A Sample Generation of Scenario Earthquake Shaking Maps via a Combination of Modal Decomposition and Empirical Copula toward Seismic Hazard Assessment

Monotonic Neural Network for Ground‐Motion Predictions to Avoid Overfitting to Recorded Sites

Ground‐Motion Prediction Model Based on Neural Networks to Extract Site Properties from Observational Records

Building-damage detection method based on machine learning utilizing aerial photographs of the Kumamoto earthquake

Validation of the New Procedures for Evaluating Parameters of Crustal Earthquakes Caused by Long Faults for Ground‐Motion Prediction

Spatial Distribution of Ground‐Motion Variability in Broadband Ground‐Motion Simulations

Appraising the PSHA Earthquake Source Models of Japan, New Zealand, and Taiwan

Updates to the Seismic Activity Models of Japan: Lessons from the Great Tohoku Earthquake

Seismic‐Hazard Analysis of Long‐Period Ground Motion of Megathrust Earthquakes in the Nankai Trough Based on 3D Finite‐Difference Simulation

Validation of the Recipe for Broadband Ground‐Motion Simulations of Japanese Crustal Earthquakes

Broadband Ground‐Motion Simulation Based on the Relationship between High‐ and Low‐Frequency Acceleration Envelopes: Application to the 2003 M w 8.3 Tokachi‐Oki Earthquake

Miniature array analysis of microtremors

Rapid Assessment of High Seismic Intensity Areas of the 2008 M w 7.9 Wenchuan Earthquake Using Satellite SAR Data

Statistical Comparison of National Probabilistic Seismic Hazard Maps and Frequency of Recorded JMA Seismic Intensities from the K-NET Strong-motion Observation Network in Japan during 1997–2006

A New Attenuation Relation for Strong Ground Motion in Japan Based on Recorded Data

3D finite-difference method using discontinuous grids

Boundary shape waveform inversion for two-dimensional basin structure using three-component array data of plane incident wave with an arbitrary azimuth

Basin-induced love waves observed using the strong-motion array at Fuchu, Japan

High-frequency seismic wave radiation from antiplane cohesive zone model and f max as source effect