盐构造与深水水道的交互作用&mdash;&mdash;以下刚果盆地为例

陈亮; 赵千慧; 王英民; 孙红军; 万琼华; 唐武; 赵鹏

doi:10.14027/j.cnki.cjxb.2017.06.011

ISSN 1000-0550 CN 62-1038/P

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盐构造与深水水道的交互作用——以下刚果盆地为例

陈亮, 赵千慧, 王英民, 孙红军, 万琼华, 唐武, 赵鹏

文章导航 > 沉积学报 > 2017 > 35(6): 1197-1204

陈亮, 赵千慧, 王英民, 孙红军, 万琼华, 唐武, 赵鹏. 盐构造与深水水道的交互作用——以下刚果盆地为例[J]. 沉积学报, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011

引用本文:

CHEN Liang, ZHAO QianHui, WANG YingMin, SUN HongJun, WAN QiongHua, TANG Wu, ZHAO Peng. Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011

Citation:

CHEN Liang, ZHAO QianHui, WANG YingMin, SUN HongJun, WAN QiongHua, TANG Wu, ZHAO Peng. Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011

引用本文:

Citation:

CHEN Liang, ZHAO QianHui, WANG YingMin, SUN HongJun, WAN QiongHua, TANG Wu, ZHAO Peng. Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011

盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

1.
中海油研究总院, 北京 100028;
2.
中国石油管道局工程有限公司国际事业部, 河北廊坊 065000;
3.
浙江大学海洋学院, 杭州 310058;
4.
中国石油化工股份有限公司石油勘探开发研究院, 北京 100083;
5.
中海石油(中国)有限公司深圳分公司, 广州 510240

详细信息

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

中图分类号: P618.13

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文章访问数: 548
HTML全文浏览量: 9
PDF下载量: 498
被引次数: 0

Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

1.
CNOOC Research Institute, Beijing 100028, China;
2.
China Petroleum Pipeline Engineering Co., Ltd. International, Langfang, Hebei 065000, China;
3.
Ocean College, Zhejiang University, Hangzhou 310058, China;
4.
Petroleum Exploration & Production Research Institute, SINOPEC, Beijing 100083, China;
5.
Shenzhen Branch of CNOOC Ltd., Guangzhou 510240, China

摘要

摘要: 在被动大陆边缘盆地，水道作为深水油气的主要储集体，是深水油气勘探的重要目标。在下刚果盆地，由于盐构造的多期活动导致对水道砂体的展布规律认识不清。研究水道和盐构造的交互作用方式有利于预测含盐盆地中水道砂体的平面分布。利用三维地震资料，在盐构造与深水水道广泛发育的下刚果盆地研究盐构造与深水水道的交互作用，建立了盐构造与水道的交互作用模式。盐构造与水道的交互作用方式主要有6种，分别为限制、改向、封堵、侵蚀、迁移和剥蚀。盐构造的活动时期与水道形成演化时期的先后关系、水道中重力流的侵蚀能力决定了盐构造与水道的交互作用方式。水道经过早期发育的盐构造且水道中重力流侵蚀能力较弱多发生限制和改向；若水道中重力流侵蚀能力很强，可发生水道对盐构造的侵蚀；若盐构造的规模较大，其可阻止水道向下游输送沉积物并造成水道中重力流的回流，形成朵体沉积。若水道与盐构造同时活动多发生水道的迁移。晚期活动的盐构造可导致其上方的水道沉积体遭受剥蚀。
- 盐构造 /
- 深水水道 /
- 迁移 /
- 交互作用 /
- 下刚果盆地
Abstract: Submarine channels as the main reservoir of deep-water oil and gas is an important goal of deep-water oil and gas exploration in passive continental margin basin. The multi-periodic tectonic activities of the salt structures result in being not clear about the distribution law of channel sand body in the Lower Congo Basin. The research on interactions between submarine channels and salt structures contributes to predict the distribution of channel sand body. In salt structures and submarine channels widely developed area of Lower Congo Basin, based on three-dimensional seismic data, the interactions between salt structures and submarine channels are analyzed and build the interaction model of salt structures related to submarine channels is established. Six submarine channels-salt structures interactions can be defined, respectively, as confinement, diversion, blocking, corrosion, deflection, and erosion. The interactions between channels and salt structures may be dictated by the timing of salt structural activities related to the channel development and the erosional power of the channels. Salt structures which predate the channel development and the weak erosional power of the flows within the submarine channels cause channels to take a moderate confinement or diversion. When the erosional power of the flows is strong enough, submarine channels can continue to incise across the salt structures. The large-scale salt structures can block the submarine channels causing reflection of turbidity alone the submarine channel, and lobes develop. Activities of the salt structures which are consistent with channels development may cause deflection. Overlying submarine channels which predate salt structures may be eroded.
- salt structures /
- deepwater channel /
- deflection /
- interactions /
- Lower Congo Basin

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[1]	付志方, 宫越, 苏玉山, 郭荣涛, 林东升, 汲生珍. 被动陆缘深水海底限制性水道三维地震表征及沉积演化 . 沉积学报, 2024, 42(1): 228-237. doi: 10.14027/j.issn.1000-0550.2022.031
[2]	宫越, 郭荣涛, 张忠民, 苏玉山, 林东升, 王兴华, 吴高奎. 刚果扇盆地深水沉积体系及控制因素研究——以渐新统-中新统为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.113
[3]	田冬梅, 姜涛. 深水水道沉积动力学发展现状与展望 . 沉积学报, 2024, 42(4): 1107-1127. doi: 10.14027/j.issn.1000-0550.2022.158
[4]	李华, 何明薇, 邱春光, 王英民, 何幼斌, 徐艳霞, 何瑞武. 深水等深流与重力流交互作用沉积（2000—2022年）研究进展 . 沉积学报, 2023, 41(1): 18-36. doi: 10.14027/j.issn.1000-0550.2022.027
[5]	赵晓明, 刘飞, 葛家旺, 冯潇飞, 张喜, 张文彪, 杨宝泉, 杨莉. 深水水道沉积构型单元分级与结构样式 . 沉积学报, 2023, 41(1): 37-51. doi: 10.14027/j.issn.1000-0550.2022.048
[6]	吴高奎, 张忠民, 陈华, 郭荣涛, 孔凡军, 宫越, 徐海, 张德民. 下刚果盆地中新统重力流沉积演化及控制因素 . 沉积学报, 2023, 41(1): 73-84. doi: 10.14027/j.issn.1000-0550.2022.032
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[11]	黄文奥, 赵晓明, 谭程鹏, 葛家旺, 冯双奇, 李晨曦, 陆文明. 西秦岭直合隆地区三叠系深水水道沉积模式分析 . 沉积学报, 2020, 38(5): 1061-1075. doi: 10.14027/j.issn.1000-0550.2019.097
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盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

1. 中海油研究总院, 北京 100028;

2. 中国石油管道局工程有限公司国际事业部, 河北廊坊 065000;

3. 浙江大学海洋学院, 杭州 310058;

4. 中国石油化工股份有限公司石油勘探开发研究院, 北京 100083;

5. 中海石油(中国)有限公司深圳分公司, 广州 510240

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

收稿日期: 2016-11-24
修回日期: 2017-02-09
刊出日期: 2017-12-10

中图分类号: P618.13

关键词:

盐构造 /

深水水道 /

迁移 /

交互作用 /

下刚果盆地

摘要: 在被动大陆边缘盆地，水道作为深水油气的主要储集体，是深水油气勘探的重要目标。在下刚果盆地，由于盐构造的多期活动导致对水道砂体的展布规律认识不清。研究水道和盐构造的交互作用方式有利于预测含盐盆地中水道砂体的平面分布。利用三维地震资料，在盐构造与深水水道广泛发育的下刚果盆地研究盐构造与深水水道的交互作用，建立了盐构造与水道的交互作用模式。盐构造与水道的交互作用方式主要有6种，分别为限制、改向、封堵、侵蚀、迁移和剥蚀。盐构造的活动时期与水道形成演化时期的先后关系、水道中重力流的侵蚀能力决定了盐构造与水道的交互作用方式。水道经过早期发育的盐构造且水道中重力流侵蚀能力较弱多发生限制和改向；若水道中重力流侵蚀能力很强，可发生水道对盐构造的侵蚀；若盐构造的规模较大，其可阻止水道向下游输送沉积物并造成水道中重力流的回流，形成朵体沉积。若水道与盐构造同时活动多发生水道的迁移。晚期活动的盐构造可导致其上方的水道沉积体遭受剥蚀。

English Abstract

Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

1. CNOOC Research Institute, Beijing 100028, China;

2. China Petroleum Pipeline Engineering Co., Ltd. International, Langfang, Hebei 065000, China;

3. Ocean College, Zhejiang University, Hangzhou 310058, China;

4. Petroleum Exploration & Production Research Institute, SINOPEC, Beijing 100083, China;

5. Shenzhen Branch of CNOOC Ltd., Guangzhou 510240, China

Received Date: 2016-11-24
Rev Recd Date: 2017-02-09
Publish Date: 2017-12-10

Keywords:

Abstract: Submarine channels as the main reservoir of deep-water oil and gas is an important goal of deep-water oil and gas exploration in passive continental margin basin. The multi-periodic tectonic activities of the salt structures result in being not clear about the distribution law of channel sand body in the Lower Congo Basin. The research on interactions between submarine channels and salt structures contributes to predict the distribution of channel sand body. In salt structures and submarine channels widely developed area of Lower Congo Basin, based on three-dimensional seismic data, the interactions between salt structures and submarine channels are analyzed and build the interaction model of salt structures related to submarine channels is established. Six submarine channels-salt structures interactions can be defined, respectively, as confinement, diversion, blocking, corrosion, deflection, and erosion. The interactions between channels and salt structures may be dictated by the timing of salt structural activities related to the channel development and the erosional power of the channels. Salt structures which predate the channel development and the weak erosional power of the flows within the submarine channels cause channels to take a moderate confinement or diversion. When the erosional power of the flows is strong enough, submarine channels can continue to incise across the salt structures. The large-scale salt structures can block the submarine channels causing reflection of turbidity alone the submarine channel, and lobes develop. Activities of the salt structures which are consistent with channels development may cause deflection. Overlying submarine channels which predate salt structures may be eroded.

引用本文:

Citation:

CHEN Liang, ZHAO QianHui, WANG YingMin, SUN HongJun, WAN QiongHua, TANG Wu, ZHAO Peng. Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011

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盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

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Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

计量

目录

盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

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Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

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盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

作者简介: 陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

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Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

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盐构造与深水水道的交互作用——以下刚果盆地为例

doi: 10.14027/j.cnki.cjxb.2017.06.011

作者简介: 陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

English Abstract

Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn

作者简介:
陈亮,男,1986年出生,工程师,深水层序地层与沉积、储层预测,E-mail:chenliang29@cnooc.com.cn