2012
DOI: 10.5047/eps.2012.04.011
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Variability of megathrust earthquakes in the world revealed by the 2011 Tohoku-oki Earthquake

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Cited by 15 publications
(11 citation statements)
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References 43 publications
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“…This eliminates the possibility of (D) for the different tsunami excitation. Speaking about (E), the results from both the local and far-field tsunami magnitude give consistent results in Equations (4) and (5). Therefore, the effect of local ocean-bottom structures alone is not the reason.…”
Section: Discussionsupporting
confidence: 52%
See 2 more Smart Citations
“…This eliminates the possibility of (D) for the different tsunami excitation. Speaking about (E), the results from both the local and far-field tsunami magnitude give consistent results in Equations (4) and (5). Therefore, the effect of local ocean-bottom structures alone is not the reason.…”
Section: Discussionsupporting
confidence: 52%
“…The 1952 Kamchatka earthquake of Mw 9.0 and the 1964 Alaska earthquake of Mw9.2 are pointed out to be of ADDS type, while the 1960 Chile earthquake of Mw9.5 and the 2010 Maule earthquake of Mw8.8 are of ASSS [4,5]. Speaking about the 2004 Sumatra-Andaman earthquake of Mw9.3, the faulting process is peculiar.…”
Section: Diversity Of Megathrust Earthquakes In the Worldmentioning
confidence: 99%
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“…Globally studies of subducting seamount systems suggest that large fracture zones are formed surrounding the seamount, and the highly fractured region can act as barriers to hinder the rupture propagation (e.g., Wang & Bilek 2011). Because the stress concentration in and around the fracture zones is high and may easily reach failure criteria, the seamount can trigger (e.g., Kumagai et al 2012;Koyama et al 2013) the failure of highly stressed asperities in the neighborhood, nucleating as a great earthquake (e.g., Kumagai et al 2012;Koyama et al 2013). Previous studies also suggest that seamounts cause persistent fault creep (e.g., Singh et al 2011) TPGA are relatively aseismic (Song and Simons, 2003).…”
Section: Rupture Segment 2 (Zone 2 16°n-19°n)mentioning
confidence: 99%
“…Koyama et al 2013). A simple classification based on three criteria, alongstrike segment boundary, along-dip segmentation and the direction of collision (orthogonal or oblique), although useful to sort out some basic differences, still lacks the necessary details and hence forces one to think in terms of these end members only.…”
Section: Mega-thrust Earthquakesmentioning
confidence: 99%