Propagation and Dispersion Characteristics of Scholte Wave in VTI Media with the Presence of Irregular Seabed

被引：0

作者：

Xiaobo Liu ^{[1
,2
]}

Yun Wang ^{[3
]}

Jianlei Zhang ^{[4
,5
]}

Haifeng Chen ^{[4
,5
]}

Hua Zhang ^{[4
,5
]}

机构：

[1] School of Ocean Sciences, China University of Geosciences

[2] Key Laboratory of Polar Geology and Marine Mineral Resources, China University of Geosciences

[3] School of Geophysics and Information Technology, China University of Geosciences

[4] Research & Development Center,BGP Inc, CNPC

[5] National Engineering Research Center for Oil and Gas Exploration Computer Software

来源：

Journal of Earth Science | 2024年 / 35卷 / 02期

基金：

北京市自然科学基金; 中国国家自然科学基金;

关键词：

D O I：

暂无

中图分类号：

P631.46 [];

学科分类号：

摘要：

INTRODUCTION Surface waves propagating along the seafloor are generally called Scholte waves, and were first discovered and studied in the early 1950s(Kugler et al., 2005; Buchen and Ben-Hador, 1996). Scholte waves exhibit a dispersion phenomenon, which implies that their velocity varies with frequency. Low-frequency Scholte waves can propagate over long distances on the seabed with little attenuation(Bohlen et al., 2004).

引用

页码：722 / 725

页数：4

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