三角洲前缘滑塌浊积岩形成过程初探

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三角洲前缘滑塌浊积岩形成过程初探

鄢继华, 陈世悦, 宋国奇, 姜在兴, 邱桂强

文章导航 > 沉积学报 > 2004 > 22(4): 573-578

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[J]. 沉积学报, 2004, 22(4): 573-578.

引用本文:

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[J]. 沉积学报, 2004, 22(4): 573-578.

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

Citation:

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

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[J]. 沉积学报, 2004, 22(4): 573-578.

引用本文:

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[J]. 沉积学报, 2004, 22(4): 573-578.

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

Citation:

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

三角洲前缘滑塌浊积岩形成过程初探

1.
石油大学地球资源与信息学院山东东营 257061;
2.
中国石油化工股份公司胜利油田山东东营 257015

基金项目: 国家十五科技攻关项目(项目编号:2001BA605A09)资助.

作者简介:
鄢继华男 1977年出生在读博士研究生沉积学

中图分类号: P642.2

计量

文章访问数: 600
HTML全文浏览量: 9
PDF下载量: 765
被引次数: 0

Preliminary Study on the Formation of Fluxoturbidite in Front of Delta

1.
Faculty of Geo Resources and Information, University of Petroleum, Dongying, Shandong 257061;
2.
Geological Scientific Research Institute, Shengli Petroleum Administration, Dongying, Shandong 257015

摘要: 通过室内水槽实验模拟了三角洲前缘滑塌浊积岩的形成过程,总结出四种滑塌浊积岩类型,即无触发机制的天然重力滑塌、地震诱发作用产生的滑塌、波浪作用产生的滑塌和与底形相关的砂岩透镜体。实验结果表明,外界触发机制是形成三角洲前缘滑塌浊积岩的重要条件,底形的变化结合波浪、地震等外界触发机制的作用更容易在三角洲前缘形成滑塌浊积体。此外,被破坏和改造的三角洲前缘更易找到滑塌浊积体;相反,形态规则、保存完好的三角洲前缘反而不利于滑塌浊积岩的形成。
- 三角洲 /
- 滑塌浊积岩 /
- 水槽实验 /
- 地震作用 /
- 波浪作用
Abstract: According to the in door flume experiment simulations, the formation of fluxoturbidite in front of delta is studied. It is summarized that there are four kinds of fluxoturbidite in front of delta. They are the fluxoturbidite with no trigger action and one associated with seismic process, one with wave action and sandstone lens correlative with landform. The experiments suggest that trigger actions are the most important conditions to form fluxoturbidite in front of delta. Together with wave action and seismic process, the change of landform can promote forming fluxoturbidite. Also, the fluxoturbidite can be found easily in front of the delta where the delta front has been destroyed and rebuilt. In contrast, the regular and good reserved delta front is disadvantaged to form fluxoturbidite.
- delta /
- fluxoturbidite /
- flume experiment /
- seismic process /
- wave action

参考文献(10)

[1]	陈嘉树,杨立明. 东辛地区沙河街组三段中部砂体沉积特征及控制因素. 石油勘探与开发, 1997,24(5):38～41[Chen Jiashu, Yang Liming. Sand body sedimentary characteristics and control factors in the middle third member of Shahejie Formation in Dongxin region. Petroleum Exploration and Development,1977,24(5):38～41]
[2]	邱桂强,王居峰,李从先.东营凹陷沙三中东营三角洲地层格架与油气勘探.同济大学学报, 2001,29(10):1195～1199[Qiu Guiqiang, Wang Jufeng, Li Congxian. Preliminary study on stratigraphy architecture of middle-Shasan Dongying delta and its significance to hydrocarbon exploration. Journal of Tongji University,2001,29(10):1195～1199]
[3]	邱桂强,王居峰,张昕,等.东营三角洲沙河街组三段中亚段地层格架初步研究及油气勘探意义.沉积学报, 2001.19(4):569～574[Qiu Guiqiang, Wang Jufeng, Zhang Xin, et al. Preliminary study on stratigraphic architecture of middle-Shasan Dongying delta and its significance to hydrocarbon exploration. Acta Sedimentologica Sinica,2001,19(4):569～574]
[4]	张春生,刘忠保,施冬,等.涌流型浊流形成及发展的实验模拟. 沉积学报, 2002.20(1):25～29[Zhang Chunsheng, Liu Zhongbao, Shi Dong,et al. The simulation experiment of surge-type turbidity current formation and development. Acta Sedimentologica Sinica,2002,20(1):25～29]
[5]	Patrice E, Carbonneau, Norm and Bergeron E. The effect of bedload transport on mean and turbulent flow properties. Geomorphology, 2000, 35:267～278
[6]	Yu'suke Kubo, Takeshi Nakajima. Laboratory experiments and numerical simulation of sediment-wave formation by turbidity currents. Marine Geology, 2002, 192: 105～121
[7]	Paul Mcleod, Steven Carey, .Stephen R, Sparks J. Behavior of particle-laden flows into the ocean: experimental simulation and geological implication. Sedimentology, 1999, 46: 523～536
[8]	Shanmugam G. 50 years of the turbidite paradigm (1950s-1990s): deep-water processes and facies models-a critical perspective. Marine and Petroleum Geology, 2000, 17:285～342
[9]	赵密福,信荃麟,刘泽容.惠民凹陷临南洼陷滑塌浊积岩的分布规律及其控制因素.石油实验地质, 2001 23(3):267～271[Zhao Mifu, Xin Quanlin, Liu Zerong. Distribution rules of fluxoturbidite in the Linnan sag of the Huimin depression and their control factors. Petroleum Geology & Experiment, 2001,23(3):267～271]
[10]	陈世悦,袁文芳,鄢继华.济阳坳陷早第三纪震积岩的发现及其意义.地质科学,2003,38(3):377～384[Chen Shiyue, Yuan Wenfang, Yan Jihua. Discovery and significance of earthquake event deposits of early Tertiary in the Jiyang depression. Chinese Journal of Geology,2003,38(3):377～384]

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计量

文章访问数: 600
HTML全文浏览量: 9
PDF下载量: 765
被引次数: 0

三角洲前缘滑塌浊积岩形成过程初探

1. 石油大学地球资源与信息学院山东东营 257061;

2. 中国石油化工股份公司胜利油田山东东营 257015

基金项目: 国家十五科技攻关项目(项目编号:2001BA605A09)资助.

作者简介:
鄢继华男 1977年出生在读博士研究生沉积学

收稿日期: 2003-12-25
修回日期: 2004-03-23
刊出日期: 2004-12-10

中图分类号: P642.2

关键词:

滑塌浊积岩 /

摘要: 通过室内水槽实验模拟了三角洲前缘滑塌浊积岩的形成过程,总结出四种滑塌浊积岩类型,即无触发机制的天然重力滑塌、地震诱发作用产生的滑塌、波浪作用产生的滑塌和与底形相关的砂岩透镜体。实验结果表明,外界触发机制是形成三角洲前缘滑塌浊积岩的重要条件,底形的变化结合波浪、地震等外界触发机制的作用更容易在三角洲前缘形成滑塌浊积体。此外,被破坏和改造的三角洲前缘更易找到滑塌浊积体;相反,形态规则、保存完好的三角洲前缘反而不利于滑塌浊积岩的形成。

English Abstract

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[J]. 沉积学报, 2004, 22(4): 573-578.

引用本文:

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[J]. 沉积学报, 2004, 22(4): 573-578.

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

Citation:

YAN Ji hua, CHEN Shi yue, SONG Guo qi, JIANG Zai xing, QIU Gui qiang. Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.

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