A phase unwrapping approach in measuring surface wave phase velocities from ambient noise

被引:0
作者
Xie, Yanan [1 ,2 ]
Luo, Yinhe [1 ,3 ]
Yang, Yingjie [2 ,4 ]
机构
[1] China Univ Geosci, Sch Geophys & Geomat, Hubei Subsurface Multiscale Imaging Key Lab, 388 Lumo Rd, Wuhan 430074, Hubei, Peoples R China
[2] Southern Univ Sci & Technol, Dept Earth & Space Sci, Shenzhen 518055, Peoples R China
[3] China Univ Geosci, Sch Geophys & Geomat, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
[4] Southern Univ Sci & Technol, Guangdong Prov Key Lab Geophys High resolut Imagin, Shenzhen 518055, Peoples R China
基金
美国国家科学基金会;
关键词
Computational seismology; Seismic noise; Surface waves and free oscillations; SEISMIC NOISE; MULTICHANNEL ANALYSIS; RADIAL ANISOTROPY; TAIWAN STRAIT; RAYLEIGH; TOMOGRAPHY; DISPERSION; BENEATH; LOVE;
D O I
10.1093/gji/ggae288
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In the past two decades or so, ambient noise tomography (ANT) has emerged as a powerful tool for investigating high-resolution crustal and upper-mantle structures. A crucial step in the ANT involves extracting phase velocities from cross-correlation functions (CCFs). However, obtaining precise phase velocities can be a formidable challenge, particularly when significant lateral velocity variations exist in shallow subsurface imaging that relies on short-period surface waves from ambient noise. To address this challenge, we propose an unwrapping correction method that enables the accurate extraction of short-period dispersion curves. Our method relies on the examination of the continuity of phase velocities extracted from CCFs between a common station and other neighbouring stations along a linear array. We demonstrate the effectiveness of our approach by applying our method to both synthetic and field data. Both applications suggest our unwrapping correction method can identify and correct unwrapping errors in phase velocity measurements, ensuring the extraction of accurate and reliable dispersion curves at short periods from ambient noise, which is essential for subsequent inversion for subsurface structures.
引用
收藏
页码:694 / 705
页数:12
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