2022
DOI: 10.1186/s40645-022-00524-0
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A new mechanical perspective on a shallow megathrust near-trench slip from the high-resolution fault model of the 2011 Tohoku-Oki earthquake

Abstract: The 2011 Tohoku-Oki earthquake generated a surprisingly large near-trench slip, and earth scientists have devoted significant attention to understanding why. Some studies proposed special rupture mechanisms, such as extensive dynamic frictional weakening; others simulated this near-trench slip behavior without supposing the extensive dynamic weakening. However, we have not reached a decisive conclusion for this question due to limited spatial near-trench slip resolution. Hence, in this study we use new tsunami… Show more

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Cited by 8 publications
(2 citation statements)
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“…Moreover, the estimated result just after the occurrence of a large earthquake is useful for the forward simulation of tsunami early warning. Although the tsunami waveform data can be directly used in an inversion to estimate the fault model (e.g., Satake 1989;Gusman et al 2012;Kubota et al 2021Kubota et al , 2022, we adopt the use of the tsunami source. This approach improves the solution stability in the quality assurance of tsunami source estimation and the consistency of the tsunami-driven seafloor geodetic data with the GNSS data (crustal deformation data).…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, the estimated result just after the occurrence of a large earthquake is useful for the forward simulation of tsunami early warning. Although the tsunami waveform data can be directly used in an inversion to estimate the fault model (e.g., Satake 1989;Gusman et al 2012;Kubota et al 2021Kubota et al , 2022, we adopt the use of the tsunami source. This approach improves the solution stability in the quality assurance of tsunami source estimation and the consistency of the tsunami-driven seafloor geodetic data with the GNSS data (crustal deformation data).…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, the estimated result just after the occurrence of a large earthquake is useful for the forward simulation of tsunami early warning. Although the tsunami waveform data can be directly used in an inversion to estimate the fault model (e.g., Satake 1989; Gusman et al 2012;Kubota et al 2021Kubota et al , 2022, we adopt the use of the tsunami source. This approach can improve the solution stability in the quality assurance of tsunami source estimation and the consistency of the tsunami-driven sea oor geodetic data with the GNSS data (crustal deformation data).…”
Section: Introductionmentioning
confidence: 99%