Joint Inversion of Active Sources and Ambient Noise for Near-Surface Structures: A Case Study in the Balikun Basin, China

被引:10
作者
Luo, Yinhe [1 ,4 ]
Lin, Jing [1 ]
Yang, Yingjie [2 ,3 ]
Wang, Limin [1 ]
Yang, Xiaozhou [1 ]
Xie, Jingyun [1 ]
机构
[1] China Univ Geosci, Hubei Subsurface Multiscale Imaging Lab SMIL, Inst Geophys & Geomat, Wuhan 430074, Hubei, Peoples R China
[2] Macquarie Univ, Ctr Excellence Core Crust Fluid Syst CCFS, Australian Res Council, Sydney, NSW 2109, Australia
[3] Macquarie Univ, Dept Earth & Planetary Sci, GEMOC, Sydney, NSW 2109, Australia
[4] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China
基金
美国国家科学基金会;
关键词
CRUSTAL STRUCTURE BENEATH; SHEAR-WAVE VELOCITY; DABIE OROGENIC BELT; LINEAR RADON-TRANSFORM; SEISMIC NOISE; MULTICHANNEL ANALYSIS; DISPERSIVE ENERGY; TOMOGRAPHY; RAYLEIGH; FIELD;
D O I
10.1785/0220180140
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
The multichannel analysis method of surface waves (MASW) is widely used to image S-wave velocities (VS) of the near surface. The MASW method can typically image VS structures at depths down to several tens of meters. However, this investigation depth is insufficient to meet the requirements of some engineering projects. Ambient noise tomography (ANT) is an appealing alternative method to map greater depths due to its ability to obtain low-frequency surface waves from ambient noise. Combining active and ambient noise surface-wave measurements helps to extend the investigation depth of near-surface VS structures. In this study, we develop a joint inversion method of combining active sources and ambient noise in a near-surface S-wave velocity investigation. We demonstrate the effectiveness of our methods using data from a surface-wave survey project in the Balikun basin, China, as a case study. We extract dispersion curves of fundamental-mode Rayleigh waves from the active source and ambient noise survey, respectively. We combine these two sets of dispersion curves to determine local Rayleigh-wave dispersion curves. Finally, we build a 2D VS model beneath the Balikun basin by inverting the resulting local dispersion curves. Our results demonstrate that combining these two sets of dispersion curves from active and ambient noise data is an effective approach to increasing investigation depth of near-surface structures.
引用
收藏
页码:2256 / 2265
页数:10
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