2006b.Zircon U-Pb Age, Hf and O Isotope Constraints on Protolith Origin of Ultrahigh-Pressure Eclogite and Gneiss in the Dabie Orogen. Chemical Geology, 231:135-158. doi: 10.1016/j.chemgeo.2006.01.005
      Zheng, Y.F., Zhang, S.B.2007.Formation and Evolution of Precambrian Continental Crust in South China. Chinese Science Bulletin, 52(1):1-12 (in Chinese with English abstract). doi: 10.1007/s11434-007-0015-5
      Zheng, Y.F., Zhang, S.B., Zhao, Z.F., et al., 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, 96:127-150. doi: 10.1016/j.lithos.2006.10.003
      Zheng, Y.F., Xiao, W.J., Zhao, G., 2013.Introduction to Tectonics of China. Gondwana Research, 23:1189-1206. doi: 10.1016/j.gr.2012.10.001
      Zhou, C., Tucker, R., Xiao, S., et al., 2004.New Constraints on the Ages of Neoproterozoic Glaciations in South China. Geology, 32:437-440. doi: 10.1130/G20286.1
      Zhou, M.F., Kennedy, A.K., Sun, M., et al., 2002a.Neoproterozoic Arc-Related Mafic Intrusions along the Northern Margin of South China:Implications for the Accretion of Rodinia. J.Geol., 110:611-618. doi: 10.1086/341762
      Zhou, M.F., Yan, D.P., Kennedy, A.K., et al., 2002b.SHRIMP U-Pb Zircon Geochronological and Geochemical Evidence for Neoproterozoic Arc-Magmatism along the Western Margin of the Yangtze Block, South China. Earth and Planetary Science Letters, 196:51-67. doi: 10.1016/S0012-821X(01)00595-7
      Zhou, M., Ma, Y., Yan, D., et al., 2006b.The Yanbian Terrane (Southern Sichuan Province, SW China):A Neoproterozoic Arc Assemblage in the Western Margin of the Yangtze Block. Precambrian Research, 144:19-38. doi: 10.1016/j.precamres.2005.11.002
      Zhou, M.F., Zhao, X.F., Chen, W.T., et al., 2014.Proterozoic Fe-Cu Metallogeny and Supercontinental Cycles of the Southwestern Yangtze Block, Southern China and Northern Vietnam. Earth-Science Reviews, 139:59-82. doi: 10.1016/j.earscirev.2014.08.013
      Zhu, X.Y., Chen, F., Li, S.Q., et al., 2011.Crustal Evolution of the North Qinling Terrain of the Qinling Orogen, China:Evidence from Detrital Zircon U-Pb Ages and Hf Isotopic Composition. Gondwana Research, 20:194-204. doi: 10.1016/j.gr.2010.12.009
      冯定犹, 李志昌, 张自超, 1991.黄陵花岗岩类岩基南部岩体侵入时代和同位素特征.资源环境与工程, (2):1-12. http://www.cnki.com.cn/Article/CJFDTOTAL-HBDK199102000.htm
      胡建, 邱检生, 王汝成, 等, 2007.新元古代Rodinia超大陆裂解事件在扬子北东缘的最初响应:东海片麻状碱性花岗岩的锆石U-Pb年代学Nd同位素制约.岩石学报, 23(6):1321-1333. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200706008.htm
      胡世玲, 王松山, 桑海清, 等, 1985.应用40Ar/39Ar快中子活化定年技术探讨江西九岭花岗闪长岩体的早期侵位时代.岩石学报, 1(3):29-34.
      高福红, 杨扬, 王枫, 等, 2014.黑龙江省东部早古生代地层的确定:地质与碎屑锆石U-Pb年代学证据.地球科学, 39(5):499-508. http://earth-science.net/WebPage/Article.aspx?id=2859
      侯振辉, 王晨香, 2007.电感耦合等离子体质谱法测定地质样品中35种微量元素.中国科学技术大学学报, 37(8): 940-944. http://www.cnki.com.cn/Article/CJFDTOTAL-ZKJD200708019.htm
      焦文放, 吴元保, 彭敏, 等, 2009.扬子板块最古老岩石的锆石U-Pb年龄和Hf同位素组成.中国科学(D辑), (7):972-978. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907009.htm
      凌文黎, 1996.扬子克拉通北缘元古宙基底同位素地质年代学和地壳增生历史:Ⅰ.后河群和西乡群.地球科学, 21(5): 491-494. http://earth-science.net/WebPage/Article.aspx?id=409
      凌文黎, 高山, 张本仁, 等, 1997.扬子克拉通北缘早前寒武纪地壳演化—后河杂岩元素和同位素地球化学限制.矿物岩石, 17(4): 26-32. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS704.004.htm
      凌文黎, 高山, 张本仁, 等, 2000.扬子陆核古元古代晚期构造热事件与扬子克拉通演化.科学通报, 45(4): 2343-2348. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200021018.htm
      凌文黎, 高山, 程建萍, 等, 2006.扬子陆核与陆缘新元古代岩浆事件对比及其构造意义——来自黄陵和汉南侵入杂岩ELA-ICPMS锆石U-Pb同位素年代学的约束.岩石学报, 22(2): 387-396. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200602011.htm
      李献华, 李武显, 何斌, 2012.华南陆块的形成与Rodinia超大陆聚合-裂解—观察, 解释与检验.矿物岩石地球化学通报, 31(6): 543-559. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201206001.htm
      柳小明, 高山, 凌文黎, 等, 2005.扬子克拉通35亿年碎屑锆石的发现及其地质意义.自然科学进展, 15(11):1334-1337. doi: 10.3321/j.issn:1002-008X.2005.11.009
      李永飞, 赖绍聪, 秦江锋, 等, 2007.碧口火山岩系地球化学特征及Sr-Nd-Pb同位素组成-晋宁期扬子北缘裂解的证据.中国科学(D辑), 37(增刊1):295-306. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2007S1031.htm
      李益龙, 周汉文, 李献华, 等, 2007.黄陵花岗岩基英云闪长岩的黑云母和角闪石40Ar-39Ar年龄及其冷却曲线.岩石学报, 23(5):1067-1074.
      李志昌, 王桂华, 张自超2002.鄂西黄陵花岗岩基同位素年龄谱.华南地质与矿产, 3:19-28. http://www.cnki.com.cn/Article/CJFDTOTAL-HNKC200203003.htm
      马大栓, 杜绍华, 肖志发, 2002.黄陵花岗岩基的成因.岩石矿物学杂志, 21(2):151-161. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200202008.htm
      马国干, 李华芹, 张自超, 1984.华南地区震旦纪时限范围的研究.宜昌地质矿产研究所所刊, 8:1-29. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198412001003.htm
      沙庆安, 刘鸿允, 张树森, 等, 1963.长江峡东区的南沱组冰碛岩.地质科学, 4(3):139-148. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX196303002.htm
      吴元保, 2002.北大别黄土岭麻粒岩锆石U-Pb离子探针定年.岩石学报, 18(3):378-382. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200203012.htm
      熊庆, 郑建平, 余淳梅, 等, 2008.宜昌圈椅埫A型花岗岩锆石U-Pb年龄和Hf同位素与扬子大陆古元古代克拉通化作用.科学通报, 53(2):2782-2792. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200822022.htm
      邢裕盛, 高振家, 王自强, 等, 1996.中国地层典:新元古界.北京:地质出版社.
      袁海华, 张志兰, 刘炜, 等, 1991.直接测定颗粒锆石207Pb/206Pb年龄的方法.矿物岩石, 11(2):72-79.
      张长俊, 1990.云南南沱组杂砾岩的成因及沉积相.成都地质学院学报, 17(4):53-61. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG199004009.htm
      张启锐, 1995.湖北省宜昌县震旦系南沱组成因的新认识.地质科学, 30(2):147-152. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX502.004.htm
      郑永飞, 2003.新元古代岩浆活动与全球变化.科学通报, 48(16):1705-1720. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200316000.htm
      郑永飞, 陈福坤, 龚冰, 等, 2003.大别-苏鲁造山带超高压变质岩原岩性质, 锆石氧同位素和U-Pb年龄证据.科学通报, 48(2):110-119. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200302001.htm
      郑永飞, 张少兵, 2007.华南前寒武纪大陆地壳的形成和演化.科学通报, 52(1):1-10. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200701000.htm
      赵自强, 邢裕盛, 马国干, 等, 1980.湖北峡东震旦系.中国震旦亚界.天津:天津科学技术出版社, 29-53.
    • 加载中

    Catalog

      通讯作者: 陈斌, bchen63@163.com
      • 1. 

        沈阳化工大学材料科学与工程学院 沈阳 110142

      1. 本站搜索
      2. 百度学术搜索
      3. 万方数据库搜索
      4. CNKI搜索

      Figures(6)  / Tables(4)

      Article views (5646) PDF downloads(83) Cited by()
      Proportional views

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return