Fault Healing and Asperity Partitioning on a Frictionally Heterogeneous Laboratory Fault
Name
JGR Solid Earth - 2025 - Song - Fault Healing and Asperity Partitioning on a Frictionally Heterogeneous Laboratory Fault.pdf
Description
Published version
Size
3.13 MB
Format
Adobe PDF
Checksum (MD5)
5ec516b6f60b4630a3179580e50d3cd3
Author(s)
Song, Jun Young
Cattania, Camilla
McLaskey, Gregory C
Date Issued
November 27, 2025
Journal
Journal of Geophysical Research: Solid Earth
Publisher
American Geophysical Union
Citation
Song, J. Y., Cattania, C., & McLaskey, G. C. (2025). Fault healing and asperity partitioning on a frictionally heterogeneous laboratory fault. Journal of Geophysical Research: Solid Earth, 130, e2025JB032055.
Version
Final published version
Abstract
Natural faults likely include both Velocity‐Weakening (VW) and Velocity‐Strengthening (VS) areas. We developed a laboratory method to replicate this frictional heterogeneity using a 760 mm long Polymethyl methacrylate (PMMA) block with 11 VW patches (bare PMMA) separated by VS barriers (Teflon tape). We compared the behavior of this Multiple Patches (MP) arrangement to those from One single VW Patch (OP) with the same total VW fault area. Seismic events that occurred in clusters with foreshocks and aftershocks were observed only in the MP tests, and total slip, maximum slip rate, seismic moment, and recurrence time of the largest event (termed the mainshock) in a slip cycle, were an order of magnitude smaller in the MP tests compared to the OP tests. Slower loading rates, corresponding to longer recurrence time, produced larger mainshock magnitudes in the OP tests, as expected due to fault healing. In contrast, the mainshock magnitude in the MP tests decreased with increasing recurrence time due to the increased effectiveness of VS barriers at slower loading rates. In some MP tests, foreshock‐like events migrated at ∼0.7 m/s, followed by faster reverse migration at ∼7 m/s, resembling Rapid Tremor Reversal (RTR) in subduction zones. We used a numerical simulation to quantitatively reproduce the RTR‐like behavior, help explain its mechanics, and constrain the friction properties of the laboratory system. Overall, our findings highlight how identical structural features on heterogeneous faults can behave differently under different loading conditions due to the velocity dependence of VS barriers.
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DOI of Published Version
https://doi.org/10.1029/2025jb032055
