Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations

Abstract Theoretical analyses using a rate‐ and state‐dependent friction law have shown quasistatic and stable slip behaviors following velocity weakening. We estimated spatiotemporal slip distributions for six slow slip events (SSEs) off the Boso Peninsula, Japan, from Global Navigation Satellite S...

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Main Authors: Takuma Kobayashi, Toshinori Sato
Format: Article
Language:English
Published: Wiley 2021-10-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2021GL095690
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author Takuma Kobayashi
Toshinori Sato
author_facet Takuma Kobayashi
Toshinori Sato
author_sort Takuma Kobayashi
collection DOAJ
description Abstract Theoretical analyses using a rate‐ and state‐dependent friction law have shown quasistatic and stable slip behaviors following velocity weakening. We estimated spatiotemporal slip distributions for six slow slip events (SSEs) off the Boso Peninsula, Japan, from Global Navigation Satellite System data and plotted their shear stress variations vs. slip velocity, here called “trajectories.” Most trajectories are similar to theoretical stable trajectories, implying that the Boso SSEs represent a quasistatic and stable process, and that the gradient of the trajectories during slip acceleration is equal to the product of the friction coefficients of the slipping plates (a–b) and the effective normal stress (σn′). Taking (a–b) = −0.003, we estimate that the effective normal stresses during the SSEs were 10–50 MPa at 12.5–20.5 km depth. These values are much smaller than the lithostatic pressures at those depths, implying high pore pressures on the slow slip interface.
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spelling doaj-art-abd807d1740d474885be2af901129cd82025-08-20T03:22:14ZengWileyGeophysical Research Letters0094-82761944-80072021-10-014820n/an/a10.1029/2021GL095690Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress VariationsTakuma Kobayashi0Toshinori Sato1Graduate School of Science Chiba University Chiba JapanGraduate School of Science Chiba University Chiba JapanAbstract Theoretical analyses using a rate‐ and state‐dependent friction law have shown quasistatic and stable slip behaviors following velocity weakening. We estimated spatiotemporal slip distributions for six slow slip events (SSEs) off the Boso Peninsula, Japan, from Global Navigation Satellite System data and plotted their shear stress variations vs. slip velocity, here called “trajectories.” Most trajectories are similar to theoretical stable trajectories, implying that the Boso SSEs represent a quasistatic and stable process, and that the gradient of the trajectories during slip acceleration is equal to the product of the friction coefficients of the slipping plates (a–b) and the effective normal stress (σn′). Taking (a–b) = −0.003, we estimate that the effective normal stresses during the SSEs were 10–50 MPa at 12.5–20.5 km depth. These values are much smaller than the lithostatic pressures at those depths, implying high pore pressures on the slow slip interface.https://doi.org/10.1029/2021GL095690Slow slip eventseffective normal stressquasistatic and stable slip behaviorhigh pore pressureoff the Boso Peninsula
spellingShingle Takuma Kobayashi
Toshinori Sato
Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
Geophysical Research Letters
Slow slip events
effective normal stress
quasistatic and stable slip behavior
high pore pressure
off the Boso Peninsula
title Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
title_full Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
title_fullStr Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
title_full_unstemmed Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
title_short Estimating Effective Normal Stress During Slow Slip Events From Slip Velocities and Shear Stress Variations
title_sort estimating effective normal stress during slow slip events from slip velocities and shear stress variations
topic Slow slip events
effective normal stress
quasistatic and stable slip behavior
high pore pressure
off the Boso Peninsula
url https://doi.org/10.1029/2021GL095690
work_keys_str_mv AT takumakobayashi estimatingeffectivenormalstressduringslowslipeventsfromslipvelocitiesandshearstressvariations
AT toshinorisato estimatingeffectivenormalstressduringslowslipeventsfromslipvelocitiesandshearstressvariations