DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Kinematic Ground-Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations

Abstract

Here, we describe a methodology for generating kinematic earthquake ruptures for use in 3D ground–motion simulations over the 0–5 Hz frequency band. Our approach begins by specifying a spatially random slip distribution that has a roughly wavenumber–squared fall–off. Given a hypocenter, the rupture speed is specified to average about 75%–80% of the local shear wavespeed and the prescribed slip–rate function has a Kostrov–like shape with a fault–averaged rise time that scales self–similarly with the seismic moment. Both the rupture time and rise time include significant local perturbations across the fault surface specified by spatially random fields that are partially correlated with the underlying slip distribution. We represent velocity–strengthening fault zones in the shallow (<5 km) and deep (>15 km) crust by decreasing rupture speed and increasing rise time in these regions. Additional refinements to this approach include the incorporation of geometric perturbations to the fault surface, 3D stochastic correlated perturbations to the P– and S–wave velocity structure, and a damage zone surrounding the shallow fault surface characterized by a 30% reduction in seismic velocity. We demonstrate the approach using a suite of simulations for a hypothetical Mw 6.45 strike–slip earthquake embedded in a generalized hard–rock velocity structure. The simulation resultsmore » are compared with the median predictions from the 2014 Next Generation Attenuation–West2 Project ground–motion prediction equations and show very good agreement over the frequency band 0.1–5 Hz for distances out to 25 km from the fault. Additionally, the newly added features act to reduce the coherency of the radiated higher frequency (f>1 Hz) ground motions, and homogenize radiation–pattern effects in this same bandwidth, which move the simulations closer to the statistical characteristics of observed motions as illustrated by comparison with recordings from the 1979 Imperial Valley earthquake.« less

Authors:
 [1];  [2]
  1. U.S. Geological Survey, Pasadena, CA (United States)
  2. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Publication Date:
Research Org.:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1420289
Report Number(s):
LLNL-JRNL-736843
Journal ID: ISSN 0037-1106
Grant/Contract Number:  
AC52-07NA27344
Resource Type:
Accepted Manuscript
Journal Name:
Bulletin of the Seismological Society of America
Additional Journal Information:
Journal Volume: 106; Journal Issue: 5; Journal ID: ISSN 0037-1106
Publisher:
Seismological Society of America
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES

Citation Formats

Graves, Robert, and Pitarka, Arben. Kinematic Ground-Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations. United States: N. p., 2016. Web. doi:10.1785/0120160088.
Graves, Robert, & Pitarka, Arben. Kinematic Ground-Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations. United States. https://doi.org/10.1785/0120160088
Graves, Robert, and Pitarka, Arben. Tue . "Kinematic Ground-Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations". United States. https://doi.org/10.1785/0120160088. https://www.osti.gov/servlets/purl/1420289.
@article{osti_1420289,
title = {Kinematic Ground-Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations},
author = {Graves, Robert and Pitarka, Arben},
abstractNote = {Here, we describe a methodology for generating kinematic earthquake ruptures for use in 3D ground–motion simulations over the 0–5 Hz frequency band. Our approach begins by specifying a spatially random slip distribution that has a roughly wavenumber–squared fall–off. Given a hypocenter, the rupture speed is specified to average about 75%–80% of the local shear wavespeed and the prescribed slip–rate function has a Kostrov–like shape with a fault–averaged rise time that scales self–similarly with the seismic moment. Both the rupture time and rise time include significant local perturbations across the fault surface specified by spatially random fields that are partially correlated with the underlying slip distribution. We represent velocity–strengthening fault zones in the shallow (<5 km) and deep (>15 km) crust by decreasing rupture speed and increasing rise time in these regions. Additional refinements to this approach include the incorporation of geometric perturbations to the fault surface, 3D stochastic correlated perturbations to the P– and S–wave velocity structure, and a damage zone surrounding the shallow fault surface characterized by a 30% reduction in seismic velocity. We demonstrate the approach using a suite of simulations for a hypothetical Mw 6.45 strike–slip earthquake embedded in a generalized hard–rock velocity structure. The simulation results are compared with the median predictions from the 2014 Next Generation Attenuation–West2 Project ground–motion prediction equations and show very good agreement over the frequency band 0.1–5 Hz for distances out to 25 km from the fault. Additionally, the newly added features act to reduce the coherency of the radiated higher frequency (f>1 Hz) ground motions, and homogenize radiation–pattern effects in this same bandwidth, which move the simulations closer to the statistical characteristics of observed motions as illustrated by comparison with recordings from the 1979 Imperial Valley earthquake.},
doi = {10.1785/0120160088},
journal = {Bulletin of the Seismological Society of America},
number = 5,
volume = 106,
place = {United States},
year = {Tue Aug 23 00:00:00 EDT 2016},
month = {Tue Aug 23 00:00:00 EDT 2016}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Citation Metrics:
Cited by: 104 works
Citation information provided by
Web of Science

Save / Share:

Works referencing / citing this record:

Broadband (0–4 Hz) Ground Motions for a Magnitude 7.0 Hayward Fault Earthquake With Three‐Dimensional Structure and Topography
journal, January 2018

  • Rodgers, Arthur J.; Pitarka, Arben; Petersson, N. Anders
  • Geophysical Research Letters, Vol. 45, Issue 2
  • DOI: 10.1002/2017gl076505

Accounting for Fault Roughness in Pseudo-Dynamic Ground-Motion Simulations
journal, April 2017

  • Mai, P. Martin; Galis, Martin; Thingbaijam, Kiran K. S.
  • Pure and Applied Geophysics, Vol. 174, Issue 9
  • DOI: 10.1007/s00024-017-1536-8

Kinematic Rupture Modeling of Ground Motion from the M7 Kumamoto, Japan Earthquake
journal, May 2019


Simulations for the development of a ground motion model for induced seismicity in the Groningen gas field, The Netherlands
journal, September 2018


Nonlinear Interaction of High‐Frequency Seismic Waves With Sliding Fault Planes
journal, November 2019

  • Sleep, Norman H.
  • Journal of Geophysical Research: Solid Earth, Vol. 124, Issue 11
  • DOI: 10.1029/2019jb017579

Nonlinear Suppression of High‐Frequency S Waves by the Near‐Field Velocity Pulse With Reference to the 2002 Denali Earthquake
journal, January 2020

  • Sleep, Norman H.; Liu, Tianze
  • Journal of Geophysical Research: Solid Earth, Vol. 125, Issue 1
  • DOI: 10.1029/2019jb018386

Empirical Models of Shear-Wave Radiation Pattern Derived from Large Datasets of Ground-Shaking Observations
journal, January 2019


High-frequency seismic wave propagation within the heterogeneous crust: effects of seismic scattering and intrinsic attenuation on ground motion modelling
journal, June 2017

  • Takemura, Shunsuke; Kobayashi, Manabu; Yoshimoto, Kazuo
  • Geophysical Journal International, Vol. 210, Issue 3
  • DOI: 10.1093/gji/ggx269

Mach wave properties in the presence of source and medium heterogeneity
journal, June 2018

  • Vyas, J. C.; Mai, P. M.; Galis, M.
  • Geophysical Journal International, Vol. 214, Issue 3
  • DOI: 10.1093/gji/ggy219

Hybrid broadband ground motion simulation validation of small magnitude earthquakes in Canterbury, New Zealand
journal, February 2020

  • Lee, Robin L.; Bradley, Brendon A.; Stafford, Peter J.
  • Earthquake Spectra, Vol. 36, Issue 2
  • DOI: 10.1177/8755293019891718

Effects of random 3D upper crustal heterogeneity on long-period (≥ 1 s) ground-motion simulations
journal, September 2018

  • Iwaki, Asako; Maeda, Takahiro; Morikawa, Nobuyuki
  • Earth, Planets and Space, Vol. 70, Issue 1
  • DOI: 10.1186/s40623-018-0930-5

Evaluation of SCEC CyberShake Ground Motions for Engineering Practice
journal, August 2019


Accounting for Fault Roughness in Pseudo-Dynamic Ground-Motion Simulations
book, December 2017


Quantification of Fault-Zone Plasticity Effects with Spontaneous Rupture Simulations
journal, February 2017


Empirical Models of Shear-Wave Radiation Pattern Derived from Large Datasets of Ground-Shaking Observations
journal, January 2019


Erratum: ‘Representation of complex seismic sources by orthogonal moment–tensor fields’
journal, June 2020

  • Jordan, Thomas H.; Juarez, Alan
  • Geophysical Journal International, Vol. 222, Issue 2
  • DOI: 10.1093/gji/ggaa164

Simulation Database of Broadband Ground-Motion Time Histories for the Rhine Graben Area
dataset, January 2022