Characterization and application of submarine seismic ambient noise in the Bohai Sea and Yellow Sea

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Abstract

Submarine seismic ambient noise imaging combines current marine and on-land seismic detection technologies. Based on data from several broadband shallow-sea type ocean bottom seismometers (SOBSs) deployed in the Bohai Sea and north Yellow Sea, this paper analyzes the submarine seismic ambient noise characteristics. It explores the theory, technology, method and application of the submarine seismic ambient noise imaging using the single-point horizontal and vertical spectral ratio method (HVSR). The observations yield the following results: 1) Submarine seismic ambient noise has consistent and constant energy, making it an appropriate passive seismic source for submarine high-frequency surface wave investigation. 2) Using the HVSR approach, a single three-component OBS could differentiate between the basement and sediments. Array seismic observation could be utilized to extract the frequency dispersion curve and invert it to obtain the velocity structure for more accurate stratification. 3) The SOBS we use is suitable for submarine surface wave exploration. 4) Tomography results with greater resolution and deeper penetration could be obtained by combining active and passive sources in a simultaneous inversion of the HVSR and frequency dispersion curve. Seamless land-to-ocean seismic research can be accomplished with submarine seismic ambient noise imaging technologies.
渤海和黄海海底地震环境噪声数据分析及其应用
海底地震环境噪声成像结合了当前的海洋和陆地地震探测技术。本文基于部署在渤海和黄海北部的多台宽带浅海型海底地震仪(SOBS)的数据,分析了海底地震环境噪声特征。本文采用单点水平和垂直谱比法(HVSR),探讨了海底地震环境噪声成像的理论、技术、方法和应用。观测结果如下1)海底地震环境噪声能量稳定、恒定,是海底高频面波研究的合适被动震源。2) 利用高频表面波研究方法,单个三分量 OBS 可以区分基底和沉积。阵列地震观测可用于提取频散曲线并反演,以获得速度结构,从而更准确地进行分层。3) 我们使用的 SOBS 适用于海底表面波探测。4) 将主动源和被动源结合起来,同时反演 HVSR 和频率频散曲线,可以获得分辨率更高、穿透力更强的层析成像结果。利用海底地震环境噪声成像技术,可以实现从陆地到海洋的无缝地震研究。
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