范文豪^1,,
宋海斌^1,,,
张锟¹,
许鹤翰²,
龚屹¹,
孙绍箐¹
1. 海洋地质国家重点实验室, 同济大学海洋与地球科学学院, 上海 200092
2. 台湾大学海洋研究所, 中国台北

基金项目: 国家重点研发计划（2018YFC0310000），全球变化专项国际合作项目（GASI-GEOGE-05）和国家自然科学基金（41976048，41576047）资助


详细信息

作者简介: 范文豪, 男, 1992年生, 主要从事海洋地球物理研究.E-mail:wenhaofan@tongji.edu.cn

通讯作者: 宋海斌, 教授, 主要从事海洋地球物理与地震海洋学研究.E-mail:hbsong@tongji.edu.cn

中图分类号: P738

收稿日期:2019-09-30
修回日期:2020-03-26
上线日期:2020-07-05

Seismic oceanography study of internal solitary waves in the northeastern South China Sea Basin

FAN WenHao^1,,
SONG HaiBin^1,,,
ZHANG Kun¹,
HSU Hohan²,
GONG Yi¹,
SUN ShaoQing¹
1. State Key laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai 200092, China
2. Institute of Oceanography, Taiwan University, Taipei, China


More Information

Corresponding author: SONG HaiBin,E-mail:hbsong@tongji.edu.cn

MSC: P738

--> Received Date: 30 September 2019
Revised Date: 26 March 2020
Available Online: 05 July 2020


摘要
摘要:以往利用地震海洋学方法发现的内孤立波大多在东沙岛附近，本文在南海海盆东北部首次利用地震海洋学方法发现了海盆中的内孤立波.通过叠前偏移观察该内孤立波细结构的变化，发现内孤立波波形在采集时间段内整体较稳定，内孤立波浅层反射相对深层变化较大.通过改进前人的方法，利用共偏移距道集叠前偏移剖面计算内孤立波视相速度.该方法比直接使用共偏移距道集拟合的共中心点-炮点对曲线线性更好，其计算的内孤立波视相速度为0.82 m·s^-1，内孤立波视传播方向为从NW向SE（172°N方向，0°指向北）.
关键词: 地震海洋学/
内孤立波/
南海海盆/
结构特征/
传播特征

Abstract:In previous work,the internal solitary waves (ISWs)discovered by seismic oceanography are mostly near the Dongsha Island. This paper uses the method of seismic oceanography to find the ISWs in the basin for the first time in the northeastern South China Sea. The pre-stack migration is used to examine the changes of the ISWs structure. It is found that the ISWs waveforms are stable overall during the acquisition period. The shallow reflection of the ISWs has a relatively larger change than the deep. By improving the methods of the predecessors,the ISWs apparent phase velocity is calculated by pre-stack migration profile using the Common Offset Gather (COG). The fitting curve of CMP (Common Mid-Point)-shot point pairs using this method has a better linearity than that using Common Offset Gather directly. The apparent phase velocity of this ISWs using the improved method is 0.82 m·s^-1,and the apparent direction of the ISWs propagation is from NW to SE (172°N,0° pointing north).
Key words:Seismic oceanography/
Internal solitary wave/
South China Sea Basin/
Structural characteristics/
Propagation characteristics



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