Slip-Weakening and Rate-Strengthening Friction Law for Shallow Layer Above the Seismogenic Zone

ABSTRACT Accurate modeling of slip-rate time functions in the shallow portion above the seismogenic zone on a fault is essential for ground-motion prediction. Recent observations, such as those from the 2016 Kumamoto, central Kyushu, Japan, earthquake (MJMA 7.3), have revealed long-period ground motions and permanent displacements with long rise times near the surface fault, indicating that contributions of the shallow fault portion must be considered in addition to strong-motion generation areas within the deep seismogenic zone. In this study, we propose a friction law applicable to fault surfaces in an elastic medium, in which a slip-rate strengthening mechanism operates below a characteristic slip rate Vc, supplementing the standard slip-weakening law. Pure slip weakening is applied within the seismogenic zone, whereas the slip-rate strengthening branch is applied to the shallow fault portion above the seismogenic zone. Dynamic rupture simulations using a 3D elastic model with a shallow stress drop of 0 MPa demonstrate that the model incorporating slip-rate strengthening suppresses slip rates on the shallow layer and reduces peak ground velocity amplitudes within approximately 1 km of the surface fault compared with a purely slip-weakening model, despite producing nearly identical overall rupture propagation and seismic moments. Sensitivity analyses further show that δ, which is the incremental parameter of the rate-strengthening friction law, primarily controls peak slip rate through its influence on the effective fracture energy, whereas Vc mainly affects rupture duration, particularly the slip-termination phase. Although long Dc or negative stress drop has traditionally been used to mimic suppression of shallow slip rates, the proposed law more efficiently reproduces a gradual slip-rate onset, prolonged slip duration, and peak suppression, compared to friction laws without slip-rate dependence that have a similar effective fracture energy. The proposed friction formulation is simple to implement, computationally efficient, and useful for large-scale source-model exploration and applications in near-fault ground-motion prediction.

Authors

Institutions

Publication Details

Journal
Bulletin of the Seismological Society of America
Published
2026-08-17
DOI
https://doi.org/10.1785/0120260032
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Slip-Weakening and Rate-Strengthening Friction Law for Shallow Layer Above the Seismogenic Zone

Ken Miyakoshi, Toshiaki Sato, Yuko Kase, Kiyoshi IRIE et al.
Bulletin of the Seismological Society of America
earthquake and tectonic studies
article

Slip-Weakening and Rate-Strengthening Friction Law for Shallow Layer Above the Seismogenic Zone

Ken Miyakoshi, Toshiaki Sato, Yuko Kase, Kiyoshi IRIE, Haruhiko Torita
article en

Abstract

ABSTRACT Accurate modeling of slip-rate time functions in the shallow portion above the seismogenic zone on a fault is essential for ground-motion prediction. Recent observations, such as those from the 2016 Kumamoto, central Kyushu, Japan, earthquake (MJMA 7.3), have revealed long-period ground motions and permanent displacements with long rise times near the surface fault, indicating that contributions of the shallow fault portion must be considered in addition to strong-motion generation areas within the deep seismogenic zone. In this study, we propose a friction law applicable to fault surfaces in an elastic medium, in which a slip-rate strengthening mechanism operates below a characteristic slip rate Vc, supplementing the standard slip-weakening law. Pure slip weakening is applied within the seismogenic zone, whereas the slip-rate strengthening branch is applied to the shallow fault portion above the seismogenic zone. Dynamic rupture simulations using a 3D elastic model with a shallow stress drop of 0 MPa demonstrate that the model incorporating slip-rate strengthening suppresses slip rates on the shallow layer and reduces peak ground velocity amplitudes within approximately 1 km of the surface fault compared with a purely slip-weakening model, despite producing nearly identical overall rupture propagation and seismic moments. Sensitivity analyses further show that δ, which is the incremental parameter of the rate-strengthening friction law, primarily controls peak slip rate through its influence on the effective fracture energy, whereas Vc mainly affects rupture duration, particularly the slip-termination phase. Although long Dc or negative stress drop has traditionally been used to mimic suppression of shallow slip rates, the proposed law more efficiently reproduces a gradual slip-rate onset, prolonged slip duration, and peak suppression, compared to friction laws without slip-rate dependence that have a similar effective fracture energy. The proposed friction formulation is simple to implement, computationally efficient, and useful for large-scale source-model exploration and applications in near-fault ground-motion prediction.

Bulletin of the Seismological Society of America
Sasaki Institute (JP), Geological Survey of Japan (JP), National Institute of Advanced Industrial Science and Technology (JP)
Peace, Justice and strong institutions
Openalex Percentile: Top 12%
earthquake and tectonic studies
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.