高级搜索

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

塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景

于炳松 陈建强 李兴武 林畅松

于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景[J]. 沉积学报, 2004, 22(1): 59-66.
引用本文: 于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景[J]. 沉积学报, 2004, 22(1): 59-66.
YUBing song, CHENJian qiang, LIXing wu, LINChang song. Rare Earth and Trace Element Patterns in Bedded- cherts from the Bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China :Implication for Depositional Environments[J]. Acta Sedimentologica Sinica, 2004, 22(1): 59-66.
Citation: YUBing song, CHENJian qiang, LIXing wu, LINChang song. Rare Earth and Trace Element Patterns in Bedded- cherts from the Bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China :Implication for Depositional Environments[J]. Acta Sedimentologica Sinica, 2004, 22(1): 59-66.

塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景

基金项目: 国家自然科学基金项目(批准号:40172042);国家重大基础研究发展规划项目(编号:G1999043304);国家博士学科点专项基金项目(编号:200049107)资助
详细信息
    作者简介:

    于炳松,男,1962年出生,博士,教授,沉积学,层序地防学和地球化学

  • 中图分类号: P588.2;P595

Rare Earth and Trace Element Patterns in Bedded- cherts from the Bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China :Implication for Depositional Environments

  • 摘要: 对塔里木盆地北部肖尔布拉克寒武系露头剖面中 8.8m厚的黑色页岩夹硅质岩组合中的硅质岩的系统采样分析表明,该硅质岩具有深源成因特征。其低的Th/U和Rb/Sr比也证明了其沉积时所具有的深部物源和热水注入迹象。硅质岩的稀土元素经北美页岩标准化后的Ce/Ce 从 0.4 2到 0.79,平均 0.5 7。Ce的负异常明显。这些稀土元素的参数特征与加利福尼亚弗朗希斯科杂岩 (FranciscanComplex)中沉积在大洋海底硅质岩的稀土元素特征十分相似。北美页岩标准化后的Eu/Eu 值从 8.0 5下降到 1.0 3。其相对较高的Eu/Eu 值很有可能反映了热水的注入。Eu/Eu 值从剖面底部到顶部的系统降低反映了剖面底部的热水作用最强烈,向上热水作用逐渐减弱。上述一系列的地球化学标志指示该硅质岩应沉积在离洋中脊不远的、具有深源物质/热水注入的远洋盆地背景中。结合区域地质和伴生黑色页岩地球化学的综合分析认为,该套硅质岩的形成与上升洋流的影响有关。上升洋流将形成于大洋盆地背景中的物质带到大陆边缘陆棚环境中发生沉积,造成了沉积在陆棚环境中的硅质岩,在地球化学组成上保留了其大洋盆地背景的特征
  • [1] Murray R W. Chemical criteria to identify the depositional environment of chert: general principles and applications. Sedimentary Geology, 1994, 90: 213~232.
    [2] Murray R W, Buchholtz ten Brink M R, Jones D L, Gerlach D C and Russ G P. Rare earth elements as indicators of different marine depositional environments in chert and shale. Geology, 1990, 18: 268~271.
    [3] Murray R W, Buchholtz ten Brink M R, Gerlach D C, Russ G P and Jones D L. Rare earth, major and trace elements in chert from the Franciscan Complex and Monterey Group, California: assessing REE sources to fine-grained marine sediments. Geochimica Cosmochimica Acta, 1991, 55: 1875~1895.
    [4] Murray R W, Buchholtz ten Brink M R, Gerlach D C, and Russ G P and Jones D L. Interoceanic variation in the rare earth, major, and trace element depositional chemistry of chert: perspectives gained from the DSDP and ODP record. Geochimica et Cosmochimica Acta, 1992, 56: 1897~1913.
    [5] Fan Delian. Polyelements in the Lower Cambrian black shale series in southern China. In:Greecs S A ed. The significance of trace elements in solving petrogenetic problems and controversies. Theophrastus Publications, 1983.447~474.
    [6] Fan Delian, Yang Ruiying, Huang Zhongxiang. The Lower Cambrian black shale series and iridium anomaly in south China. In:Academia Sinica eds. Developments in geosciences, contribution to 27th IGC.Moscow, 1984.215~224.
    [7] 范德廉,叶杰,杨瑞英,等. 扬子地台前寒武纪/寒武纪界线附近的地质事件与成矿作用.沉积学报, 1987, 5: 81~95 [Fan Delian, Ye Jie, Yang Ruiying,et al. The geological events and mineralization near the boundary line of Precambrian and Cambrian in Yangtze Platform. Acta Sedimentologica Sinica, 1987, 5: 81~95]
    [8] Chen Nansheng. Lower Cambrian black rock series and associated stratiform deposits in sothern China. Chinese Journal of Geochemistry, 1990, 9: 244~255
    [9] 涂光炽. 华南元古宙基底演化与成矿作用.北京: 科学出版社, 1993 [Tu Guangzhi. The Basement Evolution and Mineralization of Proterozoic in South China. Beijing: Science Press, 1993]
    [10] 涂光炽. 低温地球化学. 北京: 科学出版社, 1998. [Tu Guangzhi. The Low Temperature Geochemistry. Beijing: Science Press, 1998]
    [11] 李胜荣,高振敏. 湘黔寒武系牛蹄塘组黑色岩系稀土元素特征-兼论海相热水沉积岩的稀土模式. 矿物学报, 1995, 15: 225~229 [Li Shengrong, Gao Zhenming. REE character of black rock series of Niutitang Formation in Hunan and Guizhou-simultaneous discussion on the REE model of hydrothermal rocks in sea facies. Acta Mineralogica Sinica, 1995, 15: 225~229]
    [12] 李胜荣,高振敏. 湘黔下寒武统黑色岩系热演化条件. 地质地球化学, 1996, 4: 30~34 [Li Shengrong, Gao Zhenming. Conditions on thermal evolution of Lower Cambrian black rock series in Hunan and Guizhou. Geology-Geochemistry, 1996,4: 30~34]
    [13] Li Shengrong Gao Zhenming. Silicalites of hydrothermal origin in the lower Cambrian black rock series of south China. Chinese Journal of Geochemistry, 1996, 15: 113~120
    [14] Li Shengrong Gao Zhenming. Source tracing of noble metal elements in Lower Cambrian black rock series of Guizhou-Hunan Provinces, China. Science in China (Series D), 2000, 43: 625~632
    [15] 于炳松,裘愉卓,李娟. 扬子地块西南部晚元古至三叠纪沉积地球化学演化.沉积学报, 1997, 15(4): 127~133 [Yu Bingsong, Qiu Yuzhuo, Li Juan. Sedimentary geochemical evolution from Upper Proterozoic to Triassic in southwest Yangtze Massif. Acta Sedimentologica Sinica, 1997, 15(4):127~133]
    [16] 于炳松,裘愉卓. 扬子地块西南部晚元古代至三叠纪稀土元素地球化学及其地壳演化. 现代地质, 1998, 12(2): 173~179 [Yu Bingsong and Qiu Yuzhuo. REE geochemistry and crustal evolution from Upper Proterozoic to Triassic in southwest Yangtze Massif. Geoscience, 1998, 12(2): 173~179]
    [17] 于炳松,乐昌硕. 沉积岩物质成分所蕴含的地球深部信息.地学前缘, 1998, 5(3): 105~112 [Yu Bingsong, Yue Changshuo. Some information about the interior of earth contained in composition of sedimentary rocks. Earth Science Frontiers, 1998, 5(3):105~112]
    [18] Yu Bingsong, Qiu Yuzhuo. The geochemistry of sedimentary rocks and its relation to crustal evolution in the southwest Yangtze Massif. Chinese Journal of Geochemistry, 1998, 17(3): 265~274
    [19] Yu Bingsong. Control of interior sources on time-bound characteristics of minerization in southwest Yangtze Massif. Journal of China University Geosciences, 1998, 10(1):80~85
    [20] Wedepohl K H. The composition of the continental crust. Geochim. Cosmochim. Acta, 1995,59: 1217~1232
    [21] McLennan S M and Taylor S R. Th and U in sedimentary rocks: crustal evolution and sedimentary recycling. Nature, 1980, 285: 621~624
    [22] McLennan S M, Taylor S R, McCulloch M T, and Maynard J B. Geochemical and Nd-Sr isotopic composition of deep-sea turbidites: Crustal evolution and plate tectonic associations. Geochimica et Cosmochimica Acta, 1990, 54: 2015~2052
    [23] McLennan S M and Taylor S R. Sedimentary rocks and crustal evolution: Tectonic setting and secular trends. Journal of Geology, 1991, 1: 1~21
    [24] Murray R W, Jones D L, and Buchholtz ten Brink M R. Diagenetic formation of bedded chert: evidence from chemistry of the chert-shale couple. Geology, 1992, 20: 271~274
    [25] Adachi M, Yamamoto K, Sugisaki. Hydrothermal chert and associated siliceous rock from the Northern Pacific: Their geological significance as indication of ocean ridge activity. Sedimentary Geology, 1986, 47: 125~148
    [26] Girty H G. Provenance and depositional setting of Paleozoic chert and argillite, Sierra Nevada, California. Journal of Sedimentary Research, 1996, 66: 107~118
    [27] Jafri S H, Balaram V and Govil P K. Depositional environments of Cretaceous radiolarian cherts from Andaman-Nicobar Islands, northeastern Indian.Ocean Marine Geology, 1993,12: 291~301
    [28] Kunzendorf K. Regional variation of REE pattern in sediments from active plate boundaries. Marine Geology, 1988, 84: 191~199
    [29] Mirchard V. Some geochemical indicators for discrimination between diagenetic and hydrothermal metalliferous sediments. Marine Geology, 1982, 50: 241~256
    [30] Michard A. Rare earth element systematics in hydrothermal fluids. Geochimica et Cosmochimica Acta, 1989, 53: 745~750
    [31] Rangin C, Steinberg M, Bonnot-Courtois C. Geochemistry of Mesozoic bedded cherts of Central Baja California (Vizcaino-Cedros-San Benito): implication for paleogeographic reconstruction of an old oceanic basin. Earth Planet Science Letter, 1981, 54: 313~322
    [32] Boynton W V. Cosmochemistry of the Rare Earth Elements. In: Henderson P ed. Rare Earth Element Geochemistry. Developments in Geochemistry 2. Elsevier, Amsterdam, 1984. 63~114
    [33] Haskin M A and Haskin L A. Rare earth in European shales: a redetermination. Science, 1966,154: 507~509
    [34] Shimizu H and Masuda A. Cerium in chert as an indication of marine environment of its formation. Nature, 1997, 266, 24: 346~348
    [35] Nagasawa H and Suwa K. Rare-earth concentrations in 3.5-billion-year-old Onverwacht cherts: An indicator for early Precambrian crustal environments. Geochemical Journal, 1986, 20: 253~260
    [36] Lottermoser B G. Rare earth element study of exhalites within the Willyama Supergroup, Broken Hill Block, Australia. Mineral. Deposita, 1989, 24: 92~99
    [37] 乐昌硕,于炳松,田成,王荣前.新疆塔里木盆地北部层序地层及其沉积学研究.北京:地质出版社,1996 [Yue Changshuo, Yu Bingsong, Tian Cheng and Wang Rongqian. Study on Sequence Stratigraphy and Sedimentology in northern Tarim Basin. Beijing: Geological Publishing House, 1996]
    [38] L ckge A, Boussafir M, Lallier-Verges E, Littke R. Comparative study of organic matter preservation in immature sediments along the continental margins of Peru and Oman. Part, Results of petrographical and bulk geochemical data. Organic Geochemistry, 1996, 24: 437~451
    [39] Bordovskiy O K. Accumulation and transformation of organic substances in marine sediments, Part and. Marine Geology,1965, 3: 3~34
    [40] Premuzic E T, Benkovitz J S, Gaffrey J S, Walsh J J. The nature and distribution of organic matter in the surface sediments of the world oceans and seas. Organic Geochemistry, 1982, 4: 63~77
    [41] Suzuki N, Ishida K, Shinomiya Y, Ishiga H. High productivity in the earliest Triassic ocean: black shales, Southwest Japan. Palaeogeography, Palaeoclimatology, Palaeoecology,1998, 141: 53~65
    [42] Ganeshram R S, Pedersen T F, Calvert S E and Francols R. Reduced nitrogen fixation in the glacial ocean inferred from changes in marine nitrogen and phosphorus inventories. Nature, 2002, 415: 156~159
  • [1] 王峰, 刘玄春, 邓秀芹, 李元昊, 田景春, 李士祥, 尤靖茜.  鄂尔多斯盆地纸坊组微量元素地球化学特征及沉积环境指示意义 . 沉积学报, 2017, 35(6): 1265-1273. doi: 10.14027/j.cnki.cjxb.2017.06.017
    [2] 孙维萍, 扈传昱, 韩正兵, 翁焕新, 陈际雨, 潘建明.  南极普里兹湾表层沉积物微量元素分布特征及其物源指示意义 . 沉积学报, 2016, 34(2): 308-314. doi: 10.14027/j.cnki.cjxb.2016.02.009
    [3] 杨程宇, 李美俊, 倪智勇, 杨福林, 陈昊卫.  塔里木盆地西北缘玉尔吐斯组硅质岩成因及石油地质意义 . 沉积学报, 2016, 34(4): 653-661. doi: 10.14027/j.cnki.cjxb.2016.04.005
    [4] 王卓卓, 施立志, 张永生, 陈代钊, 梁江平.  湘桂地区泥盆纪硅岩Rb-Sr、Sm-Nd同位素地球化学特征及构造沉积背景研究 . 沉积学报, 2015, 33(4): 679-686. doi: 10.14027/j.cnki.cjxb.2015.04.006
    [5] 辽东湾东南部海域柱状沉积物稀土元素地球化学特征与物源识别 . 沉积学报, 2014, 32(4): 684-691.
    [6] 靳建辉.  新疆伊犁塔克尔莫乎尔沙漠全新世晚期沉积微量元素反映的古气候变化 . 沉积学报, 2011, 29(2): 336-345.
    [7] 陈文彬.  羌塘盆地那底岗日地区布曲组碳酸盐岩烃源岩稀土元素分布特征及意义 . 沉积学报, 2011, 29(3): 529-536.
    [8] 常华进.  桂北泗里口老堡组硅质岩的常量、稀土元素特征及成因指示 . 沉积学报, 2010, 28(6): 1098-1107.
    [9] 刘建清.  羌塘盆地中央隆起带南侧隆额尼—昂达尔错布曲组古油藏白云岩稀土元素特征及成因意义 . 沉积学报, 2008, 26(1): 28-38.
    [10] 伊海生.  西藏高原沱沱河盆地渐新世—中新世湖相碳酸盐岩稀土元素地球化学特征与正铕异常成因初探 . 沉积学报, 2008, 26(1): 1-10.
    [11] 蔡清海.  福建三沙湾海洋沉积物中重金属和微量元素的研究 . 沉积学报, 2007, 25(3): 456-460.
    [12] 李 军.  渤海湾盆地石炭二叠系稀土元素特征及其地质意义 . 沉积学报, 2007, 25(4): 589-596.
    [13] 张沛, 郑建平, 张瑞生, 余淳梅.  塔里木盆地塔北隆起奥陶系——侏罗系泥岩稀土元素地球化学特征 . 沉积学报, 2005, 23(4): 740-746.
    [14] 解启来, 陈多福, 漆亮, 陈先沛.  贵州瓮安陡山沱组磷块岩稀土元素地球化学特征与沉积期后变化 . 沉积学报, 2003, 21(4): 627-633.
    [15] 梁华英, 王秀璋, 程景平.  粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素 . 沉积学报, 2001, 19(3): 415-420.
    [16] 余素华, 郑洪汉.  宁夏中卫长流水剖面沉积物中稀土元素及其环境意义 . 沉积学报, 1999, 17(1): 149-155.
    [17] 伊海生, 彭军, 夏文杰.  扬子东南大陆边缘晚前寒武纪古海洋演化的稀土元素记录 . 沉积学报, 1995, 13(4): 131-137.
    [18] 丁祖国, 柴之芳, 马建国, 傅家谟, 盛国英, 彭平安, 林清.  江汉油田原油和生油岩有机抽提物中过渡族微量元素特征及其石油地球化学意义 . 沉积学报, 1992, 10(1): 108-117.
    [19] 赵一阳, 王金土, 秦朝阳, 陈毓蔚, 王贤觉, 吴明清.  中国大陆架海底沉积物中的稀土元素 . 沉积学报, 1990, 8(1): 35-43.
    [20] 李成凤, 肖继风.  用微量元素研究胜利油田东营盆地沙河街组的古盐度 . 沉积学报, 1988, 6(4): 100-107.
  • 加载中
计量
  • 文章访问数:  579
  • HTML全文浏览量:  0
  • PDF下载量:  982
  • 被引次数: 0
出版历程
  • 收稿日期:  2002-09-05
  • 修回日期:  2002-11-29
  • 刊出日期:  2004-03-10

目录

    塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景

      基金项目:  国家自然科学基金项目(批准号:40172042);国家重大基础研究发展规划项目(编号:G1999043304);国家博士学科点专项基金项目(编号:200049107)资助
      作者简介:

      于炳松,男,1962年出生,博士,教授,沉积学,层序地防学和地球化学

    • 中图分类号: P588.2;P595

    摘要: 对塔里木盆地北部肖尔布拉克寒武系露头剖面中 8.8m厚的黑色页岩夹硅质岩组合中的硅质岩的系统采样分析表明,该硅质岩具有深源成因特征。其低的Th/U和Rb/Sr比也证明了其沉积时所具有的深部物源和热水注入迹象。硅质岩的稀土元素经北美页岩标准化后的Ce/Ce 从 0.4 2到 0.79,平均 0.5 7。Ce的负异常明显。这些稀土元素的参数特征与加利福尼亚弗朗希斯科杂岩 (FranciscanComplex)中沉积在大洋海底硅质岩的稀土元素特征十分相似。北美页岩标准化后的Eu/Eu 值从 8.0 5下降到 1.0 3。其相对较高的Eu/Eu 值很有可能反映了热水的注入。Eu/Eu 值从剖面底部到顶部的系统降低反映了剖面底部的热水作用最强烈,向上热水作用逐渐减弱。上述一系列的地球化学标志指示该硅质岩应沉积在离洋中脊不远的、具有深源物质/热水注入的远洋盆地背景中。结合区域地质和伴生黑色页岩地球化学的综合分析认为,该套硅质岩的形成与上升洋流的影响有关。上升洋流将形成于大洋盆地背景中的物质带到大陆边缘陆棚环境中发生沉积,造成了沉积在陆棚环境中的硅质岩,在地球化学组成上保留了其大洋盆地背景的特征

    English Abstract

    于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景[J]. 沉积学报, 2004, 22(1): 59-66.
    引用本文: 于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景[J]. 沉积学报, 2004, 22(1): 59-66.
    YUBing song, CHENJian qiang, LIXing wu, LINChang song. Rare Earth and Trace Element Patterns in Bedded- cherts from the Bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China :Implication for Depositional Environments[J]. Acta Sedimentologica Sinica, 2004, 22(1): 59-66.
    Citation: YUBing song, CHENJian qiang, LIXing wu, LINChang song. Rare Earth and Trace Element Patterns in Bedded- cherts from the Bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China :Implication for Depositional Environments[J]. Acta Sedimentologica Sinica, 2004, 22(1): 59-66.
    参考文献 (42)

    目录

      /

      返回文章
      返回

      论文重合率自检

      根据国家对期刊质量管理要求,加强学术不端风险防范,完善学术不端体系建设标准查漏补缺工作,建议各位作者在投稿前通过本站官网进行论文查重检测。目前只有万方公司对个人用户提供检测服务,作者在外部渠道查重易造成论文与成果泄漏,来稿作者可自愿使用本站万方检测系统预查重检测。

      检测链接地址:http://cjxb.wanfangtech.net