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Diagnosing Source Geometrical Complexity of Large Earthquakes
Source inversion of W phase: speeding up seismic tsunami warning
An Mw = 7.7 slow earthquake in 1960 near the Aysén Fjord region, Chile
Static and Dynamic Scaling Relations for Earthquakes and Their Implications for Rupture Speed and Stress Drop
Representations of the radiated energy in earthquakes
Spatial heterogeneity of tectonic stress and friction in the crust
Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake
Source Inversion of the W-Phase: Real-time Implementation and Extension to Low Magnitudes
Estimation of radiated energy using the KiK-net downhole records—old method for modern data
Rupture characteristics of major and great (≥ 7.0) megathrust earthquakes from 1990 to 2015: 2. Depth dependence
Estimate of differential stress in the upper crust from variations in topography and strike along the San Andreas fault
Uncertainty estimations for seismic source inversions
Rupture characteristics of major and great (≥ 7.0) megathrust earthquakes from 1990 to 2015: 1. Source parameter scaling relationships
Evidence for a large strike-slip component during the 1960 Chilean earthquake
Joint inversion of high-rate GPS and teleseismic observations for rupture process of the 23 June 2014 (Mw 7.9) Rat Islands archipelago, Alaska, intermediate depth earthquake
W phase source inversion for moderate to large earthquakes (1990-2010)
Joint Inversion of High-Rate GPS and Teleseismic Observations for Rupture Process of the 23 June 2014 Mw 7.9 Rat Islands Archipelago Alaska Intermediate Depth Earthquake
The 22 December 2018 tsunami from flank collapse of Anak Krakatau volcano during eruption
The 2009 Samoa–Tonga great earthquake triggered doublet
Real-time W phase inversion during the 2011 off the Pacific coast of Tohoku Earthquake

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