Advanced Search
Volume 20 Issue 2
. 
Turn off MathJax
Article Contents
Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 261-266

ZHONG JianHua, WANG GuanMin, WANG XiBin, WU KongYou, HONG Mei, LI Yong, NI JinRen. Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261-266.
Citation: ZHONG JianHua, WANG GuanMin, WANG XiBin, WU KongYou, HONG Mei, LI Yong, NI JinRen. Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261-266.
shu

Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River

  • 1.

    lnstit ute of resources and lnfor mations,China university of petroleum,Dongying Shandong 257061;

  • 2.

    Changsha lnstit ute of geotectonics,CAS,Changsha 410013;

  • 3.

    Center for environmental Sciences,peking university,Beijing 100871

  • Received Date: 2001-02-13
  • Rev Recd Date: 2001-07-11
  • Publish Date: 2002-04-10
  • The Yellow River is of special hydrology, hydodynamics, sedimentary environment and deposits, resulting in forming a lot of unusual sedimentary phenomina: one of them is ice-induced slump or subsidence structure. Ice-induced slump and subsidence structure are considerably common in the lower course of the Yellow River. They mainly develop in the point bar and/or channel bar, sometimes also in levee. Their development influences and remakes the sedimentary views of the point bar and channel bar. Ice-induced slump structure is an unusual structure that is formed in such a state that the sediment is transformed from the being frozen to being melt, and its motion is featured by sliding, mainly with horizontal motion. Those ice-induced structures developing in the point bar and/or channel bar are like scales or wrinkles. Those ones like scales composed by several to more than ten,are dozens of centimeters in diameters with the thickness of mostly ten of centimeters,and their bottom boundaries are frozen ones; and those ones like wrinkles are very small in size and each wrinkle is below one centimeter in width, ten to thirty centimeters in length and two or three centimeters in thickness. Sometimes, a specical ice-induced slump may be seen in levee and it makes the edge of levee look like steps or gullies. Also, the ice-induced subsidence structure is a kind of special structures formed by ice layer's melting and its motion feature is subsiding, mainly moving vertically. Ice-melt-induced subsidence structures have the multangylar shapes and look hole-like. Their diameters are mostly several tens of centimeters to one or two meters and the largest may amount to more than ten meters and the depth is more than ten centemeters. They often develop in groups.
  • [1] 1. Fleisher P J.Dead-ice sinks and moats: Environments of stagnant ice deposition[J].Geology,1986,14:39～42

    2. Eyles N.Late Pleistocene debris-flow deposits in large glacial lakes in British Columbia and Alaska[J].Sedimentary Geology,1987,53:33～71

    3. Flectcher C J N and Desloges J R.Sediments of ice-dammed.Self-draining Ape Lake.British Columbia[J].Canadian Journal of Earth Sciences,1987,24:1 735～1 747

    4. Liverman D G E.Sedimentation in ice-dammed Hazard Lake,YuKon[J].Canadian Journal of Earth Sciences,1987,24:1 797～1 806

    5. Eyles N and McCabe A M.The Late Devensian （《22.000 BP） Irish Sea Basin: the Sedimentary record of a collapsed sheet margin[J].Quaternary Science Reviews,1989,8:307～351

    6. Aleksis D and Martin R.Late Wisconsinan sub-glacial clastic intrusive sheets along Lake Erie bluffs,at Bradtville,Ontario,Canada[J].Sedimentary Geology,1997,（2）:225～248

    7. Fletcher C J N and siddle H J.Development of glacial （Iyn Teifi,west Wales: evidence for lake-level fluctuations at the margins of the Irish Sea ice sheet[J].Journal of the Geological Society: London,1991,155: 389～399

    8. Mccabe A M,Knight J and Mccarron G.Ice-flow stages and glacial bedforms in north central Ineland: a recond of rapid environmental change duning the last glacial termination[J].Journal of the Geology Society,1999,156: 63～72

    9. Dowdeswell J A,Whittington R J,Jernings A E,Andrews J T,Mackensen A and Marienfeld P.Anorigin for laminated glacimarine sediments through sea-ice build-up and suppressed iceberg rafting[J].Sedimentology,2000,47: 557～576

    10. Harris C,Murton J and Davies M C R.Soft-sediment deformation during thawing of ice-rich frozen soils:results of scaled.Centrifuge modeling experiments[J].Sedimentology,2000,47: 687～700

    11. Stone B D.Analysis of slump slip lines and deformation fabric in slumped Pleistocene Lake Beds[J].Jour.Sed.Petrology,1976,46: 313～325

    12. Farre J F,McGregor B A,Ryan W B F and Robb J M.Breaching the shelfbreak; passage from youthful to mature phase in submarine canyon evolution[M].In: Stantey D J and Moore G J,eds.The shelf break.Soc.Econ.Paleontol.Mineral.Spec.Publ.,1983,33: 25～39

    13. Plint A G.Slump blocks,intraformation conglomerates and associated erosional structures in Pennsylvanian fluvial strata of eastern Canada[J].Sedimentology,1986,33: 387～399

    14. Van de Poll H W,Patel I M.Slump blocks,intraformational conglomerates and associated erosional structures in Pennsulvanian fluvial strata of eastern Canada[J].Sedimentology,1989,36: 137～145

    15. Plint A G.slump blocks,intraformational Conglomerates and associated erosional structures in Pennsylvanian fluvial strata of eastern Canada[J].Sedimentology,1989,36: 145～150

    16. Tama's H.Lantos M.Au evaluation of Slump fold formation using palaeomagnetic techmques[J].Sedimentary Geology,1994,90: 233～240

    17. Thomas B R,Anne R F.A submarine slide scar and channel filled with slide blocks and megarippled Globigerina sands of possible contourite origin from the Pliocene of Sumba,Indonesia[J].Sedimentary Geology,1996,103: 145～160

    18. M.R.Gibling M R,Tandon S K.Erosional marks on consolidated banks and slunp blocks in the Rupen River,north-west India[J].Sedimentology,1997,44: 339～348

    19. 钟建华，李理。黄河断流后三角洲（水上平原）的滑塌构造研究[J].沉积学报，2000,18（1）:7～12 [Zhong Jianhua,Li Li.Study of the slump structure on the Yellow River delta during its in zero[J].Acta Sedimentologica Sinica,2000,18（1）:7～12]
  • 加载中
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
Get Citation
PDF
XML

Article Metrics

Article views(465) PDF downloads(483) Cited by()

Proportional views
Related
Publishing history
  • Received:  2001-02-13
  • Revised:  2001-07-11
  • Published:  2002-04-10

Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River

  • 1. lnstit ute of resources and lnfor mations,China university of petroleum,Dongying Shandong 257061;
  • 2. Changsha lnstit ute of geotectonics,CAS,Changsha 410013;
  • 3. Center for environmental Sciences,peking university,Beijing 100871
  • Received Date: 2001-02-13
  • Rev Recd Date: 2001-07-11
  • Publish Date: 2002-04-10

Abstract: The Yellow River is of special hydrology, hydodynamics, sedimentary environment and deposits, resulting in forming a lot of unusual sedimentary phenomina: one of them is ice-induced slump or subsidence structure. Ice-induced slump and subsidence structure are considerably common in the lower course of the Yellow River. They mainly develop in the point bar and/or channel bar, sometimes also in levee. Their development influences and remakes the sedimentary views of the point bar and channel bar. Ice-induced slump structure is an unusual structure that is formed in such a state that the sediment is transformed from the being frozen to being melt, and its motion is featured by sliding, mainly with horizontal motion. Those ice-induced structures developing in the point bar and/or channel bar are like scales or wrinkles. Those ones like scales composed by several to more than ten,are dozens of centimeters in diameters with the thickness of mostly ten of centimeters,and their bottom boundaries are frozen ones; and those ones like wrinkles are very small in size and each wrinkle is below one centimeter in width, ten to thirty centimeters in length and two or three centimeters in thickness. Sometimes, a specical ice-induced slump may be seen in levee and it makes the edge of levee look like steps or gullies. Also, the ice-induced subsidence structure is a kind of special structures formed by ice layer's melting and its motion feature is subsiding, mainly moving vertically. Ice-melt-induced subsidence structures have the multangylar shapes and look hole-like. Their diameters are mostly several tens of centimeters to one or two meters and the largest may amount to more than ten meters and the depth is more than ten centemeters. They often develop in groups.

ZHONG JianHua, WANG GuanMin, WANG XiBin, WU KongYou, HONG Mei, LI Yong, NI JinRen. Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261-266.
Citation: ZHONG JianHua, WANG GuanMin, WANG XiBin, WU KongYou, HONG Mei, LI Yong, NI JinRen. Study on the Ice-Induced Slump and Subsidence Structures in the Lower Course of Yellow River[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261-266.
shu

    HTML

Reference (1)

Catalog

    Links

    Journal Online

    Contact Us

    • Website Copyright © 2011 Editorial Office of Acta Sedimentologica Sinica
    • Address: 8 Tianshui Middle Road, Lanzhou
    • Post code: 730000   Tel:（0931）8264231
    • 陇ICP备2021001824号-28
    • 甘公网安备 62010202000673号
    Wechat

    Email alert

    RSS

    Supported by: Beijing Renhe Information Technology Co. Ltd  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return