Zobrazeno 1 - 10
of 653
pro vyhledávání: '"Megathrust earthquake"'
Publikováno v:
Earth, Planets and Space, Vol 76, Iss 1, Pp 1-19 (2024)
Abstract After the 2011 Tohoku-oki earthquake, a seafloor observation system observed rapid landward deformation. These seafloor observation data are potentially explicable via modeling of a low-viscosity zone under the subducting plate, called the l
Externí odkaz:
https://doaj.org/article/099c9112ac894bdf8514ec9812c79546
Publikováno v:
Earth, Planets and Space, Vol 76, Iss 1, Pp 1-26 (2024)
Abstract The Nankai trough has repeatedly experienced large megathrust earthquakes at intervals of 100–200 years. The inland region of southwest (SW) Japan has a seismically active period from 50 years before to 10 years after megathrust earthquake
Externí odkaz:
https://doaj.org/article/8f389cee81474566a62e22d95bcca55f
Autor:
Duo Li, Alice‐Agnes Gabriel
Publikováno v:
AGU Advances, Vol 5, Iss 2, Pp n/a-n/a (2024)
Abstract Slow slip events (SSEs) have been observed in spatial and temporal proximity to megathrust earthquakes in various subduction zones, including the 2014 Mw 7.3 Guerrero, Mexico earthquake which was preceded by a Mw 7.6 SSE. However, the underl
Externí odkaz:
https://doaj.org/article/9bf5ad46858042fda4f09422fb2dcade
Autor:
Bunichiro Shibazaki
Publikováno v:
Progress in Earth and Planetary Science, Vol 10, Iss 1, Pp 1-28 (2023)
Abstract This paper summarizes the results of 10 years of research on models of the megathrust earthquake cycles and crustal deformation associated with the 2011 Tohoku-oki earthquake. Several earthquake cycle models have been proposed for the northe
Externí odkaz:
https://doaj.org/article/d75e9d41909643ee9dbc0a8f6cb317ee
Publikováno v:
Progress in Earth and Planetary Science, Vol 10, Iss 1, Pp 1-51 (2023)
Abstract Slow earthquakes are episodic slow fault slips. They form a fundamental component of interplate deformation processes, along with fast, regular earthquakes. Recent seismological and geodetic observations have revealed detailed slow earthquak
Externí odkaz:
https://doaj.org/article/59d7bb4a5c3847b7ad28fb8713f254df
Akademický článek
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Publikováno v:
Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023)
Abstract Numerous normal‐faulting aftershocks in subduction forearcs commonly follow large megathrust earthquakes. Postseismic normal faulting has been explained by stress changes induced by the stress drop along the megathrust. However, details of
Externí odkaz:
https://doaj.org/article/24bfce6d3a2747d5b27066a259738826
Akademický článek
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Akademický článek
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Publikováno v:
Geophysical Research Letters, Vol 49, Iss 17, Pp n/a-n/a (2022)
Abstract A smooth subducting seafloor usually leads to a smooth megathrust, which promotes great earthquakes. We present a case study at the northern Manila Trench to emphasize that the process depends also on sediment accretion and deformation. Here
Externí odkaz:
https://doaj.org/article/ca9573c66e734edfa8a33729296d4576