Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

S (Solid Earth Sciences ) » S-CG Complex & General

[S-CG45] Science of slow-to-fast earthquakes

Mon. May 26, 2025 1:45 PM - 3:15 PM International Conference Room (IC) (International Conference Hall, Makuhari Messe)

convener:Aitaro Kato(Earthquake Research Institute, the University of Tokyo), Asuka Yamaguchi(Atomosphere and Ocean Research Institute, The University of Tokyo), Ryoko Nakata(Graduate School of Science, The University of Tokyo), Kurama Okubo(National Research Institute for Earth Science and Disaster Resilience), Chairperson:Aitaro Kato(Earthquake Research Institute, the University of Tokyo), Ryoko Nakata(Graduate School of Science, The University of Tokyo)

2:00 PM - 2:15 PM

[SCG45-02] Sparse fault representation based on moment tensor interpolation

*Julien Thurin1 (1.University of Alaska Fairbanks)

Keywords:Finite-fault, Source charaterization, Inversion, Numerical modeling

Accurate representations of large earthquake sources are crucial for understanding rupture processes and improving seismic hazard assessments. Although finite-fault models can represent complex slip distributions, they are often overparameterized and require strong regularization. Conversely, multiple point-source approaches offer considerable simplicity but struggle to reproduce near-field static displacements and high-frequency signals. We present a sparse fault parametrization that bridges the gap between classical finite-fault and point-source models by leveraging the geometric structure of the seismic moment tensor. Using a few “key” tensors as centroids of a continuous tensor field, we show that interpolating eigenvalues and eigenvectors separately preserve source type and provide smooth transitions between orientations. This interpolation framework enables us to (1) approximate detailed finite-fault models—which we demonstrate on the USGS NEIC slip for the 2024 Noto earthquake—with a few key moment tensors and (2) upscale these sparse models for forward simulations in 3D spectral-element solvers, preserving both the dynamic and static components of the wavefield. Our results confirm that this sparse representation can provide comparable displacement fields to finite-fault models despite requiring fewer parameters. These advances highlight the potential of sparse, moment-tensor-based models for rapid-response earthquake source characterization and high-fidelity forward modeling in complex 3D Earth structures.