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    长江中下游地区白垩纪富碱火山岩浆作用

    禹尧 徐夕生

    禹尧, 徐夕生, 2009. 长江中下游地区白垩纪富碱火山岩浆作用. 地球科学, 34(1): 105-116.
    引用本文: 禹尧, 徐夕生, 2009. 长江中下游地区白垩纪富碱火山岩浆作用. 地球科学, 34(1): 105-116.
    YU Yao, XU Xi-sheng, 2009. Cretaceous Alkali-Rich Magmatism in the Middle and Lower Reaches of the Yangtze River. Earth Science, 34(1): 105-116.
    Citation: YU Yao, XU Xi-sheng, 2009. Cretaceous Alkali-Rich Magmatism in the Middle and Lower Reaches of the Yangtze River. Earth Science, 34(1): 105-116.

    长江中下游地区白垩纪富碱火山岩浆作用

    基金项目: 

    国家自然科学基金项目 40730313

    国家重点基础研究发展规划项目 2006CB403508

    详细信息
      作者简介:

      禹尧(1985—).女.硕士研究生.岩石学专业

      通讯作者:

      徐夕生, E-mail: xsxu@nju.edu.cn

    • 中图分类号: P588

    Cretaceous Alkali-Rich Magmatism in the Middle and Lower Reaches of the Yangtze River

    • 摘要: 根据长江中下游地区中生代火山岩与成矿作用的研究现状, 选择研究工作较为薄弱的、最东端的溧水盆地火山岩为研究对象, 进行了详细的锆石U-Pb同位素分析, 并结合本区4个不同中生代火山盆地火山岩地球化学、岩性地层学资料, 对各盆地中4个火山旋回的火山岩进行了对比研究.研究表明: 溧水盆地龙王山组粗面岩的结晶年龄为128Ma, 这标志着长江中下游地区由西向东中生代火山作用的全面展开.4个火山旋回的时代分别为: > 125Ma、125~120Ma、120~110Ma和110~90Ma.庐枞盆地的浮山组与宁芜盆地的姑山组+娘娘山组(即溧水盆地的观山组+甲山组) 对应较为恰当, 应属第三火山旋回.本区白垩世火山岩的地球化学特征, 反映这些幔源碱性岩浆在上升过程中受到了陆壳物质的混染, 早期火山岩(如溧水盆地龙王山组) 则是Sr矿的矿源层.

       

    • 图  1  长江中下游地区晚中生代火山岩盆地分布示意图(据倪若水等, 1998修改)

      Fig.  1.  Sketch map showing distributions of Late Mesozoic volcanic basins in the middle-lower Yangtze area

      图  2  溧水盆地地质简图(a) (据常州幅1∶20万地质图修改); (b) 为溧水盆地中生代火山岩岩性柱状图(据江苏省及上海市区域地质志, 1984); (c) 为采样剖面图

      Fig.  2.  Geological sketch map of the Lishui basin

      图  3  溧水盆地龙王山组粗面岩中代表性锆石的CL图像

      Fig.  3.  Cathodoluminescence (CL) images of representative zircons from trachyte of the Longwangshan Formation, Lishui basin

      图  4  溧水盆地龙王山组粗面岩中锆石谐和曲线图解

      Fig.  4.  Zircon U-Pb concordia diagram for trachyte from the Longwangshan Formation of Lishui basin

      图  5  长江中下游地区白垩纪各火山岩盆地火山岩年龄分布图

      图中溧水盆地火山岩年龄128 Ma来自本文; 其他数据来源: 宁芜项目编写小组, 1978; Wang and McDongau, 1980; 中科院地质研究所火山岩组, 1980;胡华光等, 1982; 李坤英, 1982; 吴利仁, 1984; McKee, 1988; 周金城等, 1994; 岳文浙等, 1999; 刘洪等, 2002; 张旗等, 2003; 楼亚儿和杜杨松, 2006

      Fig.  5.  Distribution diagram of the ages of Cretaceous volcanics from separated basins in the middle-lower Yangtze area

      图  6  (a) 长江中下游地区白垩纪各盆地火山岩的K2O-SiO2图解(Peccerillo and Taylor, 1976); (b) K2O-Na2O图解(Turner et al., 1996)

      图中实心点代表各盆地龙王山组火山岩, 空心点则为各盆地其他旋回的火山岩.数据来源: 溧水盆地据李超文等, 2004高晓峰等(2007); 宁芜盆地据王元龙等, 2001;繁昌盆地据常常印佛等, 1991;庐枞盆地据刘洪等, 2002

      Fig.  6.  Composition of Cretaceous volcanics from separated basins in the middle-lower Yangtze area plotted in K2O vs. SiO2 (a) and K2O vs. Na2O (b) variation diagram

      图  7  长江中下游地区白垩纪各盆地火山岩Harker图解

      数据来源: 溧水盆地据李超文等, 2004高晓峰等(2007); 宁芜盆地据王元龙等, 2001; 繁昌盆地据常印佛等(1991); 庐枞盆地据刘洪等, 2002

      Fig.  7.  Harker diagrams of major elements of Cretaceous volcanics from separated basins in the middle-lower Yangtze area

      图  8  长江中下游地区白垩纪各盆地火山岩稀土配分曲线(球粒陨石标准值引自Taylor and McLennan (1985)

      图中黑色实线代表各盆地中龙王山组(或相当于龙王山组) 火山岩, 阴影部分代表后继其他组火山岩.数据来源: 溧水盆地据李超文等, 2004高晓峰等(2007); 宁芜盆地据王元龙等, 2001;庐枞盆地据刘洪等, 2002

      Fig.  8.  Chondrite-normalized REE pattern diagram for Cretaceous volcanics from separated basins in the middle-lower Yangtze area

      图  9  火山岩微量元素原始地幔归一化蛛网图解

      图中(a) 庐枞盆地; (b) 宁芜盆地; (c) 溧水盆地.原始地幔标准值引自McDonough and Sun (1995); 黑色实线代表各盆地中龙王山组(或相当于龙王山组) 火山岩, 阴影部分代表后继其他组火山岩.数据来源: 溧水盆地据李超文等(2004)高晓峰等(2007); 宁芜盆地据王元龙等(2001); 庐枞盆地据刘洪等(2002)

      Fig.  9.  Primitive mantle-normalized trace element diagram for Cretaceous volcanics

      表  1  溧水盆地龙王山组粗面岩中错石LA-ICPMS定年结果

      Table  1.   LA-ICPMS U-Pb data of zircons in the trachytes from the Longwangshan Formation of Lishui basin

      表  2  长江中下游地区白垩纪各盆地火山岩年龄资料

      Table  2.   Age data of Cretaceous volcanics from separated basins in the middle-lower Yangtze area

      表  3  长江中下游地区4个火山岩盆地火山岩系对比

      Table  3.   Comparisons of volcanic rock series from four separated basins in the middle-lower Yangtze area

    • Andersen, T., 2002. Correction of common Pb in U-Pb analyses that do not report 204Pb. Chemical Geology, 192: 59-79. doi: 10.1016/S0009-2541(02)00195-X
      Arndt, N., Christensen, U., 1992. The role of lithospheric mantle in continental flood volcanism: Thermal and geochemical constraints. Journal of Geophysical Research, 97 (B7): 10967-10981. doi: 10.1029/92JB00564
      Bonin, B., 2004. Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting, mantle and crustal, sources? A review. Lithos, 78 (1-2): 1-24. doi: 10.1016/j.lithos.2004.04.042
      Bowring, S. A., Housh, T., 1995. The earth's early evolution. Science, 269 (5230): 1535-1540. doi: 10.1126/science.7667634
      Briqueu, L., Bougault, H., Joron, J. L., et al., 1984. Quantification of Nb, Ta, Ti and V anomalies in magmas associated with subduction zones: Petrogenetic implications. Earth and Planetary Science Letters, 68 (2): 297-308. doi: 10.1016/0012-821X(84)90161-4
      Chang, Y. F., Liu, X. P., Wu, Y. C., 1991. The copper-iron belt of the lower and middle reaches of the Changjiang River. Geological Publishing House, Beijing (in Chinese).
      Compiling Group of Ningwu Research Project, 1978. Porphyrite iron deposits of Ningwu area. Geological Publishing House, Beijing (in Chinese).
      Coward, M. P., Dewey, J. F., Hancock, P. L., et al., 1987. Continental extensional tectonics. Geological Society Special Publication, London.
      Gao, X. F., Guo, F., Li, C. W., et al., 2007. The genesis of two types of Late Mesozoic intermediate-felsic volcanic rocks in Lishui basin, lower Yangtze valley. Acta Petrologica et Mineralogica, 26 (1): 1-12 (in Chinese with English abstract).
      Hanchar, J. M., Miller, C. F., Wooden, J. L., et al., 1994. Evidence from xenoliths for a dynamic lower crust, eastern Mojave desert, California. Journal of Petrology, 35 (5): 1377-1415. doi: 10.1093/petrology/35.5.1377
      Hu, H. G., Hu, S. L., Wang, S. S., et al., 1982. On the ages of Jurassic and Cretaceous volcanic rocks by the radiometric dating. Acta Geologica Sinica, 56 (4): 315-323 (in Chinese with English abstract).
      Huang, Z. L., Cui, N. F., Leng, S. Q., et al., 1984. Geochemistry and origin of the Lishui strontium deposit. Journal of Wuhan Institute of Chemcial Technology, 16 (4): 60-65 (in Chinese with English abstract).
      Jackson, S. E., Pearson, N. J., Griffin, W. L., et al., 2004. The application of laser ablation-inductively coupled plasma-mass spectrometry (LAM-ICP-MS) to in situ U-Pb zircon geochronology. Chemical Geology, 11: 47-69.
      Jiangsu Provincial Bureau of Geology and Mineral Resources, 1984. Regional geology of Jiangsu Province and Shanghai City. Geological Publishing House, Beijing (in Chinese).
      Li, C. W., Guo, F., Li, X. Y., 2004. Petrogenesis and geodynamic implications of Late Mesozoic mafic volcanic rocks from the Lishui basin of the Lower Yangtze region. Geochimica, 33 (4): 361-371 (in Chinese with English abstract).
      Li, K. Y., 1982. The radiometric age, evolution in time and space, and primitive source of Mesozoic volcanics, Southeast China. Bulletin of the Nanjing Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 3: 98-118 (in Chinese).
      Li, X. H., 2000. Cretaceous magmatism and lithospheric extension in Southeast China. Journal of Asian Earth Sciences, 18 (3): 293-305. doi: 10.1016/S1367-9120(99)00060-7
      Li, X. H., Chen, Z., Liu, D., et al., 2003. Jurassic gabbro-granite-syenite suites from southern Jiangxi Province, SE China: Age, origin, and tectonic significance. International Geology Review, 45 (10): 898-921. doi: 10.2747/0020-6814.45.10.898
      Li, X. H., Li, W. X., Li, Z. X., 2007. On the genetic types and tectonic significance of early Yanshanian granites from Nanling. Chinese Science Bulletin, 52 (9): 981-991 (in Chinese). doi: 10.1360/csb2007-52-9-981
      Li, X. H., Zhou, H. W., Li, Z. X., et al., 2001. Zircon U-Pb age and petrochemical characteristics of the Neoproterozoic bimodal volcanics from western Yangtze block. Geochimica, 30 (4): 315-322 (in Chinese with English abstract).
      Liu, H., Qiu, J. S., Luo, Q. H., et al., 2002. Petrogenesis of the Mesozoic potash-rich volcanic rocks in the Luzong basin, Anhui Province: Geochemical constraints. Geochimica, 31 (2): 129-140 (in Chinese with English abstract).
      Lou, Y. E., Du, Y. S., 2006. Characteristics and zircon SHRIMP U-Pb ages of the Mesozoic intrusive rocks in Fanchang, Anhui Province. Geochimica, 35 (4): 359-366 (in Chinese with English abstract).
      Ludwig, K. R., 2001. Isoplot v. 2.2-a geochronological toolkit for Microsoft Excel. Special Publication No. 1a, 53, Berkeley Geochronology Center.
      Ma, F., Jiang, S. Y., Jiang, Y. H., et al., 2006. Fluid inclusions and H-O isotopic compositions in the Washan and Dongshan iron deposits, Ningwu basin, China. Acta Petrologica Sinica, 22 (10): 2581-2589 (in Chinese with English abstract).
      McDonough, W. F., Sun, S., 1995. The composition of the Earth. Chemical Geology, 120 (3-4): 223-253. doi: 10.1016/0009-2541(94)00140-4
      McKee, E. H., 1988. K-Ar chronology of the Luohe district, Anhui Province. China Economic Geology, 83: 433-435. doi: 10.2113/gsecongeo.83.2.433
      Ni, R. S., Wu, Q. C., Yue, W. Z., et al., 1998. The evolution and mineralization of terrestrial basins from the Lower Yangtze region. Shanghai Science and Technology Literature Publishing House, Shanghai (in Chinese).
      Peccerillo, A., Taylor, S. R., 1976. Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey. Contributions to Mineralogy and Petrology, 58 (1): 63-81. doi: 10.1007/BF00384745
      Qi, W. K., 1987. Discussion on regional tectonics of Anhui. Geological Science and Technology in Anhui, 1: 45-51 (in Chinese with English abstract).
      Ren, Q. J., Liu, X. S., Xu, Z. W., 1991. The Luzong Mesozoic volcanic-tectonic depression and its related metallogenesis. Geological Publishing House, Beijing (in Chinese).
      Tang, Y. C., Wu, Y. C., Chu, G. Z., et al., 1998. Polymetallic copper-gold deposit geology in the areas along the Yangtze River in Anhui Province. Geological Publishing House, Beijing (in Chinese).
      Taylor, S. R., McLennan, S., 1985. The continental crust: Its composition and evolution. Blackwell Scientific Publications, Oxford.
      Turner, S., Arnaud, N., Liu, J., et al., 1996. Post-collision, shoshonitic volcanism on the Tibetan Plateau: Implications for convective thinning of the lithosphere and the source of ocean island basalts. Journal of Petrology, 37 (1): 45-71. doi: 10.1093/petrology/37.1.45
      Van Achterbergh, E., Ryan, C. G., Jackson, S. E., et al., 2001. Data reduction software for LA-ICP-MS: Appendix. In: Sylvester, P. J., eds., Laser ablation-ICP-mass spectrometry in the earth sciences: Principles and applications. Mineralogy Association of Canada, Ottavoa, Canada, 239-243.
      Vervoort, J. D., Patchett, P. J., Gehrels, G. E., et al., 1996. Constraints on early earth differentiation from hafnium and neodymium isotopes. Nature, 379 (6566): 624-627. doi: 10.1038/379624a0
      Volcanics Group, Institute of Geology, Chinese Academy of Sciences, 1980. Multi-cycle and lateral distribution of Mesozoic volcanic rocks in several lower reaches of the Yangtze river region. In: International geological academic symposium. Geological Publishing House, Beijing, 108-115 (in Chinese).
      Wang, S. S., McDougall, I., 1980. K-Ar and 39Ar/40Ar ages on Mesozoic volcanic rocks from the lower Yangtze volcanic zone, southeastern China. Geol. Soc. Australia, 27: 121-128. doi: 10.1080/00167618008729127
      Wang, Y. L., Zhang, Q., Wang, Y., 2001. Geochemical characteristics of volcanic rocks from Ningwu area, and its significance. Acta Petrologica Sinica, 17 (4): 565-575 (in Chinese with English abstract).
      Wu, F. Y., Lin, J. Q., Wilde, S. A., et al., 2005. Nature and significance of the Early Cretaceous giant igneous event in eastern China. Earth and Planetary Science Letters, 233 (1-2): 103-119. doi: 10.1016/j.epsl.2005.02.019
      Wu, L. R., 1984. Meso-Cenozoic volcanic rocks in eastern China and adjacent areas. Geological Publishing House, Beijing (in Chinese).
      Xie, X., Xu, X. S., Zou, H. B., et al., 2001. Trace element and Nd-Sr-Pb isotope studies of Mesozoic and Cenozoic basalts in coastal area of SE China. Acta Petrologica Sinica, 17 (4): 617-628 (in Chinese with English abstract).
      Yu, J. J., Mao, J. W., Zhang, C. Q., et al., 2007. Mantle fluids involved in metallogenesis of Ningwu porphyry iron deposits: Evidence of C, Sr isotopes. Progress in Natural Science, 17 (9): 1216-1221 (in Chinese with English abstract).
      Yue, W. Z., Ding, B. L., 1999. Study on Cretaceous stratigraphic sequence of continental basin in Jiangsu. Resources Survey and Environment, 20: 287-344 (in Chinese with English abstract).
      Zhang, Q., Jian, P., Liu, D. Y., et al., 2003. Zircon SHRIMP dating of volcanic rocks from Ningwu area, and its significance. Science in China (Ser. D), 33 (4): 309-314 (in Chinese).
      Zhao, T. P., Zhou, J. C., Chen, K. R., et al., 1994. Classification of rock series and discussion on petrogenesis of Lishui Mesozoic volcanic complex. Journal of Nanjing University (Earth Sciences), 6 (3): 252-258 (in Chinese).
      Zhou, J. C., Zhao, T. P., Chen, K. R., et al., 1994. Analyses of tectonic setting for occurrence of Lishui Mesozoic shoshonite series and its evolutional relationship. Journal of Nanjing University (Natural Science Edition), 30 (3): 504-510 (in Chinese with English abstract).
      Zhou, X. M., Sun, T., Shen, W. Z., et al., 2006. Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: A response to tectonic evolution. Episodes, 29 (1): 26-33. doi: 10.18814/epiiugs/2006/v29i1/004
      常印佛, 刘湘培, 吴言昌, 1991. 长江中下游铜铁成矿带. 北京: 地质出版社.
      高晓峰, 郭锋, 李超文, 等, 2007. 溧水盆地两类晚中生代中酸性火山岩的岩石成因. 岩石矿物学杂志, 26 (1): 1-12. doi: 10.3969/j.issn.1000-6524.2007.01.002
      胡华光, 胡世玲, 王松山, 等, 1982. 根据同位素年龄讨论侏罗白垩纪火山岩系地层的时代. 地质学报, 56 (4): 315-323. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198204002.htm
      黄志良, 崔南方, 冷盛强, 等, 1994. 溧水锶矿成矿地球化学及矿床成因研究. 武汉化工学院学报, 16 (4): 60-65. https://www.cnki.com.cn/Article/CJFDTOTAL-WHHG404.016.htm
      江苏省地质矿产局, 1984. 江苏省及上海市区域地质志. 北京: 地质出版社.
      李超文, 郭锋, 李晓勇, 2004. 溧水盆地晚中生代基性火山岩成因与深部动力学过程探讨. 地球化学, 33 (4): 361-371. doi: 10.3321/j.issn:0379-1726.2004.04.005
      李坤英, 1982. 中国东南部中生代火山岩的同位素年龄、时间和空间演化及其原始物质来源. 南京地质矿产研究所所刊, 3: 98-118. https://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ198201005.htm
      李献华, 李武显, 李正祥, 2007. 再论南岭燕山早期花岗岩的成因类型与构造意义. 科学通报, 52 (9): 981-991. doi: 10.3321/j.issn:0023-074X.2007.09.001
      李献华, 周汉文, 李正祥, 等, 2001. 扬子块体西缘新元古代双峰式火山岩的锆石U-Pb年龄和岩石化学特征. 地球化学, 30 (4): 315-322. doi: 10.3321/j.issn:0379-1726.2001.04.003
      刘洪, 邱检生, 罗清华, 等, 2002. 安徽庐枞中生代富钾火山岩成因的地球化学制约. 地球化学, 31 (2): 129-140. doi: 10.3321/j.issn:0379-1726.2002.02.004
      楼亚儿, 杜杨松, 2006. 安徽繁昌中生代侵入岩的特征和锆石SHRIMP测年. 地球化学, 35 (4): 359-366. doi: 10.3321/j.issn:0379-1726.2006.04.003
      马芳, 蒋少涌, 姜耀辉, 等, 2006. 宁芜盆地凹山和东山铁矿床流体包裹体和氢氧同位素研究. 岩石学报, 22 (10): 2581-2589. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610018.htm
      倪若水, 吴其初, 岳文浙, 等, 1998. 长江中下游中生代陆相盆地演化与成矿作用. 上海: 上海科学技术文献出版社.
      倪若水, 吴其初, 岳文浙, 等, 1998. 长江中下游中生代陆相盆地演化与成矿作用. 上海: 上海科学技术文献出版社.
      齐文凯, 1987. 安徽区域地质构造几个问题的讨论. 安徽地质科技, 1: 45-51.
      任启江, 刘孝善, 徐兆文, 1991. 安徽庐枞中生代火山构造洼地及其成矿作用. 北京: 地质出版社.
      唐永成, 吴言昌, 储国正, 等, 1998. 安徽沿江地区铜金多金属矿床地质. 北京: 地质出版社.
      王元龙, 张旗, 王焰, 2001. 宁芜火山岩的地球化学特征及其意义. 岩石学报, 17 (4): 565-575. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200104006.htm
      吴利仁, 1984. 华东及邻区中、新生代火山岩. 北京: 科学出版社.
      谢昕, 徐夕生, 邹海波, 等, 2001. 中国东南沿海中-新生代玄武岩微量元素和Nd-Sr-Pb同位素研究. 岩石学报, 17 (4): 617-628. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200104011.htm
      余金杰, 毛景文, 张长青, 2007. 地幔流体参与宁芜玢岩铁矿成矿——碳、锶同位素证据. 自然科学进展, 17 (9): 1216-1221. doi: 10.3321/j.issn:1002-008x.2007.09.009
      岳文浙, 丁保良, 1999. 江苏白垩纪陆相层序地层研究. 资源调查与环境, 20: 287-344. https://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ199904001.htm
      张旗, 简平, 刘敦一, 等, 2003. 宁芜火山岩的锆石SHRIMP定年及其意义. 中国科学(D辑), 33 (4): 309-314. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200304002.htm
      赵太平, 周金城, 陈克荣, 等, 1994. 江苏溧水中生代火山杂岩岩系划分及成因讨论. 南京大学学报, 6 (3): 252-258.
      中国科学院地质研究所火山岩组, 1980. 长江下游若干地区中生代火山岩的多旋回和侧向分布. 国际交流地质学术论文集, 北京: 地质出版社, 108-115.
      周金城, 赵太平, 陈克荣, 1994. 溧水中生代橄榄安粗岩系的构造环境及演化关系. 南京大学学报(自然科学版), 30 (3): 504-510. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ403.018.htm
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    • 收稿日期:  2008-10-17
    • 刊出日期:  2009-01-25

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