Ambient Noise Array Tomography Using Regionalized Phase Velocities From Array-Based Methods

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Kaifeng Zhao, Yingjie Yang, Yinhe Luo, Hao Jin, Chengxin Jiang
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引用次数: 0

Abstract

With the advancement of dense seismic arrays, array-processing methods for ambient noise data have become highly effective in extracting high-quality broadband surface wave dispersion curves from ambient noise. Recent advancements in array data processing methods have enabled the extraction of multimode dispersion curves, offering improved constraints on deep Earth structures. However, these array-based methods often produce regionalized dispersion curves, and conventional phase velocity maps constructed by interpolating these dispersion curves typically have limited resolution, and display smooth images of phase velocities. In this study, we develop an array tomography method aimed at improving the resolution of ambient noise tomography by utilizing dispersion curves extracted through array-based data processing. To demonstrate the effectiveness of our method in enhancing tomography resolution, we construct fundamental-mode 2-D Rayleigh wave phase velocity maps by applying our approach to regionalized dispersion curves obtained from array-based methods in the western United States. By comparing our tomographic results with those from conventional array-based methods, we show that our method can produce more accurate and higher-resolution phase velocity maps. Additionally, our approach is versatile and can be applied to construct high-resolution 1-D and 2-D velocity structures using regionalized phase velocities obtained from various other array-based data processing methods.

基于阵列方法的区域化相速度环境噪声阵列层析成像
随着密集地震阵列的发展,环境噪声数据的阵列处理方法在从环境噪声中提取高质量的宽带表面波频散曲线方面变得非常有效。阵列数据处理方法的最新进展使多模色散曲线的提取成为可能,从而改善了对深部地球结构的约束。然而,这些基于阵列的方法通常产生区域化的色散曲线,并且通过插值这些色散曲线构建的传统相速度图通常具有有限的分辨率,并且显示相速度的平滑图像。在本研究中,我们开发了一种阵列层析成像方法,旨在利用基于阵列的数据处理提取的色散曲线来提高环境噪声层析成像的分辨率。为了证明我们的方法在提高断层扫描分辨率方面的有效性,我们将我们的方法应用于美国西部基于阵列的方法获得的区域化色散曲线,构建了基模二维瑞利波相速度图。通过将我们的层析成像结果与传统的基于阵列的方法进行比较,我们表明我们的方法可以产生更精确和更高分辨率的相速度图。此外,我们的方法是通用的,可以使用从各种其他基于阵列的数据处理方法获得的区域化相速度来构建高分辨率的1-D和2-D速度结构。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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