The 2011 Magnitude 9.0 Tohoku-Oki Earthquake: Mosaicking the Megathrust from Seconds to Centuries
By Mark Simons, S. Minson, A. Sladen, F. Ortega, Junle Jiang, S. Owen, L. Meng, Jean-Paul Ampuero, Shengji Wei, R. Chu and 5 more. Science, 2011
747 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/a0cc9f28e0eae96041364b4618c792a3fa241f3d
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In Geophysics
- D. Jackson
- Fengyan Shi
- James T. Kirby
- Y. Kagan
- Jeffrey C. Harris
- Stephan T. Grilli
- Tayebeh S. Tajalli Bakhsh
- C. Kyriakopoulos
Citations in the corpus
- Source parameter inversion for recent great earthquakes from a decade‐long observation of global gravity fields (2013, methodology): “1 of Wieczorek and Simons [2005]. Therefore, we use the localized spherical harmonic coefficients within the bandwidth, Lh+1 to Ls Lh, from monthly GRACE L2 data.”
- Tohoku earthquake: a surprise? (2011, background): “Simons et al. (2011) propose a 500-1,000 year interval based in part on the historic record.”
- 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.”
- Ionospheric Detection of Natural Hazards (2019, background): “, Simons et al., 607 2011; Bletery et al., 2014; Figure 10a). More recently, Thomas et al. (2018) and Astafyeva & 608 Shults (2019) demonstrated that the GNSS seismo-ionospheric imagery can work for 609”
- GipsyX/RTGx, a new tool set for space geodetic operations and research (2020, background): “many, include synthetic aperture radar (SAR) from aircraft, ocean floating buoys used to determine sea surface height, co-seismic deformation, and ice sheet movement, see [Hensley et al., 2008; Bonnefond et al., 2003; Born et al., 1994; Simons et al., 2011; Doake et al., 2002] for example.”