深水浊流沉积综述

Henry W. Posamentier; Venkatarathnam Kolla; 刘化清

doi:10.14027/j.issn.1000-0550.2019.049

ISSN 1000-0550 CN 62-1038/P

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深水浊流沉积综述

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清

文章导航 > 沉积学报 > 2019 > 37(5): 879-903

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

引用本文:

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Henry W. Posamentier, Venkatarathnam Kolla, LIU HuaQing. An Overview of Deep-water Turbidite Deposition[J]. Acta Sedimentologica Sinica, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Citation:

Henry W. Posamentier, Venkatarathnam Kolla, LIU HuaQing. An Overview of Deep-water Turbidite Deposition[J]. Acta Sedimentologica Sinica, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

引用本文:

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Henry W. Posamentier, Venkatarathnam Kolla, LIU HuaQing. An Overview of Deep-water Turbidite Deposition[J]. Acta Sedimentologica Sinica, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Citation:

深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

1.
美国得克萨斯州, 伍德兰, 托普赛德罗德伍 25号 77380;
2.
美国得克萨斯州, 休斯顿, 拉蓬特 6907号 77083;
3.
中国石油勘探开发研究院西北分院, 兰州 730020

基金项目: 国家科技重大专项（2017ZX05001-003）

详细信息

通讯作者:
刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

中图分类号: P512.2

计量

文章访问数: 381
HTML全文浏览量: 67
PDF下载量: 216
被引次数: 0

An Overview of Deep-water Turbidite Deposition

1.
25 Topside Row Drive, The Woodlands, TX 77380, US;
2.
6907 La Puente Dr., Houston, Texas 77083, US;
3.
Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China

Funds: National Science and Technology Major Project, No. 2017ZX05001-003

摘要

摘要: 深水浊积岩通常发育在风暴浪基面以下、几十米至数千米的水体深度范围内。当沉积中心位于或接近陆架边缘时，浊流沉积系统往往最为活跃，而且通常与相对海平面下降时期的低位体系域有关。深水沉积事件可细分为低位域早期和低位域晚期。低位域早期以规模不断增大和更频繁的流体（浊流）事件为特征；而低位域晚期则以规模逐渐变小且频率降低的流体（浊流）事件为特征。因此，在低位域早期，流体流量不断增大，水道以侵蚀并逐渐变深为主，仅能残存较少的沉积物。随后，在低位域晚期，流体流量逐渐变小，因而水道内的沉积填充物可以得以保存。浊流体系通常发育3个特征迥异的区域：区域1对应浊流体系的近端（上游），以支流峡谷为特征；区域2为浊流体系的中间部分，以单一补给水道复合体系为特征，因浊流水体的高度比补给水道高，因而常常发育天然堤沉积；区域3为浊流体系的远端，以频繁的决口、砂质溢岸以及水道充填为特征，从地貌学上可以将其描述为末端扇，从沉积过程来看，可将其称为前缘分散体系。从层序地层学的角度来看，低位域沉积常常夹持于富泥的远端高位域和海侵体系域沉积之间。低位域早期—晚期沉积序列往往是以富砂的区域3末端扇沉积被区域2水道—天然堤沉积所覆盖为特征。
- 浊流 /
- 深水重力流 /
- 支流峡谷 /
- 补给水道复合体 /
- 天然堤 /
- 分流水道 /
- 末端扇 /
- 综述
Abstract: Deep-water turbidites commonly are deposited in water depths below storm wave base. These depths range from a few tens of meters to thousands of meters. Turbidite systems tend to be most active when depocenters lie at or near shelf margins,and this proximity of depocenters to shelf margins tends to be associated most commonly with times of relative sea level lowstand. Deep water depositional episodes can be divided into early and late lowstand time. Deposition during early lowstand is characterized by progressively larger and more frequent flow events,whereas deposition during late lowstand is characterized by progressively smaller and less frequent flow events. Consequently,during early lowstand time,erosion of channels tends to dominate such that channels tend to become progressively deeper with minimal preservation of deposits within feeder channels;successive flows are overfit. Subsequently during late lowstand progressively smaller flows tend to be underfit resulting in preservation of channel fill deposits. Turbidite systems tend to be characterized by three discrete regions:Region 1 corresponds to the most proximal reaches of turbidite systems dominated by canyons that commonly are tributive. Region 2 corresponds to that part of the turbidite system characterized by a single feeder channel complex that was characterized by flows with heights greater than confining walls,hence associated with levees. Region 3 corresponds to that part of the system distally, that is characterized by frequent avulsions and sand-prone overbank as well as channel-fill deposits,which can be described geomorphologically as a terminal fan. From a process perspective,Region 3 can be described as a frontal splay. From a sequence stratigraphic perspective,lowstand deposits commonly are bracketed by mud prone distal highstand and transgressive systems tract deposits. The succession of early to late lowstand deposition commonly is characterized by sand-rich Region 3 fan deposits overlain by leveed channel deposits of region 2.
- turbidity current /
- deep-water gravity flow /
- tributive canyon /
- feeder channel complex /
- levee /
- distributive channel /
- terminal fan /
- overview

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[1]	刘杰, 孙美静, 高红芳, 李学杰. 台湾东部海域沉积物波特征及其成因探讨 . 沉积学报, 2019, 37(1): 155-162. doi: 10.14027/j.issn.1000-0550.2018.106
[2]	朱筱敏, 谈明轩, 董艳蕾, 李维, 秦祎, 张自力. 当今沉积学研究热点讨论——第20届国际沉积学大会评述 . 沉积学报, 2019, 37(1): 1-16. doi: 10.14027/j.issn.1000-0550.2018.185
[3]	徐伟, 李正宇, 刘艺萌, 刘军钊, 王启明. 渤中25-1油田沙三段重力流沉积模式及油气地质意义 . 沉积学报, 2018, 36(3): 557-569. doi: 10.14027/j.issn.1000-0550.2018.075
[4]	张昌民, 朱锐, 赵康, 胡威, 尹艳树, 李少华, 尹太举. 从端点走向连续:河流沉积模式研究进展述评 . 沉积学报, 2017, 35(5): 926-944. doi: 10.14027/j.cnki.cjxb.2017.05.006
[5]	谈明轩, 朱筱敏, 耿名扬, 刘常妮. 沉积物重力流流体转化沉积-混合事件层 . 沉积学报, 2016, 34(6): 1108-1119. doi: 10.14027/j.cnki.cjxb.2016.06.009
[6]	. 弯曲海底峡谷中浊流的三维流动及沉积的初步研究 . 沉积学报, 2013, 31(6): 1001-1007.
[7]	孙辉. 孟加拉湾缅甸若开盆地上新统斜坡水道复合体沉积特征 . 沉积学报, 2011, 29(4): 695-703. doi:
[8]	李冬. 琼东南盆地中央峡谷深水天然堤—溢岸沉积 . 沉积学报, 2011, 29(4): 689-694. doi:
[9]	李林. 重力流沉积：理论研究与野外识别 . 沉积学报, 2011, 29(4): 677-688. doi:
[10]	张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征 . 沉积学报, 2011, 29(1): 1-13. doi:
[11]	李顺明. 沾化凹陷桩西油田古近系东营组重力流水道的沉积特征及形成条件 . 沉积学报, 2010, 28(1): 83-90. doi:
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[13]	王海荣. 南海东北部台湾浅滩陆坡的浊流沉积物波的发育及其成因的构造控制 . 沉积学报, 2008, 26(1): 39-45. doi:
[14]	刘正华. 歧南凹陷沙河街组重力流水道砂体成岩作用和孔隙演化模式 . 沉积学报, 2007, 25(2): 183-191. doi:
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[16]	刘善印, 钟大赉, 吴根耀. 滇西南景谷—镇沅地区第三纪重力流沉积及其地质意义 . 沉积学报, 1998, 16(2): 50-54.
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[18]	张晓宝, 方国庆, 何海清. 西秦岭上三叠统浊积岩系中波痕的主要特征及其成因探讨 . 沉积学报, 1994, 12(4): 124-131.
[19]	刘家铎. 西南太平洋新喀里多尼亚洛亚蒂盆地的现代沉积作用 . 沉积学报, 1992, 10(4): 137-145.
[20]	端木合顺, 朱莲芳. 酒西盆地下白垩统下沟组重力流水下扇沉积 . 沉积学报, 1990, 8(2): 75-86.

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文章访问数: 381
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深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

1. 美国得克萨斯州, 伍德兰, 托普赛德罗德伍 25号 77380;

2. 美国得克萨斯州, 休斯顿, 拉蓬特 6907号 77083;

3. 中国石油勘探开发研究院西北分院, 兰州 730020

基金项目: 国家科技重大专项（2017ZX05001-003）

通讯作者: 刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

收稿日期: 2019-02-10
修回日期: 2019-06-26
刊出日期: 2019-10-10

中图分类号: P512.2

关键词:

浊流 /

天然堤 /

末端扇 /

摘要: 深水浊积岩通常发育在风暴浪基面以下、几十米至数千米的水体深度范围内。当沉积中心位于或接近陆架边缘时，浊流沉积系统往往最为活跃，而且通常与相对海平面下降时期的低位体系域有关。深水沉积事件可细分为低位域早期和低位域晚期。低位域早期以规模不断增大和更频繁的流体（浊流）事件为特征；而低位域晚期则以规模逐渐变小且频率降低的流体（浊流）事件为特征。因此，在低位域早期，流体流量不断增大，水道以侵蚀并逐渐变深为主，仅能残存较少的沉积物。随后，在低位域晚期，流体流量逐渐变小，因而水道内的沉积填充物可以得以保存。浊流体系通常发育3个特征迥异的区域：区域1对应浊流体系的近端（上游），以支流峡谷为特征；区域2为浊流体系的中间部分，以单一补给水道复合体系为特征，因浊流水体的高度比补给水道高，因而常常发育天然堤沉积；区域3为浊流体系的远端，以频繁的决口、砂质溢岸以及水道充填为特征，从地貌学上可以将其描述为末端扇，从沉积过程来看，可将其称为前缘分散体系。从层序地层学的角度来看，低位域沉积常常夹持于富泥的远端高位域和海侵体系域沉积之间。低位域早期—晚期沉积序列往往是以富砂的区域3末端扇沉积被区域2水道—天然堤沉积所覆盖为特征。

English Abstract

An Overview of Deep-water Turbidite Deposition

1. 25 Topside Row Drive, The Woodlands, TX 77380, US;

2. 6907 La Puente Dr., Houston, Texas 77083, US;

3. Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China

Funds: National Science and Technology Major Project, No. 2017ZX05001-003

Received Date: 2019-02-10
Rev Recd Date: 2019-06-26
Publish Date: 2019-10-10

Keywords:

Abstract: Deep-water turbidites commonly are deposited in water depths below storm wave base. These depths range from a few tens of meters to thousands of meters. Turbidite systems tend to be most active when depocenters lie at or near shelf margins,and this proximity of depocenters to shelf margins tends to be associated most commonly with times of relative sea level lowstand. Deep water depositional episodes can be divided into early and late lowstand time. Deposition during early lowstand is characterized by progressively larger and more frequent flow events,whereas deposition during late lowstand is characterized by progressively smaller and less frequent flow events. Consequently,during early lowstand time,erosion of channels tends to dominate such that channels tend to become progressively deeper with minimal preservation of deposits within feeder channels;successive flows are overfit. Subsequently during late lowstand progressively smaller flows tend to be underfit resulting in preservation of channel fill deposits. Turbidite systems tend to be characterized by three discrete regions:Region 1 corresponds to the most proximal reaches of turbidite systems dominated by canyons that commonly are tributive. Region 2 corresponds to that part of the turbidite system characterized by a single feeder channel complex that was characterized by flows with heights greater than confining walls,hence associated with levees. Region 3 corresponds to that part of the system distally, that is characterized by frequent avulsions and sand-prone overbank as well as channel-fill deposits,which can be described geomorphologically as a terminal fan. From a process perspective,Region 3 can be described as a frontal splay. From a sequence stratigraphic perspective,lowstand deposits commonly are bracketed by mud prone distal highstand and transgressive systems tract deposits. The succession of early to late lowstand deposition commonly is characterized by sand-rich Region 3 fan deposits overlain by leveed channel deposits of region 2.

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

引用本文:

Henry W. Posamentier, Venkatarathnam Kolla, 刘化清. 深水浊流沉积综述[J]. 沉积学报, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Henry W. Posamentier, Venkatarathnam Kolla, LIU HuaQing. An Overview of Deep-water Turbidite Deposition[J]. Acta Sedimentologica Sinica, 2019, 37(5): 879-903. doi: 10.14027/j.issn.1000-0550.2019.049

Citation:

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深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

通讯作者:
刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

计量

An Overview of Deep-water Turbidite Deposition

计量

目录

深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

1. 美国得克萨斯州, 伍德兰, 托普赛德罗德伍 25号 77380;

2. 美国得克萨斯州, 休斯顿, 拉蓬特 6907号 77083;

3. 中国石油勘探开发研究院西北分院, 兰州 730020

通讯作者: 刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

English Abstract

An Overview of Deep-water Turbidite Deposition

1. 25 Topside Row Drive, The Woodlands, TX 77380, US;

2. 6907 La Puente Dr., Houston, Texas 77083, US;

3. Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China

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深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

通讯作者: 刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

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An Overview of Deep-water Turbidite Deposition

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出版历程

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深水浊流沉积综述

doi: 10.14027/j.issn.1000-0550.2019.049

1. 美国得克萨斯州, 伍德兰, 托普赛德罗德伍 25号 77380; 2. 美国得克萨斯州, 休斯顿, 拉蓬特 6907号 77083; 3. 中国石油勘探开发研究院西北分院, 兰州 730020

通讯作者: 刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

English Abstract

An Overview of Deep-water Turbidite Deposition

1. 25 Topside Row Drive, The Woodlands, TX 77380, US; 2. 6907 La Puente Dr., Houston, Texas 77083, US; 3. Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
刘化清,男,教授级高级工程师,E-mail:liu_hq@petrochina.com.cn

1. 美国得克萨斯州, 伍德兰, 托普赛德罗德伍 25号 77380;

2. 美国得克萨斯州, 休斯顿, 拉蓬特 6907号 77083;

3. 中国石油勘探开发研究院西北分院, 兰州 730020

1. 25 Topside Row Drive, The Woodlands, TX 77380, US;

2. 6907 La Puente Dr., Houston, Texas 77083, US;

3. Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China