Shallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 Mw 9.0 Tohoku-Oki Earthquake
By Satoshi Ide, A. Baltay, Gregory C. Beroza. Science, 2011
629 citations recorded by the source corpus.
Subfields: Artificial Intelligence, Geophysics
View Paper: https://www.semanticscholar.org/paper/5098e34d018560043fa7a3126d2a55de3d7459ec
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Citations in the corpus
- Numerical Simulation of the 2011 Tohoku Tsunami Based on a New Transient FEM Co-seismic Source: Comparison to Far- and Near-Field Observations (2013, background): “…Institute at the University of Tokyo, all indicated that the earthquake was predominantly thrust with a moment more than Mo ^ 4.0 9 10 22 Nm, and a variety of seismic, geodetic, and tsunami genesis studies concluded that the magnitude was indeed Mw = 9.0 (e.g., IDE et al. 2011; SIMONS et al. 2011).”
- Compressive sensing of the Tohoku‐Oki Mw 9.0 earthquake: Frequency‐dependent rupture modes (2011, background): “However, CS (Figure 2f) finds the locations exactly with super lateral resolution.”
- Gravity anomalies, crustal structure, and seismicity at subduction zones: 1. Seafloor roughness and subducting relief (2015, background): “0 Tohoku-Oki earthquake ruptured 400 km of strike [Ide et al., 2011; Koketsu et al., 2011; Lay et al., 2011; Simons et al., 2011].”
- Source model for generating strong ground motions during the 2011 off the Pacific coast of Tohoku Earthquake (2011, neutral): “Slip distribution models have been inverted using teleseismic, geodetic, and tsunami data by many researchers (e.g., Fujii and Satake, 2011; Ide et al., 2011; Iinuma et al., 2011; Yagi and Nishimura, 2011; Yamanaka, 2011).”
- Tsunami source of the 2011 Tohoku‐Oki earthquake, Japan: Inversion analysis based on dispersive tsunami simulations (2011, background): “Dynamic fault rupture possibly causes larger slip near the surface than predicted by a static model [Mikumo and Miyatake, 1993; Aagaard et al., 2001; Oglesby and Day, 2001; Ide et al., 2011].”