黄河下游冰成滑塌与塌陷构造的研究

钟建华; 王冠民; 王夕宾; 吴孔友; 洪梅; 李勇; 倪晋仁

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黄河下游冰成滑塌与塌陷构造的研究

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁

文章导航 > 沉积学报 > 2002 > 20(2): 261-266

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 2002, 20(2): 261-266.

引用本文:

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 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.

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 2002, 20(2): 261-266.

引用本文:

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 2002, 20(2): 261-266.

Citation:

黄河下游冰成滑塌与塌陷构造的研究

1.
石油大学地球资源与环境学院山东东营 257061;
2.
中国科学院长沙大地构造研究所长沙 410013;
3.
北京大学环境科学中心北京 100871

基金项目: 国家自然科学基金项目(批准号:499972037);国家重点基础研究发展规划项目(批准号:G1999043603);山东省自然科学基金项目(批准号:Q99E01);高校博士点基金项目(20010425004)联合资助。

详细信息

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

中图分类号: P694

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文章访问数: 547
HTML全文浏览量: 12
PDF下载量: 487
被引次数: 0

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

摘要

摘要: 黄河是一条有着特殊水文、水动力、沉积环境及沉积物的河流。因此，它盛产特殊的沉积现象———冰成滑塌与塌陷构造便是其中之一。冰成滑塌与塌陷构造在黄河下游非常发育，它们主要发育在边、心滩上，有时天然堤上也有发育。它们的发育深刻地影响和改造了边、心滩的沉积景观。冰成滑塌构造是一种在沉积物从冰冻状态转向冰成状态发育的一种特殊构造，其运动学特点是以滑，即以水平运动为主，冰成滑塌构造多呈鳞片状或皱褶状。鳞片状者直径多在数十厘米；“鳞片”厚度多在十厘米左右，多由数个到十余个鳞片组成。其底界是冰冻界面；皱褶状者规模甚小，每一皱褶的宽度一般宽在一厘米以内，长十到二、三十厘米，厚二、三厘米。多由数十个微型滑塌组合成一褶皱片。在天然堤内缘有一种特殊的冰成滑塌，它们使天然堤边缘呈阶步状或沟渠状，非常引人注目。冰成塌陷构造也是一种由冰层融化所形成的特殊构造，其运动学特点是“塌”，即以垂直运动为主。冰成塌陷构造多呈多角形坑洞状。直径多在数十厘米到一、二米，大者可达十余米，深度多在十余厘米。一般成群发育。
- 冰成 /
- 滑塌 /
- 塌陷 /
- 黄河
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.
- ice-induced /
- slump /
- subsidence /
- Yellow River

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参考文献(1)

[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]

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黄河下游冰成滑塌与塌陷构造的研究

1. 石油大学地球资源与环境学院山东东营 257061;

2. 中国科学院长沙大地构造研究所长沙 410013;

3. 北京大学环境科学中心北京 100871

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

收稿日期: 2001-02-13
修回日期: 2001-07-11
刊出日期: 2002-04-10

中图分类号: P694

关键词:

冰成 /

滑塌 /

塌陷 /

黄河

摘要: 黄河是一条有着特殊水文、水动力、沉积环境及沉积物的河流。因此，它盛产特殊的沉积现象———冰成滑塌与塌陷构造便是其中之一。冰成滑塌与塌陷构造在黄河下游非常发育，它们主要发育在边、心滩上，有时天然堤上也有发育。它们的发育深刻地影响和改造了边、心滩的沉积景观。冰成滑塌构造是一种在沉积物从冰冻状态转向冰成状态发育的一种特殊构造，其运动学特点是以滑，即以水平运动为主，冰成滑塌构造多呈鳞片状或皱褶状。鳞片状者直径多在数十厘米；“鳞片”厚度多在十厘米左右，多由数个到十余个鳞片组成。其底界是冰冻界面；皱褶状者规模甚小，每一皱褶的宽度一般宽在一厘米以内，长十到二、三十厘米，厚二、三厘米。多由数十个微型滑塌组合成一褶皱片。在天然堤内缘有一种特殊的冰成滑塌，它们使天然堤边缘呈阶步状或沟渠状，非常引人注目。冰成塌陷构造也是一种由冰层融化所形成的特殊构造，其运动学特点是“塌”，即以垂直运动为主。冰成塌陷构造多呈多角形坑洞状。直径多在数十厘米到一、二米，大者可达十余米，深度多在十余厘米。一般成群发育。

English Abstract

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

Keywords:

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.

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 2002, 20(2): 261-266.

引用本文:

钟建华, 王冠民, 王夕宾, 吴孔友, 洪梅, 李勇, 倪晋仁. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报, 2002, 20(2): 261-266.

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黄河下游冰成滑塌与塌陷构造的研究

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

计量

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

计量

目录

黄河下游冰成滑塌与塌陷构造的研究

1. 石油大学地球资源与环境学院山东东营 257061;

2. 中国科学院长沙大地构造研究所长沙 410013;

3. 北京大学环境科学中心北京 100871

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

English Abstract

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

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黄河下游冰成滑塌与塌陷构造的研究

作者简介: 钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

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

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出版历程

目录

黄河下游冰成滑塌与塌陷构造的研究

1. 石油大学地球资源与环境学院 山东东营 257061; 2. 中国科学院长沙大地构造研究所 长沙 410013; 3. 北京大学环境科学中心 北京 100871

作者简介: 钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

English Abstract

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

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

1. 石油大学地球资源与环境学院山东东营 257061;

2. 中国科学院长沙大地构造研究所长沙 410013;

3. 北京大学环境科学中心北京 100871

作者简介:
钟建华,男,1958年出生,教授,博士生导师,沉积学、构造地质学

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