Advanced Search
Volume 32 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(5): 487-495
Wang Guoru, Chen Hongde, Zhu Zhijun, Lin Liangbiao, Fan Yu. THE CHARACTERISTICS AND GEOLOGICAL IMPLICATIONS OF RARE EARTH ELEMENTS IN SANDSTONE OF LOWER SILURIAN XIAOHEBA FORMATION IN THE SOUTHEASTERN SICHUAN—WESTERN HUNAN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 487-495. doi: 10.11781/sysydz201005487
Citation: Wang Guoru, Chen Hongde, Zhu Zhijun, Lin Liangbiao, Fan Yu. THE CHARACTERISTICS AND GEOLOGICAL IMPLICATIONS OF RARE EARTH ELEMENTS IN SANDSTONE OF LOWER SILURIAN XIAOHEBA FORMATION IN THE SOUTHEASTERN SICHUAN—WESTERN HUNAN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 487-495. doi: 10.11781/sysydz201005487
shu

THE CHARACTERISTICS AND GEOLOGICAL IMPLICATIONS OF RARE EARTH ELEMENTS IN SANDSTONE OF LOWER SILURIAN XIAOHEBA FORMATION IN THE SOUTHEASTERN SICHUAN—WESTERN HUNAN

doi: 10.11781/sysydz201005487
  • 1.

    State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan 610059, China

  • 2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China

  • 3. College of Geosciences and Measurement Engineering, East China Institute of Technology, Fuzhou, Jiangxi 344000, China

  • Received Date: 2010-04-09
  • Rev Recd Date: 2010-08-09
  • Publish Date: 2010-10-28
    Abstract
  • By means of ICP—MS,thirty seven sandstone samples of Xiaoheba Formation have been tested,and their rare earth elements and volume of relative associated trace elements have been analyzed.It indicates that total rare earth elements are higher.LREE/HREE and LaN/YbN show that differentiations between LREE and HREE are obvious;LREE is abundant,while HREE is defective.LREE is obviously rightward heeling,while HREE is even,and Eu is obviously negative anomaly,while Ce is normal.According to characteristics of Ceanom,seawater was in an anoxic environment,while it was an oxidizing environment near the Qianzhong uplift.The geochemical characteristics of rare earth elements indicate that the provenance came from active uplifted continental margin.Research results of predecessors suggested that the provenance came from the west wing of Xuefengshan uplift in a line of Guzhang,Zhijiang,Yuanling,Huaihua area,also involved basic rocks,ultrabasic rocks,basic—intermediate effusive rocks of Neoproterozoic Banxi Group.Banxi Group also appear in Changde,Taoyuan,Anhua area.

     

    • FullText(HTML)
  • loading
    • References(38)
  • [1]
    BHATIA M R.Rare earth elements geochemistry of Australian Paleozoic graywacks and mudstones provenance and tectonic control[J].Sedimentary Geology,1985,45(1-2):97-113.
    [2]
    MCLENNAN S M.Rare earth elements in sedimentary rocks influence of provenance and sedimentary processes[J].Reviews in Mineralogy,1989,21(1):169-200.
    [3]
    杨兴莲,朱茂炎,赵元龙,等.黔东震旦系-下寒武统黑色岩系稀土元素地球化学特征[J].地质论评,2008,54(1):3-15.
    [4]
    蒋德和,杨振强,赵时久.湘中地区中奥陶统沉积岩的稀土元素地球化学[J].沉积学报,1994,12(1):106-111.
    [5]
    张廷山,陈晓慧,兰光志,等.川东南地区志留纪稀土元素分布及其地质意义[J].西南石油学院学报,1998,20(3):26-30.
    [6]
    李双建,肖开华,沃玉进,等.湘西、黔北地区志留系稀土元素地球化学特征及其地质意义[J].现代地质,2008,22(2):273-280.
    [7]
    侯伟,刘招君,王伟涛,等.黑龙江省东部绥滨坳陷下白垩统泥岩稀土元素地球化学特征[J].古地理学报,2007,9(2):207-215.
    [8]
    周炼,胡兆初,袁红林,等.扬子克拉通早奥陶世古海水地球化学特征:来自牙形石微量元素的证据[J].地球化学,2005,34(3):227-234.
    [9]
    李红敬,解习农,周炼,等.扬子地区二叠系硅质岩成因分析及沉积环境研究[J].石油实验地质,2009,31(6):564-569.
    [10]
    徐晓春,王文俊,熊亚平,等.安徽石台早寒武世黑色岩系稀土元素地球化学特征及其地质意义[J].岩石矿物学杂志,2009,28(2):118-128.
    [11]
    张沛,郑建平,张瑞生,等.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[J].沉积学报,2005,23(4):740-746.
    [12]
    刘长江,桑树勋,欧阳金宝.淄博煤田煤的稀土元素地球化学特征[J].沉积学报,2008,26(6):1028-1034.
    [13]
    孙卉,边少之,宋柏荣,等.渤海湾盆地辽河坳陷兴隆台潜山变质岩地球化学特征[J].石油实验地质,2009,31(6):602-607.
    [14]
    李军,桑树勋,林会喜,等.渤海湾盆地石炭二叠系稀土元素地球化学特征及其地质意义[J].沉积学报,2007,25(4):589-596.
    [15]
    张金亮,张鑫.塔中地区志留系砂岩元素地球化学特征与物源判别意义[J].岩石学报,2007,23(11):2990-3002.
    [16]
    陈庆春,吴智平,李伟,等.济阳坳陷稀土元素特征及其在物源对比中的应用[J].地质论评,2003,49(6):622-629.
    [17]
    刘锐娥,卫孝峰,王亚丽,等.泥质岩稀土元素地球化学特征在物源分析中的意义:以鄂尔多斯盆地上古生界为例[J].天然气地球科学,2005,23(6):788-791.
    [18]
    刘俊海,杨香华,于水,等.东海盆地丽水凹陷古新统沉积岩的稀土元素地球化学特征[J].现代地质,2003,17(4):421-427.
    [19]
    李双应,岳书仓,杨健,等.皖北新元古代刘老碑组页岩的地球化学特征及其地质意义[J].地质科学,2003,38(2):241-253.
    [20]
    邵磊,李献华,韦刚健,等.南海陆坡高速堆积物的物质来源[J].中国科学(D辑),2001,31(10):828-833.
    [21]
    杨守业,李从先.REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):164-167.
    [22]
    朱如凯,郭宏莉,何东博,等.中国西北地区石炭系泥岩稀土元素地球化学特征及其地质意义[J].地质科学,2002,16(2):130-136.
    [23]
    CULLERS R L,BASU A,SUTTNER L J.Geochemical signature of provenance in sand-size mineral in soil and stream near the tabacco roobatholith,Montana,USA[J].Chemical Geology,1988,70:335-348.
    [24]
    刘宁,樊德华,郝运轻,等.稀土元素分析方法研究及应用:以渤海湾盆地东营凹陷永安地区物源分析为例[J].石油实验地质,2009,31(4):427-432.
    [25]
    万方,许效松.川滇黔桂地区志留纪构造-岩相古地理[J].古地理学报,2003,5(2):180-186.
    [26]
    郑荣才,朱如凯,翟文亮,等.川西类前陆盆地晚三叠世须家河期构造演化及层序充填样式[J].中国地质,2008,35(2):246-255.
    [27]
    陈洪德,庞林,倪新锋,等.中上扬子地区海相油气勘探前景[J].石油实验地质,2007,29(1):13-18.
    [28]
    许国明,王国司,石国山.黔中隆起及其南北斜坡区天然气勘探前景[J].贵州地质,2008,25(2):27-31.
    [29]
    杨晓萍,张宝民,柳少波.四川盆地南部志留系碳酸盐灰泥丘成因与储集性[J].海相油气地质,2002,7(4):26-32.
    [30]
    宋文海.川东南下志留统小河坝砂岩含气地质条件论述:一个未来的勘探区块[J].天然气勘探与开发,1998,21(2):1-5.
    [31]
    王根海.中国南方海相地层油气勘探现状及建议[J].石油学报,2000,21(5):1-6.
    [32]
    王中刚,于学远,赵振华.稀土元素地球化学[M].北京:科学出版社,1989:90-93.
    [33]
    ELDERFIELD H,GREAVES M J,The rare earth elements in seawater[J].Nature,1982,296:214-219.
    [34]
    赵振华.微量元素地球化学原理[M].北京:科学出版社,1997:143-223.
    [35]
    BHATIA M R,CROOK K A W.Trace element characteristics of gyaywake and tectonic of sedimentary basins[J].Contrib Mineral Petrol,1986,92:181-193.
    [36]
    刘钟伟.湖南前寒武纪火山岩地球化学特征及产出构造环境[J].湖南地质,1994,13(3):137-146.
    [37]
    BHATIA M R.Plate tectonics and geochemical composition of sandstone[J].J Geol,1983,91(6):611-627.
    [38]
    刘岫峰.沉积岩实验室研究方法[M].北京:地质出版社,1991:213-218.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 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
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1968) PDF downloads(1182) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return