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High‐Resolution Fault‐Rupture Imaging by Combining a Backprojection Method With Binarized MUSIC Spectral Image Calculation
https://nied-repo.bosai.go.jp/records/2893
https://nied-repo.bosai.go.jp/records/289387d2c3da-844e-43e4-9877-80e9e6304892
Item type | researchmap(1) | |||||||||||
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公開日 | 2024-04-29 | |||||||||||
タイトル | ||||||||||||
言語 | en | |||||||||||
タイトル | High‐Resolution Fault‐Rupture Imaging by Combining a Backprojection Method With Binarized MUSIC Spectral Image Calculation | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
著者 |
Mitsutaka Oshima
× Mitsutaka Oshima
× Hiroshi Takenaka
× Makoto Matsubara
|
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抄録 | ||||||||||||
内容記述タイプ | Other | |||||||||||
内容記述 | Abstract Backprojection (BP) methods are widely used for estimating the fault rupture processes; however, they are inherently susceptible to noise. Hence, noise suppression is an important research target. In this paper, we develop a fault rupture imaging method by combining beamforming‐based BP and MUltiple Signal Classification (MUSIC), which realizes artificial noise suppression at a high spatial resolution. The stations are grouped into arrays according to the SH wave radiation coefficients, and MUSIC analysis is performed on each array. The MUSIC spectral images of these arrays are binarized and then multiplied by the BP images. Spatial filtering is also applied to the images based on the possible range of the rupture velocity and rise time. When tested using synthetic test data, the proposed method worked as expected. We then applied this method to the 2016 Kumamoto earthquake by interpolating the travel times from the observed travel times of relocated hypocenters using a 3‐D velocity structure model. In the area of large slip and slip rate approximately 30–50 km from the hypocenter on the Futagawa fault, the spatiotemporal evolution of the fault ruptures and waveform inversion results were generally in harmony. The distributions of the low‐ and high‐frequency seismic radiations are complementary, as is understood in the context of fault rupture physics. This method can aid in understanding and modeling the details of seismic radiation sources, enabling the accurate prediction of strong ground motion even in near‐fault areas. | |||||||||||
言語 | en | |||||||||||
書誌情報 |
en : Journal of Geophysical Research: Solid Earth 巻 127, 号 11, 発行日 2022-11 |
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出版者 | ||||||||||||
言語 | en | |||||||||||
出版者 | American Geophysical Union (AGU) | |||||||||||
ISSN | ||||||||||||
収録物識別子タイプ | EISSN | |||||||||||
収録物識別子 | 2169-9356 | |||||||||||
DOI | ||||||||||||
関連識別子 | 10.1029/2022jb024003 |