密度羽流构型特征、控制因素及其对深水沉积的启示&#x02014;&#x02014;对河口和其他环境中密度羽流进行的全球卫星调查

SHANMUGAM G

doi:10.11698/PED.2018.04.07

石油勘探与开发 >

2018 , Vol. 45 >Issue 4: 608 - 625

DOI: https://doi.org/10.11698/PED.2018.04.07

油气勘探

密度羽流构型特征、控制因素及其对深水沉积的启示——对河口和其他环境中密度羽流进行的全球卫星调查

SHANMUGAM G

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Department of Earth and Environmental Sciences, The University of Texas at Arlington, Arlington, TX 76019, USA

Shanmugam G（1944-）,男,博士,美国德克萨斯州立大学教授,主要从事过程沉积学、事件沉积学、层序地层学、成岩作用、烃源岩地球化学等多方面研究。地址：Department of Earth and Environmental Sciences,The University of Texas at Arlington,Arlington, TX 76019, USA。E-mail: shanshanmugam@aol.com

收稿日期: 2018-02-02

修回日期: 2018-06-11

网络出版日期: 2018-05-28

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A global satellite survey of density plumes at river mouths and at other environments: Plume configurations, external controls, and implications for deep-water sedimentation

SHANMUGAM G

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Department of Earth and Environmental Sciences, The University of Texas at Arlington, Arlington, TX 76019, USA

Received date: 2018-02-02

Revised date: 2018-06-11

Online published: 2018-05-28

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摘要

基于对美国国家航空和航天局（NASA）数千幅卫星图像的系统汇编,对45个密度羽流（包含21条主要河流和6种不同的沉积环境）进行实例分析,首次揭示现代环境中各种密度羽流自然构型变化特征,指出密度羽流至少有24种构型。研究发现密度羽流受多达18种包括海洋、气象和其他复杂因素控制：①中国黄河受到潮汐和河道变化的影响;②中国长江在冬季受陆架潮流和潮汐垂直混合的影响;③阿根廷和乌拉圭里约热内卢的拉普拉塔河口受洋流控制;④美国加利福尼亚州旧金山湾受潮流影响;⑤印度洋马纳尔湾受季风环流影响;⑥埃及红海受风成尘埃影响;⑦美国大西洋边缘受飓风气旋影响;⑧斯里兰卡受海啸影响;⑨阿拉斯加柯柏河受高坡辫状河三角洲的影响;⑩伊利湖受湖震影响;?纳米比亚大陆边缘受上升涌流影响;?白令海受浮游生物的影响;?大西洋大巴哈马海岸受鱼类活动影响;?印度尼西亚受火山活动影响;?格陵兰岛受冰川融化的影响;?南太平洋受珊瑚礁的影响;?卡罗莱纳州大陆凸起受地形坑洼的影响;?日本大槌湾受内部狂浪控制。河流-洪水成因的异重流以泥质为主,且往往出现在内陆架靠近海岸线的沉积环境中;从成因机制上讲,异重流无法通过陆架把砂砾输送到深海;此外,野外观察表明这类异重流不能在深水环境中形成米级厚度的砂层。因此,河流-洪水触发的异重岩不可能成为深水沉积储集层,除非另有证据。图44表1参91

关键词： NASA卫星; 密度羽流; 河口环境; 控制因素; 异重流; 海底扇; 深水沉积储集层

本文引用格式

SHANMUGAM G . 密度羽流构型特征、控制因素及其对深水沉积的启示——对河口和其他环境中密度羽流进行的全球卫星调查[J]. 石油勘探与开发, 2018 , 45(4) : 608 -625 . DOI: 10.11698/PED.2018.04.07

Abstract

The U. S. National Aeronautics and Space Administration (NASA) has archived thousands of satellite images of density plumes in its online publishing outlet called 'Earth Observatory' since 1999. Although these images are in the public domain, there has not been any systematic compilation of configurations of density plumes associated with various sedimentary environments and processes. This article, based on 45 case studies covering 21 major rivers (e.g., Amazon, Betsiboka, Congo [Zaire], Copper, Hugli [Ganges], Mackenzie, Mississippi, Niger, Nile, Rhone, Rio de la Plata, Yellow, Yangtze, Zambezi, etc.) and six different depositional environments (i.e., marine, lacustrine, estuarine, lagoon, bay, and reef), is the first attempt in illustrating natural variability of configurations of density plumes in modern environments. There are, at least, 24 configurations of density plumes. An important finding of this study is that density plumes are controlled by a plethora of 18 oceanographic, meteorological, and other external factors. Examples are: 1) Yellow River in China by tidal shear front and by a change in river course; 2) Yangtze River in China by shelf currents and vertical mixing by tides in winter months; 3) Rio de la Plata Estuary in Argentina and Uruguay by Ocean currents; 4) San Francisco Bay in California by tidal currents; 5) Gulf of Manner in the Indian Ocean by monsoonal currents; 6) Egypt in Red Sea by Elian dust; 7) U.S. Atlantic margin by cyclones; 8) Sri Lanka by tsunamis; 9) Copper River in Alaska by high-gradient braid delta; 10) Lake Erie by seiche; 11) continental margin off Namibia by upwelling; 12) Bering Sea by phytoplankton; 13) the Great Bahama Bank in the Atlantic Ocean by fish activity; 14) Indonesia by volcanic activity; 15) Greenland by glacial melt; 16) South Pacific Ocean by coral reef; 17) Carolina continental Rise by pockmarks; and 18) Otsuchi Bay in Japan by internal bore. The prevailing trend in promoting a single type of river-flood triggered hyperpycnal flow is flawed because there are 16 types of hyperpycnal flows. River-flood derived hyperpycnal flows are muddy in texture and they occur close to the shoreline in inner shelf environments. Hyperpycnal flows are not viable transport mechanisms of sand and gravel across the shelf into the deep sea. The available field observations suggest that they do not form meter-thick sand layers in deep water settings. For the above reasons, river-flood triggered hyperpycnites are considered unsuitable for serving as petroleum reservoirs in deep-water environments until proven otherwise.

Key words： NASA satellites; density plumes; river-mouth environments; controlling factors; hyperpycnal flows; submarine fans; deep-water reservoirs

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