辫状河现代沉积研究与相模式──中国永定河剖析

廖保方; 张为民; 李列; 逯径铁; 葛云龙; 闻兰; 薛培华; 郭睿

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辫状河现代沉积研究与相模式──中国永定河剖析

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿

文章导航 > 沉积学报 > 1998 > 16(1): 34-39

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

引用本文:

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

Liao Baofang, Zhang Weimin, Li Lie, Lu Jing Tie, Ge Yunlong, Wen Lan, Xue Peihua, Guo Rui. Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e[J]. Acta Sedimentologica Sinica, 1998, 16(1): 34-39.

Citation:

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

引用本文:

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

Citation:

辫状河现代沉积研究与相模式──中国永定河剖析

1 华北石油职工大学河北固安 065506;
2 石油勘探开发科学研究院北京 100083

详细信息

作者简介:
廖保方男 32岁副教授硕士沉积学

中图分类号: P641.43

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文章访问数: 969
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被引次数: 0

Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

1 Huabei Petroleum Vocation University HeBei Guan 065506;
2 Research Institute of Petroleum Exploration and Development CNPC Beijing 100083

摘要

摘要: 永定河是一条多河型河流，自上而下，包括了辩状河→曲流河→分流网状河的河型空间转换。其间辫状河段可明显区分为两类亚型：即冲积扇区的高坡降辫状河和冲积平原区低坡降辫状河。二者在河流形态、沉积物特征等方面显示不同。而沉积作用机制和砂体沉积模式是近似的，二者均进行垂向加积作用，均发生五个级次的沉积再作用面，均发育三个级次类型的薄夹层：滞留层、落淤层、颗粒降纹层与颗粒流纹层。其中落淤层最具指相意义。在河道经常摆动迁移过程中，最终形成砂体广泛展布的“叠覆泛砂体”。这种辫状河沉积模式──“叠覆泛砂体”为油气储集提供了良好的储集空间和场所。
- 高坡降辫状河 /
- 低坡降辫状河 /
- 落淤层 /
- 沉积模式 /
- 叠覆泛砂体
Abstract: There are multipatterns in the Yongding River and they transfer from the braided to meandering,then toan abranched channel along the flow direction. The braided stream segment can be subdivided into two types:One is a high slope braided river which is distributed in the fluvial fan，water 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 固安县水利局编.固安县水利志.北京:中国人事出版社，l99l. 7

2 裘亦楠主编.储层地质模式.石油科技论文集.北京:石油工业出版社，1990. 5

3 薛培华.河流点坝相储层模式概论.北京:石油工业出版社，1991.1

4 米阿尔AD.河流沉积体系分析，吴伟译.北京:石油工业出版社，1987. 9

5 Bridge J S,Gabel S I.Flow and sediment dynamics in a low sinuosi-ty, braided river: Calamus river. Nebraska Sandhills. Sedimentolo-gy,1992,39(1):125-142

6 Godin P D. Fining-upward cycles in the sandy braided-river depositsof the Westwater Canyon member(Upper Jurrassic),Morrison for-mation,New Mexico. Sedimentary Geology,1991, 70(1) : 61- 82

7 Feldman H R. Pleistocene braided stream deposits from northwest-ern South Carolina. Southeastern Geology,1990,31(4):223-234

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辫状河现代沉积研究与相模式──中国永定河剖析

1 华北石油职工大学河北固安 065506;

2 石油勘探开发科学研究院北京 100083

作者简介:
廖保方男 32岁副教授硕士沉积学

收稿日期: 1996-10-04
修回日期: 1997-07-07
刊出日期: 1998-03-10

中图分类号: P641.43

关键词:

落淤层 /

摘要: 永定河是一条多河型河流，自上而下，包括了辩状河→曲流河→分流网状河的河型空间转换。其间辫状河段可明显区分为两类亚型：即冲积扇区的高坡降辫状河和冲积平原区低坡降辫状河。二者在河流形态、沉积物特征等方面显示不同。而沉积作用机制和砂体沉积模式是近似的，二者均进行垂向加积作用，均发生五个级次的沉积再作用面，均发育三个级次类型的薄夹层：滞留层、落淤层、颗粒降纹层与颗粒流纹层。其中落淤层最具指相意义。在河道经常摆动迁移过程中，最终形成砂体广泛展布的“叠覆泛砂体”。这种辫状河沉积模式──“叠覆泛砂体”为油气储集提供了良好的储集空间和场所。

English Abstract

Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

1 Huabei Petroleum Vocation University HeBei Guan 065506;

2 Research Institute of Petroleum Exploration and Development CNPC Beijing 100083

Received Date: 1996-10-04
Rev Recd Date: 1997-07-07
Publish Date: 1998-03-10

Keywords:

deformed bedding /
delta /
Yellow River /
/

Abstract: There are multipatterns in the Yongding River and they transfer from the braided to meandering,then toan abranched channel along the flow direction. The braided stream segment can be subdivided into two types:One is a high slope braided river which is distributed in the fluvial fan，water 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.

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

引用本文:

廖保方, 张为民, 李列, 逯径铁, 葛云龙, 闻兰, 薛培华, 郭睿. 辫状河现代沉积研究与相模式──中国永定河剖析[J]. 沉积学报, 1998, 16(1): 34-39.

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辫状河现代沉积研究与相模式──中国永定河剖析

作者简介:
廖保方男 32岁副教授硕士沉积学

计量

Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

计量

目录

辫状河现代沉积研究与相模式──中国永定河剖析

1 华北石油职工大学河北固安 065506;

2 石油勘探开发科学研究院北京 100083

作者简介:
廖保方男 32岁副教授硕士沉积学

English Abstract

Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

1 Huabei Petroleum Vocation University HeBei Guan 065506;

2 Research Institute of Petroleum Exploration and Development CNPC Beijing 100083

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辫状河现代沉积研究与相模式──中国永定河剖析

作者简介: 廖保方 男 32岁 副教授 硕士 沉积学

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Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

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出版历程

目录

辫状河现代沉积研究与相模式──中国永定河剖析

1 华北石油职工大学 河北固安 065506; 2 石油勘探开发科学研究院 北京 100083

作者简介: 廖保方 男 32岁 副教授 硕士 沉积学

English Abstract

Study on Modern Deposit of a Braided Stream and Facies Model-Taking the Yongding River as an Exampl e

1 Huabei Petroleum Vocation University HeBei Guan 065506; 2 Research Institute of Petroleum Exploration and Development CNPC Beijing 100083

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
廖保方男 32岁副教授硕士沉积学

1 华北石油职工大学河北固安 065506;

2 石油勘探开发科学研究院北京 100083

作者简介:
廖保方男 32岁副教授硕士沉积学

1 Huabei Petroleum Vocation University HeBei Guan 065506;

2 Research Institute of Petroleum Exploration and Development CNPC Beijing 100083