Extent, duration and speed of the 2004 Sumatra–Andaman earthquake imaged by the Hi-Net array
By M. Ishii, P. Shearer, H. Houston, J. Vidale. Nature, 2005
681 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/d9c99f0414884e084c3c7586fb297ff2fa5f08e6
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In Geophysics
Citations in the corpus
- Multiple CMT source analysis of the 2004 Sumatra earthquake (2005, methodology): “A second source is then introduced with an initial location approximately 1� N of the single-source location, with a time delay of approximately 30 s. This time delay is chosen with a rupture speed of � 3 km/s in mind [Ammon et al., 2005; Ishii et al., 2005 ].”
- Seismic imaging: From classical to adjoint tomography (2012, methodology): “The first step of this method is, in essence, a more sophisticated version of the back-projection technique used for imaging earthquake rupture processes (e.g., Ishii et al., 2005; Larmat et al., 2010).”
- Compressive sensing of the Tohoku‐Oki Mw 9.0 earthquake: Frequency‐dependent rupture modes (2011, methodology): “[4] In the time domain, back‐projection of teleseismic P waves [Ishii et al., 2005; Walker and Shearer, 2009; Xu et al., 2009] has been used to image the rupture of earthquakes.”
- Far-field tsunami hazard from mega-thrust earthquakes in the Indian Ocean (2008, background): “Ishii et al. 2005; Banerjee et al. 2007): a first one at (3.4◦N; 94.2◦E) with � u = 18 m and a moment M 0 = 3.7 × 1029 dyn × cm, a second one at (7◦N; 94◦E) with � u = 15 m and M 0 = 5. 1 × 1029 dyn × cm, and a third one at (10.6◦N; 94.1◦E) with � u = 12 m and M 0 = 2.5 × 1029 dyn × cm. We find, on”
- GRACE detects coseismic and postseismic deformation from the Sumatra‐Andaman earthquake (2007, methodology): “…a few hundred km south of the of Sumatra-Andaman earthquake, which does not agree with the results of Han et al. [2006] based on GRACE Level-1 range/rage-rate data and seismic 3 of 5 model prediction of the Sumatra-Andaman rupture or estimate derived from seismic array data [Ishii et al., 2005].”