深水重力流水道沉积研究进展<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2020.01.010

古地理学报 ›› 2020, Vol. 22 ›› Issue (1): 161-174. doi: 10.7605/gdlxb.2020.01.010

深水重力流水道沉积研究进展^*

李华^1,2, 何幼斌^1,2

1 长江大学地球科学学院,湖北武汉 430100;
2 长江大学沉积盆地研究中心,湖北武汉 430100

收稿日期:2019-05-06 出版日期:2020-02-01 发布日期:2020-03-04
通讯作者: 何幼斌,男,1964年生,教授,主要研究方向为沉积学。E-mail: 100709@yangtzeu.edu.cn。
作者简介:李华,男,1984年生,博士,副教授,主要研究方向为深水沉积。E-mail: 501026@yangtzeu.edu.cn。
基金资助:
*“十三五”国家科技重大专项(编号: 2017ZX05032-002-003)、国家自然基金项目(编号: 41472096、41502101)、长江青年基金(编号: 2015cqn26)、湖北省教育厅科学研究计划中青年人才项目(编号: Q20171308)及地质资源与地质工程一流学科开放基金项目联合资助

Research progress on deepwater gravity flow channel deposit

Li Hua^1,2, He You-Bin^1,2

1 School of Geosciences,Yangtze University,Wuhan 430100, China;
2 Research Center of Sedimentary Basin,Yangtze University,Wuhan 430100,China

Received:2019-05-06 Online:2020-02-01 Published:2020-03-04
Contact: He You-Bin,born in 1964,is a professor. Now he is mainly engaged in research on sedimentology. E-mail: 100709@yangtzeu.edu.cn.
About author:Li Hua,born in 1984,is an associate professor. He is mainly engaged in deepwater deposits. E-mail: 501026@yangtzeu.edu.cn.
Supported by:
; Co-funded by the National Key Technology Research and Development Program of China during the “13th Five-Year Plan”(No.2017ZX05032-002-003),the National Natural Science Foundation of China(Nos. 41472096,41502101),Yangtze Youth Fund of Yangtze University(No.2015cqn26), the Youth Talent Project of the Science Research Program of the Education Department of Hubei Province of China(No. Q20171308) and Open Foundation of TOP Disciplines in Yangtze University

摘要/Abstract

摘要： 深水水道是深水区常见的地貌单元,既是深水重力流沉积物的搬运通道,又是其主要沉积场所。对重力流水道沉积研究已有60余年的历史,成果极为丰富。本文简要回顾了深水水道沉积研究历程及最新研究成果,总结了主要水道类型沉积特征及形成机理。重力流水道可分为复合型水道、垂向加积型水道、迁移型水道和分支小水道。复合型水道形成与重力流演化过程密切相关,其内部发育轴部沉积、碎屑流/滑塌沉积、水道—堤岸沉积体系及迁移型水道。弯曲型迁移水道多为重力流自生环流而成,顺直型迁移水道为等深流与重力流共同作用而成。重力流水道研究的发展方向主要有3个方面,即:(1)积极开展多手段和方法综合研究;(2)深入系统对比研究其形成机制及主控因素;(3)加强储集层分布规律研究。

关键词: 深水水道, 复合型水道, 迁移型水道, 重力流

Abstract: Deepwater channel is usually geomorphology in deepwater zone,which is not only transport way of deepwater gravity flow sediment,but also is mainly sedimentary place. There have been abundant fruits on gravity flow channel for more than 60 years. The research process and latest achievement are reviewed,characteristic and mechanism of deepwater channel have been summarized in this paper. The gravity flow channel could be divided into complex channel,vertical aggradation channel,migrational channel and small bifurcated channels. The process of complex channel is closely related to evolution of gravity flow. Channel axial deposits,debris flow/slump deposit,channel-levee system and migrational channel develop in complex channel. Sinuous migrational channel secondary circulation of gravity flow was formed. Strait migrational channel is interaction between gravity flow and contour current. The direction of work on gravity flow channel in the future always results from were proposed as follows: (1)more way and method comprehensive research; (2)systematic comparative study on mechanism and mainly controlling factors; (3)reinforce to work on the reservoir distribution.

Key words: deepwater channel, complex channel, migrational channel, gravity flow

中图分类号:

TE121.3

李华, 何幼斌. 深水重力流水道沉积研究进展^*[J]. 古地理学报, 2020, 22(1): 161-174.

Li Hua, He You-Bin. Research progress on deepwater gravity flow channel deposit[J]. JOPC, 2020, 22(1): 161-174.

http://www.gdlxb.cn/CN/Y2020/V22/I1/161

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