Morphological differences across the Shumagin-Semidi fault segments control slip behaviors and tsunami genesis in the Aleutian-Alaska subduction zone-Reference-Cited by-同舟云学术

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Morphological differences across the Shumagin-Semidi fault segments control slip behaviors and tsunami genesis in the Aleutian-Alaska subduction zone

Published:2024-09 Issue: Volume:15 Page:100215
ISSN:2666-0334
Container-title:Quaternary Science Advances
language:en
Short-container-title:Quaternary Science Advances

Author:

Qiu Qiang^ORCID,Li Linlin,Yang Xiaodong,Lin Jian,Chua Constance Ting

Publisher

Elsevier BV

Reference78 articles.

1. Earthquake cycle simulations with rate-and-state friction and power-law viscoelasticity;Allison;Tectonophysics,2018

2. Optimizing a model of coseismic rupture for the 22 july 2020 MW 7.8 Simeonof earthquake by exploiting acute sensitivity of tsunami excitation across the shelf break;Bai;J. Geophys. Res. Solid Earth,2022

3. Frictional and structural controls of seismic super-cycles at the Japan trench;Barbot;Earth Planets Space,2020

4. Slow-slip, slow earthquakes, period-two cycles, full and partial ruptures, and deterministic chaos in a single asperity fault;Barbot;Tectonophysics,2019

5. Asthenosphere flow modulated by megathrust earthquake cycles;Barbot;Geophys. Res. Lett.,2018

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