黄河三角洲变形层理的研究

钟建华; 马在平

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

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

计量

文章访问数: 553
HTML全文浏览量: 15
PDF下载量: 548
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

HTML全文

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

[1]	徐嘉毅, 刘丽, 葛家旺, 赵晓明. 不同潮差影响的陆架三角洲沉积模式-基于Delft3D数值模拟的启示 . 沉积学报, 2025, (): -. doi: 10.14027/j.issn.1000-0550.2024.123
[2]	王俊辉, 张伟, 李莉, 鲜本忠, 周源. 平衡指数解释深水、浅水三角洲地貌的差异【水槽沉积模拟实验专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.087
[3]	贺华瑞, 栾锡武, 龚梁轩, 叶传红, 闫恒. 南昆嵩凹陷中新世以来三角洲地震响应与沉积充填演化 . 沉积学报, 2023, 41(5): 1568-1582. doi: 10.14027/j.issn.1000-0550.2022.024
[4]	王昕, 魏思源, 吕奇奇, 代榕, 呼焕, 毕宇航, 张丽雯, 梁岩, 张建坤. 基于物理模拟的三角洲前缘横向砂坝发育过程及形成机理 . 沉积学报, 2023, 41(3): 818-827. doi: 10.14027/j.issn.1000-0550.2021.150
[5]	李富强, 高红山, 张连科, 李宗盟, 庞红丽, 潘保田. 基于粒度参数特征对黄河后套平原段岩芯沉积环境的分析 . 沉积学报, 2019, 37(6): 1234-1243. doi: 10.14027/j.issn.1000-0550.2019.004
[6]	钟建华, 宋冠先, 倪良田, 孙宁亮, 郝兵, 葛毓柱, 薛纯琦, 孙景耀, 刘闯, 曹梦春. 黄河下游与黄河三角洲现代非地震变形层理的研究 . 沉积学报, 2019, 37(2): 239-253. doi: 10.14027/j.issn.1000-0550.2018.168
[7]	李小平, 柳保军, 丁琳, 郝建光, 龚文. 海相三角洲沉积单元划分及其对勘探砂体对比的意义——基于现代珠江三角洲沉积水动力综合研究 . 沉积学报, 2016, 34(3): 555-562. doi: 10.14027/j.cnki.cjxb.2016.03.013
[8]	. 黄河泛滥平原全新世沙尘暴活动的历史记录——以颖河上游一典型剖面为例 . 沉积学报, 2008, 26(1): 144-150.
[9]	王居峰. 东营三角洲—浊积扇高频层序叠加样式与岩性圈闭 . 沉积学报, 2005, 23(2): 303-309.
[10]	王峰, 王多云, 高明书, 姚永朝, 王志坤, 李树同, 秦红. 陕甘宁盆地姬塬地区三叠系延长组三角洲前缘的微相组合及特征 . 沉积学报, 2005, 23(2): 218-224.
[11]	王永红, 沈焕庭, 张卫国. 长江与黄河河口沉积物磁性特征对比的初步研究 . 沉积学报, 2004, 22(4): 658-663.
[12]	鄢继华, 陈世悦, 宋国奇, 姜在兴, 邱桂强. 三角洲前缘滑塌浊积岩形成过程初探 . 沉积学报, 2004, 22(4): 573-578.
[13]	何江, 李朝生, 王新伟, 孙卫国, 米娜. 多离子体系中黄河沉积物对重金属的竞争吸附研究 . 沉积学报, 2003, 21(3): 500-505.
[14]	王冠民, 温志峰, 马在平. 黄河下游边滩表面的鱼类遗迹 . 沉积学报, 2003, 21(4): 579-585.
[15]	王洪宝, 钟建华, 王书宝. 黄河三角洲平原上的气胀构造特征、成因及意义 . 沉积学报, 2003, 21(4): 571-578.
[16]	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 . 沉积学报, 2002, 20(2): 261-266.
[17]	钟建华, 王洪宝. 黄河下游河道的冻裂研究 . 沉积学报, 2002, 20(4): 650-655.
[18]	孙景耀, 陈辉军, 朱明春. 黄河济南以下河段某些异常地质作用及几种典型沉积构造研究 . 沉积学报, 2001, 19(1): 79-84.
[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 . 沉积学报, 2000, 18(1): 7-12.
[20]	钟建华, 马在平. 黄河三角洲胜利Ⅰ号心滩的研究 . 沉积学报, 1998, 16(3): 38-43,51.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 553
HTML全文浏览量: 15
PDF下载量: 548
被引次数: 0

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.

全文HTML

参考文献 (1)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

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

计量

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

计量

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

计量

出版历程

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

计量

出版历程

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

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