• 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

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    扬子北部三峡地区南沱组冰碛岩的物源特征:锆石年龄和地球化学证据

    胡蓉 李双庆 王伟 陈福坤

    胡蓉, 李双庆, 王伟, 陈福坤, 2016. 扬子北部三峡地区南沱组冰碛岩的物源特征:锆石年龄和地球化学证据. 地球科学, 41(10): 1630-1654. doi: 10.3799/dqkx.2016.121
    引用本文: 胡蓉, 李双庆, 王伟, 陈福坤, 2016. 扬子北部三峡地区南沱组冰碛岩的物源特征:锆石年龄和地球化学证据. 地球科学, 41(10): 1630-1654. doi: 10.3799/dqkx.2016.121
    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

    扬子北部三峡地区南沱组冰碛岩的物源特征:锆石年龄和地球化学证据

    doi: 10.3799/dqkx.2016.121
    基金项目: 

    国家自然科学基金项目 40973042

    国家自然科学基金项目 41090372

    详细信息
      作者简介:

      胡蓉(1985-),女,硕士,主要研究沉积地球化学.E-mail: rong1104@mail.ustc.edu.cn

      通讯作者:

      李双庆,E-mail: lsq@ustc.edu.cn

    • 中图分类号: P597

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

    • 摘要: 扬子陆块新元古代地层发育完整并广泛分布,三峡地区南沱组冰碛岩是扬子北部南华纪的冰成杂砾岩,不整合地覆盖在新元古代黄陵花岗岩之上.南沱组冰碛岩成分复杂,分选性差,缺乏可对比的标志,其沉积时代和物源组成研究较少且存在争议.对南沱组冰碛岩开展锆石U-Pb定年工作,得到最年轻的锆石年龄为706±7 Ma,印证了南沱组沉积时代应不早于700 Ma的说法,并可与Marinoan冰期对应.所获得锆石U-Pb年龄谱峰值主要分为~3.0 Ga,2.5~2.3 Ga,2.05~1.95 Ga和900~700 Ma,反映了扬子陆块4次地壳再造事件,其中古元古代和太古代年龄与崆岭杂岩相似,900~800 Ma和800~700 Ma的锆石年龄与附近黄陵花岗岩和扬子北缘岩体一致.冰碛砂岩的微量元素和同位素组成分异明显,可能是扬子北缘岩体、黄陵花岗岩和崆岭杂岩不同程度混合的结果.南沱组冰碛岩中包裹的花岗质砾石表现出不同的微量元素特征,具有偏低的稀土含量和亏损的重稀土组成,结合其锆石U-Pb年龄和Sr-Nd同位素特征,这些花岗质砾石主体可能来自于附近黄陵花岗岩和崆岭岩基.南沱组冰碛岩的物质组成特征反映了新元古时期,扬子地区强烈的裂谷岩浆作用所导致的北高南低的地势环境.

       

    • 图  1  研究区地质

      a.中国扬子、华夏、华北和塔里木板块的分布位置;b.三峡地区和黄陵背斜的地质简图.据McFadden et al.(2009)Xiao et al.(2012)修改

      Fig.  1.  Geology of research area

      图  2  三峡地区九龙湾南沱组典型剖面特征

      a.南沱组与莲沱组的界线;b.南沱组与陡山沱组的界线;c.南沱组;d.南沱组冰碛岩中的砾石

      Fig.  2.  Outcrop pictures of the Nantuo Formation in the Jiulongwan section

      图  3  三峡地区九龙湾剖面南沱组冰碛岩样品

      Fig.  3.  Sample of tillite of the Nantuo formation in the Jiulongwan section

      图  4  三峡地区九龙湾剖面南沱组冰碛岩锆石U-Pb年龄谐和图和直方分布图

      Fig.  4.  Zircon U-Pb concordia and histogram of zircon ages for tillite of the Nantuo formation in the Jiulongwan section

      图  5  三峡地区九龙湾剖面南沱组冰碛岩

      a.稀土元素球粒陨石标准化图解;b.微量元素原始地幔标准化蛛网图;其中黑色线条为南沱组冰碛砂岩,红色线条为南沱组被包裹的花岗质砾石,球粒陨石数据来自于Boynton(1984),原始地幔数据来自于Sun and McDonough(1989)

      Fig.  5.  Chondrite-normalized REE patterns and primitive mantle-normalized trace element patterns of the Nantuo tillite in Jiulongwan section

      图  6  三峡地区九龙湾剖面南沱组冰碛岩的Sr-Nd同位素

      崆岭杂岩,包括花岗质片麻岩和TTG岩套(Gao et al., 2011; Chen et al., 2013);黄陵花岗岩基,包括黄陵庙、三斗坪、大老岭和晓峰岩套(Zhang et al., 2008a, 2009; Zhao et al., 2013);扬子北缘,岩性包括奥长花岗岩、英云闪长岩、花岗闪长岩、混合岩、斜长角闪岩、变流纹岩和火山岩(凌文黎, 1996; 凌文黎等, 1997; Ling et al., 2003; Zhao and Zhou, 2008; 李永飞等, 2007)

      Fig.  6.  The Sr-Nd isotope compositions of tillite of the Nantuo formation in the Jiulongwan section

      表  1  扬子北部三峡地区九龙湾剖面南沱组冰碛岩样品描述

      Table  1.   Sample description of tillite of the Nantuo formation in the Jiulongwan section, northern Yangze block

      样品号 样品描述 样品位置
      NT0601 灰绿色块状冰碛含砾砂岩,含砾10%~15%,砾径为0.5~2.0 mm,次棱角状,砾石有泥质岩、花岗岩、石英等
      NT0602 粗粒黑云母二长花岗岩,冰碛岩中挑选出来的砾石,含有斜长石、钾长石、石英和少量黑云母等矿物
      NT0603 浅灰色扁圆状冰碛含砾粉砂岩,砾石含量低,砾径小,主要有石英、泥岩等
      NT0604 深灰色块状冰碛含砾砂岩,砾石含量低,主要有石英、泥岩等,有的石英砾径长达3 mm 30°46′58.7″N 111°02′01.0″E
      NT0605 灰绿色块状冰碛砂岩
      NT0607 灰色块状冰碛石英中砂岩,含有石英和绢云母等
      NT0608 深灰色扁圆状冰碛细砂岩,含有石英等
      NT0609 深灰色块状冰碛含砾粉砂岩
      NT0610 粗粒黑云母二长花岗岩,冰碛岩中挑选出来的砾石,主要矿物为石英、斜长石、钾长石和黑云母等 30°48′31.1″N 111°03′26.2″E
      NT0611 深灰色块状冰碛细砂岩,含有石英等
      NT0612 花岗质岩石,冰碛岩中挑选出来的砾石,钾长石斑晶比较大,直径长达约3 cm
      NT0613 凝灰质火山岩,含杂砾泥质岩,砾石成分复杂多样,大小不一,大至几十厘米,小至小于1 cm 30°48′31.2″N 111°03′26.0″E
      NT0614 灰绿色块状冰碛含砾砂岩,含砾15%~20%,砾径为0.5~3.0 mm,次棱角状,砾石有泥质岩、石英等
      NT0615 紫红色块状冰碛泥质砂岩
      NT0616 灰白色凝灰质火山岩
      下载: 导出CSV

      表  2  扬子北部三峡地区九龙湾剖面南沱组冰碛岩LA-ICP-MS锆石U-Pb年龄

      Table  2.   U-Pb isotope data of zircons from tillite of Nantuo formation in Jiulongwan section, northern Yangtze bloek, obtained by the LA-ICPMS technique

      表  3  扬子北部三峡地区南沱组冰碛岩全岩微量元素组成

      Table  3.   Trace-element concentrations (10-6) for tillite of the Nantuo formation in the Jiulongwan section, northern Yangtze block

      样品编号 NT0601 NT0602 NT0603 NT0604 NT0608 NT0609 NT0610 NT0611 NT0612 NT0615
      Li 13.4 16.5 12.6 9.63 24.5 24.9 12.2 9.69 12.2 23.0
      Be 0.36 4.22 0.96 0.34 0.55 1.37 3.71 0.94 1.54 1.99
      Sc 8.74 1.10 5.79 5.12 4.31 12.1 0.95 8.92 3.03 12.2
      V 14.3 3.41 9.51 17.4 24.8 73.0 12.4 41.1 27.5 70.3
      Cr 4.99 5.50 8.92 42.4 9.26 48.3 6.14 17.3 8.34 58.5
      Co 3.56 1.30 1.66 3.80 7.26 14.1 2.30 6.94 5.01 11.5
      Ni 6.85 5.19 7.81 10.9 30.4 31.2 4.10 11.4 9.34 24.1
      Cu 12.3 1.72 17.0 6.48 33.4 24.9 6.19 21.7 5.82 17.2
      Ga 18.3 22.4 14.7 6.92 13.6 19 21.0 16.3 19.1 17.1
      Rb 46.2 339 69.0 33.7 36.1 78.8 198 93.6 48.8 88.2
      Sr 196 88.3 76.6 53.3 196 67.7 125 84.9 615 115
      Y 31.7 8.73 23.9 22.1 31.6 29.3 6.41 24.6 15.1 29.6
      Zr 174 54.1 214 123 226 196 110 230 193 246
      Nb 6.01 12.1 10.8 3.86 8.03 11.2 7.87 8.20 6.52 10.9
      Cs 6.15 6.64 2.17 1.32 3.32 4.21 4.89 5.12 1.36 3.77
      Ba 622 984 372 410 2 772 729 471 320 1 141 1 280
      La 29.5 16.5 63.2 31.1 24.7 25.2 15.0 12.5 47.2 35.3
      Ce 59.8 26.0 121 49.2 51.7 50.2 27.9 28.9 83.5 70.2
      Pr 7.16 3.30 13.2 7.17 6.19 6.20 2.85 3.79 10.4 8.20
      Nd 27.8 11.2 42.3 27.2 25.0 24.6 9.83 15.7 36.6 31.2
      Sm 5.48 2.18 5.50 5.07 5.15 5.25 1.75 3.54 5.76 6.09
      Eu 1.04 0.39 1.08 1.03 1.57 1.16 0.64 0.77 1.29 1.31
      Gd 4.53 1.58 4.22 4.21 4.59 4.53 1.38 3.16 4.10 5.21
      Tb 0.70 0.22 0.54 0.62 0.73 0.74 0.17 0.56 0.50 0.82
      Dy 4.58 1.24 3.41 3.54 4.51 4.59 0.88 3.53 2.56 4.97
      Ho 1.07 0.23 0.73 0.68 0.96 0.95 0.16 0.77 0.43 1.00
      Er 3.55 0.70 2.37 1.91 2.86 2.76 0.47 2.27 1.23 2.91
      Tm 0.64 0.11 0.38 0.28 0.45 0.44 0.07 0.36 0.17 0.46
      Yb 4.80 0.73 2.58 1.86 3.04 2.88 0.45 2.41 1.15 2.96
      Lu 0.80 0.11 0.40 0.29 0.50 0.45 0.07 0.39 0.17 0.46
      Hf 4.75 2.05 5.45 2.84 5.21 4.97 3.52 5.53 4.62 6.18
      Ta 0.70 1.41 0.65 0.24 0.44 0.70 0.63 0.45 0.87 0.71
      Pb 28.0 26.7 16.2 8.17 5.37 6.09 46.0 20.6 24.5 6.57
      Th 12.5 9.05 8.67 5.89 5.66 9.97 32.6 6.38 13.2 8.63
      U 1.73 1.23 1.65 0.71 1.18 1.51 6.98 1.63 1.05 1.38
      ΣREE 150.7 64.4 260.5 133.9 131.5 129.5 61.6 78.3 194.9 170.6
      (La/Yb)N 4.4 16.2 17.6 12.0 5.8 6.3 23.9 3.7 29.4 8.6
      Eu/Eu* 0.32 0.17 0.37 0.53 0.57 0.36 0.32 0.31 0.38 0.39
      Ce/Ce* 0.95 0.78 0.95 0.75 0.97 0.93 0.93 1.02 0.86 0.94
      注:N为球粒陨石标准化后的值;Eu/Eu*=Eu/(Sm*Gd)0.5;Ce/Ce*=3Ce/(2La+Nd)(Boynton, 1984).
      下载: 导出CSV

      表  4  扬子北部三峡地区九龙湾剖面南沱组冰碛岩全岩Sr-Nd同位素组成

      Table  4.   Sr and Nd isotopic composition of whole-rock samples of tillite of the Nantuo formation in the Jiulongwan section, northern Yangtze block

      样品编号 Rb (10-6) Sr (10-6) 87Rb/86Sr 87Sr/86Sr m (10-6) 87Sr/86Sr(t) Sm (10-6) Nd (10-6) 147Sm/144Nd 143Nd/144Nd m (10-6) TDM* (Ma) TDM2+ (Ma) εNd(t)
      NT0601 46.2 196.0 0.683 0.718 511 10 0.712 327 5.48 27.8 0.119 2 0.512 098 6 1.69 1.52 -4.2
      NT0602 339.0 88.3 11.270 0.861 078 12 0.758 957 2.18 11.2 0.117 7 0.511 872 7 2.02 1.82 -8.5
      NT0603 69.0 76.6 2.611 0.725 601 11 0.701 953 5.50 42.3 0.078 6 0.511 982 5 1.32 1.45 -3.2
      NT0604 33.7 53.3 1.832 0.722 552 11 0.705 958 5.07 27.2 0.112 7 0.512 063 7 1.64 1.53 -4.4
      NT0605 23.9 351.0 0.197 0.713 709 9 0.711 924 2.83 16.1 0.106 2 0.511 634 8 2.14 2.07 -12.3
      NT0607 10.6 192.0 0.160 0.713 271 11 0.711 823 4.61 25.1 0.111 0 0.511 998 5 1.71 1.61 -5.5
      NT0608 36.1 196.0 0.533 0.713 923 11 0.709 093 5.15 25.0 0.124 5 0.512 133 6 1.73 1.51 -4.0
      NT0609 78.8 67.7 3.376 0.731 690 11 0.701 115 5.25 24.6 0.129 0 0.512 154 7 1.79 1.50 -4.0
      NT0610 198.0 125.0 4.623 0.797 533 13 0.755 657 1.75 9.83 0.107 6 0.511 103 7 2.92 2.79 -22.7
      NT0611 93.6 84.9 3.195 0.725 033 13 0.696 092 3.54 15.7 0.136 3 0.512 581 5 1.12 0.97 3.8
      NT0612 48.8 615.0 0.230 0.718 761 11 0.716 679 5.76 36.6 0.095 1 0.510 683 5 3.15 3.28 -29.9
      NT0615 88.2 115.0 2.222 0.723 575 12 0.703 445 6.09 31.2 0.118 0 0.512 081 7 1.70 1.54 -4.5
      注:Rb、Sr、Sm和Nd的含量是在ICP-MS上测量的;t为同位素比值初始值;εNd(t)的测量参数据Bouvier et al.(2008);*.单阶段模式年龄的计算据DePaolo(1981);+二阶段模式年龄据Liew and Hofmann(1988);Sr和Nd同位素组成的初始值据Condon et al.(2005)回算到635 Ma.
      下载: 导出CSV
    • 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
    图(6) / 表(4)
    计量
    • 文章访问数:  5307
    • HTML全文浏览量:  1826
    • PDF下载量:  73
    • 被引次数: 0
    出版历程
    • 收稿日期:  2016-05-13
    • 刊出日期:  2016-10-03

    目录

      /

      返回文章
      返回