黄河三角洲变形层理的研究

钟建华; 马在平

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黄河三角洲变形层理的研究

钟建华, 马在平

文章导航 > 沉积学报 > 1998 > 16(1): 45-49

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

引用本文:

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

Citation:

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

引用本文:

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

Citation:

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

黄河三角洲变形层理的研究

中国石油大学勘探系山东东营 257062

基金项目: 中国石油大学博士基金

详细信息

作者简介:
钟建华男 40岁博士构造地质学

中图分类号: P548

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文章访问数: 472
HTML全文浏览量: 1
PDF下载量: 544
被引次数: 0

Study on the Deformation Bedding in the Delta, of Yellow River

Exploration Department University of Petroleum ShanDong Doingyin 257062

摘要

摘要: 黄河三角洲发育了非常丰富的变形层理，规模不一，类型多样，成因复杂，概括起来有下列几种：泄水变形层理、重力滑动变形层理、流水牵引变形层理、沙波滑移变形层理、生物扰动变形层理、波浪改造变形层理及滑塌变形层理七种。其中以泄水变形层理和流水牵引变形层理最为常见和典型。泄水变形层理上表面往往有一乳头状或脊状的突起，有时中心有一泄水孔，与上下部层理呈突变接触。流水牵引变形层理具有五个特点：（1）变形层理之上经常可以见到没有层理或具平行层理的细泥砾（砂）层，或者逆行沙波、逆行爬升层理，显示了变形层理之上有高速水流作用；（2）有时可以看到褶曲状变形层理轴面向下游倾倒，但常常无规律可寻；（3）与上覆层理多为突变接触，与下伏层理突变或渐变接触，取决于变形强烈程度；（4）大部分变形强列，呈包卷状，囊状或管状；（5）分布稳定，有时可见多级组合产出。
- 变形层理 /
- 三角洲 /
- 黄河
Abstract: Deformed beddings of differentsizes areoften observed in the Yellow River Delta. They are formed bywater escaping,gravitational sliding,water flow dragging,ripple gliding,bioturbation,wave action and slump-ing,and can be divided into seven types according to their origins. Those formed by water escaping and waterflow dragging are the most common and typical ones among them. On surfaces of the deformed beddings of water escaping type，there are usually many nipple-like and do-ral fin-like projectings which may sometimes have a hole for water escaping in the center of each projecting，and the deformed beddings may have abrupt contact with their neighbor beddings. Deformed beddings of wa-ter flow dragging type usually possess five characteristics as follows: (1)the overlying sedments and sedimentary structures of them,such as clay boulder or sand-sized grainsin massive and parallel beddings，regressive sand waves，climbing-ripple laminations, are all formed by waterflow of high velocity. (2)the axial planes of fold curve-like deformed beddings are often randomly oriented,al-though they may sometimes dip toward the upper reach. (3)usually,they show abrupt contact with overlyingbeddings and gradual or abrupt contact with underlying beddings of them according to extent of deformation.(4)most of them are deformed severely and show very complicated appearences such as the cabbage-like onesand the bag-like or tube-like ones. (5)they are steadily widespread and sometimes may be well-stratified andgraded.
- deformed bedding /
- delta /
- Yellow River

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参考文献(1)

[1]

1 姜在兴，周丽清，林承焰等.河流中的异常水流及其沉积作用— 以黄河下游为例.科学通报，1992.37(1):54-56

2 姜在兴，王留奇，马在平等.黄河三角洲现代沉积研究.山东:石油大学出版社，1993. 50

3 钟建华.黄河三角洲的三种典型沉积构造.西北大学学报(自然科学版),1996,12(增刊):506-510

4 钟建华.沙岩岩墙(岩脉、岩床)的一种可能成因—冲蚀沟槽的充填.岩相古地理，1996,16(2):25一29

5 钟建华，马在平.泥沙钟乳—一种特殊的沉积构造.科学通报， 1997,42(17):1853-1856

6 Seed H B.Idriss 1 M. Analysis of Soilliquefaction. Niigata earth- quake: American Society of civil Engineering. Journal of Soil and Foundations Divition,1967.93.83-108

7 Seed H B. Landslides during earthquakes due to liqufaction. Journal of Soil Mechanics Foundations Divition.Am,Soc,Civ.Engrs.1968. S4.SMt.1053-1122

8 Lowc D R. Water escape structures in coarse graded sediments. Sedimcntology.1975.22:157-204

9 刘宝猫主编.沉积岩石学.北京:地质出版社，1980. 93

10 Owen G. Experinental soft-sediment deformation: structures formed by the liquefaction of unconsolidated sands and some an- cient examples. Sedimentology,1996, 43:279-293

11 Ten Haal E. Sigrificence of convolute lamination. Geol. Mijnbouw, 1995，18:188 194

12 Allen J'R L. The possible mechanics of convolute lamination in graded sand beds. Geol Soc.1972,London.134:19一31

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黄河三角洲变形层理的研究

中国石油大学勘探系山东东营 257062

基金项目: 中国石油大学博士基金

作者简介:
钟建华男 40岁博士构造地质学

收稿日期: 1997-01-05
修回日期: 1997-09-25
刊出日期: 1998-03-10

中图分类号: P548

关键词:

变形层理 /

三角洲 /

黄河

摘要: 黄河三角洲发育了非常丰富的变形层理，规模不一，类型多样，成因复杂，概括起来有下列几种：泄水变形层理、重力滑动变形层理、流水牵引变形层理、沙波滑移变形层理、生物扰动变形层理、波浪改造变形层理及滑塌变形层理七种。其中以泄水变形层理和流水牵引变形层理最为常见和典型。泄水变形层理上表面往往有一乳头状或脊状的突起，有时中心有一泄水孔，与上下部层理呈突变接触。流水牵引变形层理具有五个特点：（1）变形层理之上经常可以见到没有层理或具平行层理的细泥砾（砂）层，或者逆行沙波、逆行爬升层理，显示了变形层理之上有高速水流作用；（2）有时可以看到褶曲状变形层理轴面向下游倾倒，但常常无规律可寻；（3）与上覆层理多为突变接触，与下伏层理突变或渐变接触，取决于变形强烈程度；（4）大部分变形强列，呈包卷状，囊状或管状；（5）分布稳定，有时可见多级组合产出。

English Abstract

Study on the Deformation Bedding in the Delta, of Yellow River

Exploration Department University of Petroleum ShanDong Doingyin 257062

Received Date: 1997-01-05
Rev Recd Date: 1997-09-25
Publish Date: 1998-03-10

Keywords:

Abstract: Deformed beddings of differentsizes areoften observed in the Yellow River Delta. They are formed bywater escaping,gravitational sliding,water flow dragging,ripple gliding,bioturbation,wave action and slump-ing,and can be divided into seven types according to their origins. Those formed by water escaping and waterflow dragging are the most common and typical ones among them. On surfaces of the deformed beddings of water escaping type，there are usually many nipple-like and do-ral fin-like projectings which may sometimes have a hole for water escaping in the center of each projecting，and the deformed beddings may have abrupt contact with their neighbor beddings. Deformed beddings of wa-ter flow dragging type usually possess five characteristics as follows: (1)the overlying sedments and sedimentary structures of them,such as clay boulder or sand-sized grainsin massive and parallel beddings，regressive sand waves，climbing-ripple laminations, are all formed by waterflow of high velocity. (2)the axial planes of fold curve-like deformed beddings are often randomly oriented,al-though they may sometimes dip toward the upper reach. (3)usually,they show abrupt contact with overlyingbeddings and gradual or abrupt contact with underlying beddings of them according to extent of deformation.(4)most of them are deformed severely and show very complicated appearences such as the cabbage-like onesand the bag-like or tube-like ones. (5)they are steadily widespread and sometimes may be well-stratified andgraded.

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

引用本文:

钟建华, 马在平. 黄河三角洲变形层理的研究[J]. 沉积学报, 1998, 16(1): 45-49.

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

Citation:

Zhong Jianhua, Ma Zaiping. Study on the Deformation Bedding in the Delta, of Yellow River[J]. Acta Sedimentologica Sinica, 1998, 16(1): 45-49.

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黄河三角洲变形层理的研究

作者简介:
钟建华男 40岁博士构造地质学

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Study on the Deformation Bedding in the Delta, of Yellow River

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目录

黄河三角洲变形层理的研究

中国石油大学勘探系山东东营 257062

作者简介:
钟建华男 40岁博士构造地质学

English Abstract

Study on the Deformation Bedding in the Delta, of Yellow River

Exploration Department University of Petroleum ShanDong Doingyin 257062

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黄河三角洲变形层理的研究

作者简介: 钟建华 男 40岁 博士 构造地质学

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Study on the Deformation Bedding in the Delta, of Yellow River

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出版历程

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黄河三角洲变形层理的研究

中国石油大学勘探系 山东东营 257062

作者简介: 钟建华 男 40岁 博士 构造地质学

English Abstract

Study on the Deformation Bedding in the Delta, of Yellow River

Exploration Department University of Petroleum ShanDong Doingyin 257062

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 40岁博士构造地质学

中国石油大学勘探系山东东营 257062

作者简介:
钟建华男 40岁博士构造地质学