Bio
My research focuses on the development and use of physics-based computational simulations to characterize and understand earthquakes, tsunamis, and volcanoes, and similar phenomena. My approach is to identify the fundamental mechanical processes governing a system of interest, develop numerical models incorporating these processes, validate them using geophysical observations, and then use the models to predict system behavior. Specific research areas include earthquake rupture dynamics and earthquake source processes, tsunami generation, volcano seismology and infrasound, ice stream stick-slip events and flexural-gravity waves in ice shelves, and numerical methods for wave propagation.
Administrative Appointments
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Reginald A. Daly Postdoctoral Fellow, Department of Earth and Planetary Sciences, Harvard University (2005 - 2007)
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Research Associate in Geophysics, Department of Earth and Planetary Sciences, Harvard University (2007 - 2009)
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Lecturer on Applied Mathematics, School of Engineering and Applied Sciences, Harvard University (2008 - 2009)
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Assistant Professor, Department of Geophysics, Stanford University (2009 - Present)
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Affiliated Faculty Member, Institute for Computational and Mathematical Engineering, Stanford University (2011 - Present)
Honors & Awards
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Jefferson Scholar, University of Virginia (1996-2000)
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Member, Phi Beta Kappa (1999)
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B.S. Physics with Highest Distinction, University of Virginia (2000)
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Parsons Fellow in computational science, University of California, Santa Barbara, Physics (2000)
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James W. Elkins Award, University of Virginia Physics (2000)
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John Cardy Award, UCSB Physics (2001)
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Graduate Fellow, National Defense Science and Engineering (2001-2005)
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Outstanding Student Paper, American Geophysical Union (2002)
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UCSB Affiliates Graduate Dissertation Fellowship, University of California, Santa Barbara (2004)
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Outstanding Student Paper, American Geophysical Union (2004)
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Student Presentation Award, Seismological Society of America (2004)
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Editors' Citation for Excellence in Refereeing, Geophysical Research Letters (2007)
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Certificate of Distinction in Teaching, Harvard University (2008)
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Terman Fellow, Stanford University (2009-2012)
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Best Poster Award, Society of Industrial and Applied Mathematics (SIAM) Geosciences (2011)
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Fellow, Physics, Alfred P. Sloan Foundation (2012)
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NSF CAREER award on Subduction Zone Hazards: Megathrust Rupture Dynamics and Tsunamis, National Science Foundation (2013-2017)
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School of Earth Sciences Excellence in Teaching Award, Stanford University (2014)
Boards, Advisory Committees, Professional Organizations
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Invited speaker, Stanford Club of Marin (2015 - 2015)
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Invited speaker for Stanford Admit Weekend, Academic Expo, Stanford University (2015 - 2015)
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Faculty search committee, member, Department of Geophysics, Stanford University (2014 - 2015)
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External Program review panel member, USGS-NEHRP (National Earthquake Hazards Reduction Program) (2014 - 2014)
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Invited speaker, Stanford Alumni Club of the Desert (2014 - 2014)
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Invited speaker, Southern California Earthquake Center (SCEC) Annual Meeting (2014 - 2014)
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Invited speaker, Incorporated Research Institutions for Seismology, Grand Challenges in Faulting and Deformation Processes (2014 - 2014)
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Invited speaker, American Geophysical Union Fall Meeting (two invited talks) (2014 - 2014)
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Invited speaker, Computational Infrastructure for Geodynamics Crustal Deformation Modeling Workshop (2014 - 2014)
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Invited speaker, Penn State (2014 - 2014)
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Invited speaker, Caltech (2014 - 2014)
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Invited speaker for Stanford Admit Weekend, Academic Expo, Stanford University (2014 - 2014)
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Invited speaker, Annual meeting, Seismological Society of America (2014 - 2014)
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Invited speaker, Rock and Fluid Physics: Academic and Industrial Perspectives Conference, Shell Technology Centre, Amsterdam (2014 - 2014)
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Geophysics Admissions Committee, Stanford University (2013 - 2014)
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School of Earth Sciences Teaching Task Force, Stanford University (2013 - 2014)
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Co-organizer for annual meeting special session on Earthquake Source Physics, Seismological Society of America (2013 - 2013)
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External Program review panel member, USGS-NEHRP (National Earthquake Hazards Reduction Program) (2013 - 2013)
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Invited speaker, King Abdullah University of Science and Technology (2013 - 2013)
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Invited speaker, University of British Columbia (2013 - 2013)
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Invited speaker, Lockheed Martin Advanced Technology Center (2013 - 2013)
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Invited speaker at New Student Orientation, Engaging with Faculty, Stanford University (2013 - 2013)
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Invited speaker for Stanford Admit Weekend, Academic Expo, Stanford University (2013 - 2013)
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Advisory Board, Computational Geosciences MS Program, Institute for Computational and Mathematical Engineering, Stanford Univeristy (2012 - Present)
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Co-leader of Computational Science disciplinary group, member of Planning Committee, Southern California Earthquake Center (SCEC) (2012 - Present)
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Chair, 5th Chinese-American Kavli Frontiers of Science Symposium, Earthquake Mechanics and Forecasting, National Academy of Sciences, (2012 - 2012)
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Co-organizer for annual meeting special session on Seismicity in Volcanic Environments, Seismological Society of America (2012 - 2012)
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Invited speaker at New Student Orientation, Engaging with Faculty, Stanford University (2012 - 2012)
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Invited speaker, Fall Meeting, American Geophysical Union (2012 - 2012)
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Invited speaker, New Perspective on Great Earthquakes Along Subduction Zones, International Conference (2012 - 2012)
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Stanford School of Earth Sciences Council, Stanford University (2011 - Present)
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Geophysics Department Seminar Series Organizer, Stanford University (2011 - 2012)
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Co-organizer for Geosciences Minisymposium on Computational Challenges in Earthquake Simulation, Society for Industrial and Applied Mathematics (SIAM) (2011 - 2011)
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Invited speaker, University of California, Santa Cruz (2011 - 2011)
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Invited speaker at New Student Orientation, Engaging with Faculty, Stanford University (2011 - 2011)
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Invited speaker, Fall Meeting, American Geophysical Union (2011 - 2011)
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Undergraduate Premajor Advisor, Stanford University (2010 - Present)
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Co-convener for International Workshop on Multiscale and Multiphysics Processes in Geomechanics, Stanford University (2010 - 2010)
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Delegate, Panel on Earthquake Research, U.S.-Japan Natural Resources (UJNR) (2010 - 2010)
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External Program review panel member, USGS-NEHRP (National Earthquake Hazards Reduction Program) (2010 - 2010)
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Invited speaker, Lawrence Livermore National Laboratory (2010 - 2010)
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Invited speaker, University of California, Berkeley, Seismological Laboratory (2010 - 2010)
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Invited speaker, University of Oregon (2010 - 2010)
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Invited speaker, Lockheed Martin Advanced Technology Center (2010 - 2010)
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Invited speaker, University of California, Berkeley, Applied Mathematics (2010 - 2010)
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Geophysics Undergraduate Curriculum Committee, Stanford University (2009 - 2010)
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Co-convener, Workshop on Dynamic Weakening Mechanisms, Southern California Earthquake Center (2009 - 2009)
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Co-organizer for earthquake rupture code validation project, Southern California Earthquake Center (2007 - 2011)
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Associate Editor, Journal of Geophysical Research-Solid Earth (2005 - 2008)
Professional Education
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Ph.D., University of California, Santa Barbara, Physics (2005)
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B.S., University of Virginia, Physics (2000)
Current Research and Scholarly Interests
Research
My research focuses on the development and use of physics-based computational simulations to characterize and understand earthquakes, tsunamis, and volcanoes, and similar phenomena. My approach is to identify the fundamental mechanical processes governing a system of interest, develop numerical models incorporating these processes, validate them using geophysical observations, and then use the models to predict system behavior. Specific research areas include earthquake rupture dynamics and earthquake source processes, tsunami generation, volcano seismology and infrasound, ice stream stick-slip events and flexural-gravity waves in ice shelves, and numerical methods for wave propagation.
Teaching
I teach courses on mechanics and modeling (GEOPHYS 120/220: Geophysical Mechanics and Dynamics), numerical methods (CME 108/MATH 114: Introduction to Scientific Computing), wave generation and propagation (GEOPHYS 238: Waves in Solids and Fluids), and earthquakes (GEOPHYS 229: Earthquake Rupture Dynamics).
Professional Awards
NSF CAREER award, 2013; Alfred P. Sloan Fellow in Physics, 2012
Projects
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Collaborative Development of Numerical Methods for Wave Propagation, Stanford University and Uppsala University
My group has partnered with Professor Ken Mattsson at Uppsala University, Sweden, to develop numerical methods for wave propagation problems. We simulate flexural-gravity waves in floating ice shelves offshore Antarctica, seismic waves and tsunamis from earthquakes, and acoustic waves from volcanic eruptions and explosions.
Location
Uppsala, Sweden
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Villarica Volcano
We use infrasound waves to help forecast eruptions at Villarica Volcano, Chile.
Location
Villarica, Chile
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Antarctic Ice Shelves
We study how ocean waves flex and bend ice shelves, potentially contributing to rifting, fracture growth, and ice shelf disintegration.
Location
Antarctica
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Kilauea Volcano
We use seismic data to image the shallow "plumbing system" of Kilauea Volcano, Hawaii.
Location
Kilauea Volcano, Hawaii
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2011 Tohoku Earthquake and Tsunami
We perform computer simulations of the magnitude 9 Tohoku earthquake and tsunami.
Location
Sendai, Japan
2024-25 Courses
- Earthquake Rupture Dynamics
GEOPHYS 229 (Aut) - Physical Volcanology
GEOPHYS 385R (Aut, Win, Spr) - Theoretical Geophysics
GEOPHYS 385D (Aut, Win, Spr) -
Independent Studies (5)
- Honors Program
GEOPHYS 198 (Aut, Sum) - Master's Research
CME 291 (Aut, Win, Spr, Sum) - Report on Energy Industry Training
GEOPHYS 255 (Aut) - Research in Geophysics
GEOPHYS 400 (Aut, Win, Spr, Sum) - Undergraduate Research in Geophysics
GEOPHYS 196 (Aut, Win, Spr, Sum)
- Honors Program
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Prior Year Courses
2023-24 Courses
- Geophysical Mechanics and Dynamics
GEOPHYS 120, GEOPHYS 220 (Win) - Physical Volcanology
GEOPHYS 385R (Aut, Win, Spr) - Theoretical Geophysics
GEOPHYS 385D (Aut, Win, Spr)
2022-23 Courses
- Geophysical Mechanics and Dynamics
GEOPHYS 120, GEOPHYS 220 (Aut) - Introduction to Scientific Computing
CME 108 (Win) - Physical Volcanology
GEOPHYS 385R (Aut, Win, Spr) - Theoretical Geophysics
GEOPHYS 385D (Aut, Win, Spr, Sum) - Waves in Solids and Fluids
GEOPHYS 238 (Spr)
2021-22 Courses
- Earthquake Rupture Dynamics
GEOPHYS 229 (Aut) - Earthquake Seismology, Deformation, and Stress
GEOPHYS 385L (Aut) - Introduction to Scientific Computing
CME 108, MATH 114 (Win) - Physical Volcanology
GEOPHYS 385R (Sum) - Theoretical Geophysics
GEOPHYS 385D (Aut, Win, Spr, Sum)
- Geophysical Mechanics and Dynamics
Stanford Advisees
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Doctoral Dissertation Reader (AC)
Laura Blackstone, Emma Weijia Liu, Axel Wang -
Postdoctoral Faculty Sponsor
Vidar Stiernstroem, Wenqiang Zhang -
Doctoral Dissertation Advisor (AC)
Qing Ji, Mario Ruiz -
Doctoral (Program)
Natalia Berrios-Rivera, Rikuto Fukushima
All Publications
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Adjoint-based inversion for stress and frictional parameters in earthquake modeling
JOURNAL OF COMPUTATIONAL PHYSICS
2024; 519
View details for DOI 10.1016/j.jcp.2024.113447
View details for Web of Science ID 001325182900001
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Fault-Valve Instability: A Mechanism for Slow Slip Events
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2024; 129 (10)
View details for DOI 10.1029/2024JB029165
View details for Web of Science ID 001334639200001
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Fluid-driven aseismic fault slip with permeability enhancement and dilatancy.
Philosophical transactions. Series A, Mathematical, physical, and engineering sciences
2024; 382 (2276): 20230255
Abstract
Injection-induced seismicity and aseismic slip often involve the reactivation of long-dormant faults, which may have extremely low permeability prior to slip. In contrast, most previous models of fluid-driven aseismic slip have assumed linear pressure diffusion in a fault zone of constant permeability and porosity. Slip occurs within a frictional shear crack whose edge can either lag or lead pressure diffusion, depending on the dimensionless stress-injection parameter that quantifies the prestress and injection conditions. Here, we extend this foundational work by accounting for permeability enhancement and dilatancy, assumed to occur instantaneously upon the onset of slip. The fault zone ahead of the crack is assumed to be impermeable, so fluid flow and pressure diffusion are confined to the interior, slipped part of the crack. The confinement of flow increases the pressurization rate and reduction of fault strength, facilitating crack growth even for severely understressed faults. Suctions from dilatancy slow crack growth, preventing propagation beyond the hydraulic diffusion length. Our new two-dimensional and three-dimensional solutions can facilitate the interpretation of induced seismicity data sets. They are especially relevant for faults in initially low permeability formations, such as shale layers serving as caprock seals for geologic carbon storage, or for hydraulic stimulation of geothermal reservoirs.This article is part of the theme issue 'Induced seismicity in coupled subsurface systems'.
View details for DOI 10.1098/rsta.2023.0255
View details for PubMedID 38945161
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Dynamic Rupture Simulations of Caldera Collapse Earthquakes: Effects of Wave Radiation, Magma Viscosity, and Evidence of Complex Nucleation at Kilauea 2018
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2024; 129 (4)
View details for DOI 10.1029/2023JB028280
View details for Web of Science ID 001196097500001
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Ambient noise from the atmosphere within the seismic hum period band: A case study of hurricane landfall
Earth and Planetary Science Letters
2024; 629: 118589
View details for DOI 10.1016/j.epsl.2024.118589
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Simulation of flexural-gravity wave propagation for elastic plates in shallow water using an energy-stable finite difference method with weakly enforced boundary and interface conditions
JOURNAL OF COMPUTATIONAL PHYSICS
2023; 493
View details for DOI 10.1016/j.jcp.2023.112470
View details for Web of Science ID 001080957800001
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Quantifying the probability of rupture arrest at restraining and releasing bends using earthquake sequence simulations
EARTH AND PLANETARY SCIENCE LETTERS
2023; 617
View details for DOI 10.1016/j.epsl.2023.118276
View details for Web of Science ID 001038333600001
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Modeling and inversion in acoustic-elastic coupled media using energy-stable summation-by-parts operators
GEOPHYSICS
2023; 88 (3): T137-T150
View details for DOI 10.1190/GEO2022-0195.1
View details for Web of Science ID 001020940000002
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Influence of port opening dynamics on the acoustic signature of pneumatic marine seismic sources
GEOPHYSICS
2023; 88 (3): P15-P36
View details for DOI 10.1190/GEO2022-0346.1
View details for Web of Science ID 001015139800002
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Influence of Creep Compaction and Dilatancy on Earthquake Sequences and Slow Slip
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2023; 128 (4)
View details for DOI 10.1029/2022JB025969
View details for Web of Science ID 001000304700001
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Incorporating Full Elastodynamic Effects and Dipping Fault Geometries in Community Code Verification Exercises for Simulations of Earthquake Sequences and Aseismic Slip (SEAS)
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2023; 113 (2): 499-523
View details for DOI 10.1785/0120220066
View details for Web of Science ID 000968430000001
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Comparison of methods for coupled earthquake and tsunami modelling
GEOPHYSICAL JOURNAL INTERNATIONAL
2023; 234 (1): 404-426
View details for DOI 10.1093/gji/ggad053
View details for Web of Science ID 000945861500004
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Hindcasting injection-induced aseismic slip and microseismicity at the Cooper Basin Enhanced Geothermal Systems Project.
Scientific reports
2022; 12 (1): 19481
Abstract
There is a growing recognition that subsurface fluid injection can produce not only earthquakes, but also aseismic slip on faults. A major challenge in understanding interactions between injection-related aseismic and seismic slip on faults is identifying aseismic slip on the field scale, given that most monitored fields are only equipped with seismic arrays. We present a modeling workflow for evaluating the possibility of aseismic slip, given observational constraints on the spatial-temporal distribution of microseismicity, injection rate, and wellhead pressure. Our numerical model simultaneously simulates discrete off-fault microseismic events and aseismic slip on a main fault during fluid injection. We apply the workflow to the 2012 Enhanced Geothermal System injection episode at Cooper Basin, Australia, which aimed to stimulate a water-saturated granitic reservoir containing a highly permeable ([Formula: see text] [Formula: see text]) fault zone. We find that aseismic slip likely contributed to half of the total moment release. In addition, fault weakening from pore pressure changes, not elastic stress transfer from aseismic slip, induces the majority of observed microseismic events, given the inferred stress state. We derive a theoretical model to better estimate the time-dependent spatial extent of seismicity triggered by increases in pore pressure. To our knowledge, this is the first time injection-induced aseismic slip in a granitic reservoir has been inferred, suggesting that aseismic slip could be widespread across a range of lithologies.
View details for DOI 10.1038/s41598-022-23812-7
View details for PubMedID 36376409
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Models of Injection-Induced Aseismic Slip on Height-Bounded Faults in the Delaware Basin Constrain Fault-Zone Pore Pressure Changes and Permeability
GEOPHYSICAL RESEARCH LETTERS
2022; 49 (11)
View details for DOI 10.1029/2021GL097330
View details for Web of Science ID 000812038600001
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Ultra and Very Long Period Seismic Signatures of Unsteady Eruptions Predicted From Conduit Flow Models
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2022; 127 (6)
View details for DOI 10.1029/2022JB024313
View details for Web of Science ID 000813539100001
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Physics-Based Model Reconciles Caldera Collapse Induced Static and Dynamic Ground Motion: Application to Kilauea 2018
GEOPHYSICAL RESEARCH LETTERS
2022; 49 (8)
View details for DOI 10.1029/2021GL097440
View details for Web of Science ID 000781874000001
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Community-Driven Code Comparisons for Three-Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2022; 127 (3)
View details for DOI 10.1029/2021JB023519
View details for Web of Science ID 000776510500043
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Infrasound Radiation From Impulsive Volcanic Eruptions: Nonlinear Aeroacoustic 2D Simulations
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2021; 126 (9)
View details for DOI 10.1029/2021JB021940
View details for Web of Science ID 000703087900066
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Effect of Porosity and Permeability Evolution on Injection-Induced Aseismic Slip
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2021; 126 (7)
View details for DOI 10.1029/2020JB021258
View details for Web of Science ID 000678880700046
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Influence of Shear Heating and Thermomechanical Coupling on Earthquake Sequences and the Brittle-Ductile Transition
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2021; 126 (6)
View details for DOI 10.1029/2020JB021394
View details for Web of Science ID 000665206200037
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Elastic wave propagation in anisotropic solids using energy-stable finite differences with weakly enforced boundary and interface conditions
JOURNAL OF COMPUTATIONAL PHYSICS
2021; 424
View details for DOI 10.1016/j.jcp.2020.109842
View details for Web of Science ID 000588203600022
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Earthquake Sequence Dynamics at the Interface Between an Elastic Layer and Underlying Half-Space in Antiplane Shear
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2020; 125 (12)
View details for DOI 10.1029/2020JB020007
View details for Web of Science ID 000603664600044
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Fault valving and pore pressure evolution in simulations of earthquake sequences and aseismic slip.
Nature communications
2020; 11 (1): 4833
Abstract
Fault-zone fluids control effective normal stress and fault strength. While most earthquake models assume a fixed pore fluid pressure distribution, geologists have documented fault valving behavior, that is, cyclic changes in pressure and unsteady fluid migration along faults. Here we quantify fault valving through 2-D antiplane shear simulations of earthquake sequences on a strike-slip fault with rate-and-state friction, upward Darcy flow along a permeable fault zone, and permeability evolution. Fluid overpressure develops during the interseismic period, when healing/sealing reduces fault permeability, and is released after earthquakes enhance permeability. Coupling between fluid flow, permeability and pressure evolution, and slip produces fluid-driven aseismic slip near the base of the seismogenic zone and earthquake swarms within the seismogenic zone, as ascending fluids pressurize and weaken the fault. This model might explain observations of late interseismic fault unlocking, slow slip and creep transients, swarm seismicity, and rapid pressure/stress transmission in induced seismicity sequences.
View details for DOI 10.1038/s41467-020-18598-z
View details for PubMedID 32973184
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Role of Fluid Injection on Earthquake Size in Dynamic Rupture Simulations on Rough Faults
GEOPHYSICAL RESEARCH LETTERS
2020; 47 (13)
View details for DOI 10.1029/2020GL088377
View details for Web of Science ID 000551465400057
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Non-stiff boundary and interface penalties for narrow-stencil finite difference approximations of the Laplacian on curvilinear multiblock grids
JOURNAL OF COMPUTATIONAL PHYSICS
2020; 408
View details for DOI 10.1016/j.jcp.2020.109294
View details for Web of Science ID 000521731200027
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Lava lake sloshing modes during the 2018 Kilauea Volcano eruption probe magma reservoir storativity
EARTH AND PLANETARY SCIENCE LETTERS
2020; 536
View details for DOI 10.1016/j.epsl.2020.116110
View details for Web of Science ID 000521110800006
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The Community Code Verification Exercise for Simulating Sequences of Earthquakes and Aseismic Slip (SEAS)
SEISMOLOGICAL RESEARCH LETTERS
2020; 91 (2): 874–90
View details for DOI 10.1785/0220190248
View details for Web of Science ID 000518383600030
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Influence of fault roughness on surface displacement: from numerical simulations to coseismic slip distributions
GEOPHYSICAL JOURNAL INTERNATIONAL
2020; 220 (3): 1857–77
View details for DOI 10.1093/gji/ggz545
View details for Web of Science ID 000525944600029
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The State of Stress on the Fault Before, During, and After a Major Earthquake
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 48, 2020
2020; 48: 49–74
View details for DOI 10.1146/annurev-earth-053018-060507
View details for Web of Science ID 000613951000004
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Magma Oscillations in a Conduit-Reservoir System, Application to Very Long Period (VLP) Seismicity at Basaltic Volcanoes: 2. Data Inversion and Interpretation at Klauea Volcano
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2020; 125 (1)
View details for DOI 10.1029/2019JB017456
View details for Web of Science ID 000530895100005
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Magma Oscillations in a Conduit-Reservoir System, Application to Very Long Period (VLP) Seismicity at Basaltic Volcanoes: 1. Theory
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2020; 125 (1)
View details for DOI 10.1029/2019JB017437
View details for Web of Science ID 000530895100006
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Dynamic rupture and earthquake sequence simulations using the wave equation in second-order form
GEOPHYSICAL JOURNAL INTERNATIONAL
2019; 219 (2): 796–815
View details for DOI 10.1093/gji/ggz319
View details for Web of Science ID 000491050200005
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Fully Coupled Simulations of Megathrust Earthquakes and Tsunamis in the Japan Trench, Nankai Trough, and Cascadia Subduction Zone
PURE AND APPLIED GEOPHYSICS
2019; 176 (9): 4009–41
View details for DOI 10.1007/s00024-018-1990-y
View details for Web of Science ID 000484943000011
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Poroelastic effects destabilize mildly rate-strengthening friction to generate stable slow slip pulses
JOURNAL OF THE MECHANICS AND PHYSICS OF SOLIDS
2019; 130: 262–79
View details for DOI 10.1016/j.jmps.2019.06.007
View details for Web of Science ID 000483422100014
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Simulation and inversion of harmonic infrasound from open-vent volcanoes using an efficient quasi-1D crater model
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
2019; 380: 64–79
View details for DOI 10.1016/j.jvolgeores.2019.05.007
View details for Web of Science ID 000474329500005
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Combining Dynamic Rupture Simulations with Ground-Motion Data to Characterize Seismic Hazard from M-w 3 to 5.8 Earthquakes in Oklahoma and Kansas
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2019; 109 (2): 652–71
View details for DOI 10.1785/0120180042
View details for Web of Science ID 000462138500012
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What controls the initial peak of an air-gun source signature?
GEOPHYSICS
2019; 84 (2): P27–P45
View details for DOI 10.1190/GEO2018-0298.1
View details for Web of Science ID 000462613600048
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Tsunami Wavefield Reconstruction and Forecasting Using the Ensemble Kalman Filter
GEOPHYSICAL RESEARCH LETTERS
2019; 46 (2): 853–60
View details for DOI 10.1029/2018GL080644
View details for Web of Science ID 000458607400036
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Simulation of acoustic and flexural-gravity waves in ice-covered oceans
JOURNAL OF COMPUTATIONAL PHYSICS
2018; 373: 230–52
View details for DOI 10.1016/j.jcp.2018.06.060
View details for Web of Science ID 000445108800010
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A finite difference method for earthquake sequences in poroelastic solids
COMPUTATIONAL GEOSCIENCES
2018; 22 (5): 1351–70
View details for DOI 10.1007/s10596-018-9757-1
View details for Web of Science ID 000444706400012
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Mach wave properties in the presence of source and medium heterogeneity
GEOPHYSICAL JOURNAL INTERNATIONAL
2018; 214 (3): 2035–52
View details for DOI 10.1093/gji/ggy219
View details for Web of Science ID 000439648000033
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Earthquake cycle simulations with rate-and-state friction and power-law viscoelasticity
TECTONOPHYSICS
2018; 733: 232–56
View details for DOI 10.1016/j.tecto.2017.10.021
View details for Web of Science ID 000432640200017
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A Suite of Exercises for Verifying Dynamic Earthquake Rupture Codes
SEISMOLOGICAL RESEARCH LETTERS
2018; 89 (3): 1146–62
View details for DOI 10.1785/0220170222
View details for Web of Science ID 000440583400021
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Forecasting the Eruption of an Open-Vent Volcano Using Resonant Infrasound Tones
GEOPHYSICAL RESEARCH LETTERS
2018; 45 (5): 2213–20
View details for DOI 10.1002/2017GL076506
View details for Web of Science ID 000428402400011
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Accounting for Fault Roughness in Pseudo-Dynamic Ground-Motion Simulations
PURE AND APPLIED GEOPHYSICS
2017; 174 (9): 3419–50
View details for DOI 10.1007/s00024-017-1536-8
View details for Web of Science ID 000411873600007
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Treatment of the polar coordinate singularity in axisymmetric wave propagation using high-order summation-by-parts operators on a staggered grid
COMPUTERS & FLUIDS
2017; 149: 138-149
View details for DOI 10.1016/j.compfluid.2017.03.015
View details for Web of Science ID 000400038700010
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Slow-slip events on the Whillans Ice Plain, Antarctica, described using rate-and-state friction as an ice stream sliding law
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
2017; 122 (4): 973-1003
View details for DOI 10.1002/2016JF004183
View details for Web of Science ID 000401157700011
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The effect of compliant prisms on subduction zone earthquakes and tsunamis
EARTH AND PLANETARY SCIENCE LETTERS
2017; 458: 213-222
View details for DOI 10.1016/j.epsl.2016.10.050
View details for Web of Science ID 000392685100020
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Excitation and resonance of acoustic-gravity waves in a column of stratified, bubbly magma
JOURNAL OF FLUID MECHANICS
2016; 797: 431-470
View details for DOI 10.1017/jfm.2016.257
View details for Web of Science ID 000376600800020
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Dynamic earthquake rupture simulations on nonplanar faults embedded in 3D geometrically complex, heterogeneous elastic solids
JOURNAL OF COMPUTATIONAL PHYSICS
2016; 305: 185-207
View details for DOI 10.1016/j.jcp.2015.10.021
View details for Web of Science ID 000366156600010
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Rupture complexity and the supershear transition on rough faults
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2016; 121 (1): 210-224
View details for DOI 10.1002/2015JB012512
View details for Web of Science ID 000373073200013
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Tremor during ice-stream stick slip
CRYOSPHERE
2016; 10 (1): 385-399
View details for DOI 10.5194/tc-10-385-2016
View details for Web of Science ID 000377602600025
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Nucleation and dynamic rupture on weakly stressed faults sustained by thermal pressurization
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2015; 120 (11): 7606-7640
View details for DOI 10.1002/2015JB012322
View details for Web of Science ID 000368437800020
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High-order finite difference modeling of tsunami generation in a compressible ocean from offshore earthquakes
COMPUTATIONAL GEOSCIENCES
2015; 19 (2): 327-340
View details for DOI 10.1007/s10596-015-9472-0
View details for Web of Science ID 000355335100005
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Rupture dynamics and ground motions from earthquakes in 2-D heterogeneous media
GEOPHYSICAL RESEARCH LETTERS
2015; 42 (6): 1701-1709
View details for DOI 10.1002/2014GL062982
View details for Web of Science ID 000353170000012
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Vibrationalmodes of hydraulic fractures: Inference of fracture geometry fromresonant frequencies and attenuation
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2015; 120 (2): 1080-1107
View details for DOI 10.1002/2014JB011286
View details for Web of Science ID 000351466000026
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Simulation of Earthquake Rupture Dynamics in Complex Geometries Using Coupled Finite Difference and Finite Volume Methods
COMMUNICATIONS IN COMPUTATIONAL PHYSICS
2015; 17 (2): 337-370
View details for DOI 10.4208/cicp.111013.120914a
View details for Web of Science ID 000353693400002
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Constraining shallow slip and tsunami excitation in megathrust ruptures using seismic and ocean acoustic waves recorded on ocean-bottom sensor networks
EARTH AND PLANETARY SCIENCE LETTERS
2014; 396: 56-65
View details for DOI 10.1016/j.epsl.2014.04.001
View details for Web of Science ID 000336819900006
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An efficient numerical method for earthquake cycles in heterogeneous media: Alternating subbasin and surface-rupturing events on faults crossing a sedimentary basin
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2014; 119 (4): 3290-3316
View details for DOI 10.1002/2013JB010614
View details for Web of Science ID 000337688600038
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A 2D Pseudodynamic Rupture Model Generator for Earthquakes on Geometrically Complex Faults
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2014; 104 (1): 95-112
View details for DOI 10.1785/0120130138
View details for Web of Science ID 000330579800006
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Predicting fault damage zones by modeling dynamic rupture propagation and comparison with field observations
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2014; 119 (2): 1251-1272
View details for DOI 10.1002/2013JB010335
View details for Web of Science ID 000333034600027
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Strong Ground Motion Prediction Using Virtual Earthquakes
SCIENCE
2014; 343 (6169): 399-403
Abstract
Sedimentary basins increase the damaging effects of earthquakes by trapping and amplifying seismic waves. Simulations of seismic wave propagation in sedimentary basins capture this effect; however, there exists no method to validate these results for earthquakes that have not yet occurred. We present a new approach for ground motion prediction that uses the ambient seismic field. We apply our method to a suite of magnitude 7 scenario earthquakes on the southern San Andreas fault and compare our ground motion predictions with simulations. Both methods find strong amplification and coupling of source and structure effects, but they predict substantially different shaking patterns across the Los Angeles Basin. The virtual earthquake approach provides a new approach for predicting long-period strong ground motion.
View details for DOI 10.1126/science.1245678
View details for Web of Science ID 000330039300043
View details for PubMedID 24458636
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Frictional-faulting model for harmonic tremor before Redoubt Volcano eruptions
NATURE GEOSCIENCE
2013; 6 (8): 652-656
View details for DOI 10.1038/NGEO1879
View details for Web of Science ID 000322441900018
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Additional shear resistance from fault roughness and stress levels on geometrically complex faults
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2013; 118 (7): 3642-3654
View details for DOI 10.1002/jgrb.50262
View details for Web of Science ID 000324952300025
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Rupture to the Trench: Dynamic Rupture Simulations of the 11 March 2011 Tohoku Earthquake
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2013; 103 (2B): 1275-1289
View details for DOI 10.1785/0120120136
View details for Web of Science ID 000318277200008
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Ground motion prediction of realistic earthquake sources using the ambient seismic field
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2013; 118 (5): 2102-2118
View details for DOI 10.1029/2012JB009603
View details for Web of Science ID 000327299800053
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Simulation of Dynamic Earthquake Ruptures in Complex Geometries Using High-Order Finite Difference Methods
JOURNAL OF SCIENTIFIC COMPUTING
2013; 55 (1): 92-124
View details for DOI 10.1007/s10915-012-9624-5
View details for Web of Science ID 000316148400005
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Solving the Surface-Wave Eigenproblem with Chebyshev Spectral Collocation
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2012; 102 (3): 1214-1223
View details for DOI 10.1785/0120110183
View details for Web of Science ID 000304870500021
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Special Issue Honoring Professor James R. Rice
JOURNAL OF APPLIED MECHANICS-TRANSACTIONS OF THE ASME
2012; 79 (3)
View details for DOI 10.1115/1.4005965
View details for Web of Science ID 000303261700001
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Guided Waves Along Fluid-Filled Cracks in Elastic Solids and Instability at High Flow Rates
JOURNAL OF APPLIED MECHANICS-TRANSACTIONS OF THE ASME
2012; 79 (3)
View details for DOI 10.1115/1.4005961
View details for Web of Science ID 000303261700021
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Observation of far-field Mach waves generated by the 2001 Kokoxili supershear earthquake
GEOPHYSICAL RESEARCH LETTERS
2012; 39
View details for DOI 10.1029/2011GL050725
View details for Web of Science ID 000301667500001
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Interaction of Waves with Frictional Interfaces Using Summation-by-Parts Difference Operators: Weak Enforcement of Nonlinear Boundary Conditions
JOURNAL OF SCIENTIFIC COMPUTING
2012; 50 (2): 341-367
View details for DOI 10.1007/s10915-011-9485-3
View details for Web of Science ID 000299001800005
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Earthquake Ruptures with Strongly Rate-Weakening Friction and Off-Fault Plasticity, Part 2: Nonplanar Faults
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2011; 101 (5): 2308-2322
View details for DOI 10.1785/0120100076
View details for Web of Science ID 000295214100024
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Earthquake Ruptures with Strongly Rate-Weakening Friction and Off-Fault Plasticity, Part 1: Planar Faults
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2011; 101 (5): 2296-2307
View details for DOI 10.1785/0120100075
View details for Web of Science ID 000295214100023
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Verifying a Computational Method for Predicting Extreme Ground Motion
SEISMOLOGICAL RESEARCH LETTERS
2011; 82 (5): 638-644
View details for DOI 10.1785/gssrl.82.5.638
View details for Web of Science ID 000294523000004
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EARTHQUAKE RUPTURES ON ROUGH FAULTS
International Workshop on Multiscale and Multiphysics Processes in Geomechanics
SPRINGER-VERLAG BERLIN. 2011: 145–148
View details for Web of Science ID 000329001600037
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Coherence of Mach fronts during heterogeneous supershear earthquake rupture propagation: Simulations and comparison with observations
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2010; 115
View details for DOI 10.1029/2009JB006819
View details for Web of Science ID 000280720800004
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Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2009; 114
View details for DOI 10.1029/2008JB006143
View details for Web of Science ID 000267937100001
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The SCEC/USGS Dynamic Earthquake Rupture Code Verification Exercise
SEISMOLOGICAL RESEARCH LETTERS
2009; 80 (1): 119-126
View details for DOI 10.1785/gssrl.80.1.119
View details for Web of Science ID 000262378800016
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Earthquake slip between dissimilar poroelastic materials
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2008; 113 (B9)
View details for DOI 10.1029/2007JB005405
View details for Web of Science ID 000259203000002
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Attenuation of radiated ground motion and stresses from three-dimensional supershear ruptures
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2008; 113 (B8)
View details for DOI 10.1029/2007JB005182
View details for Web of Science ID 000258824500002
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Conditions governing the occurrence of supershear ruptures under slip-weakening friction
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2007; 112 (B7)
View details for DOI 10.1029/2006JB004717
View details for Web of Science ID 000247882600004
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Distinguishing barriers and asperities in near-source ground motion
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2005; 110 (B11)
View details for DOI 10.1029/2005JB003736
View details for Web of Science ID 000233163200004
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Near-source ground motion from steady state dynamic rupture pulses
GEOPHYSICAL RESEARCH LETTERS
2005; 32 (3)
View details for DOI 10.1029/2004GL021793
View details for Web of Science ID 000226900900006
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Dissipative interface waves and the transient response of a three-dimensional sliding interface with Coulomb friction
JOURNAL OF THE MECHANICS AND PHYSICS OF SOLIDS
2005; 53 (2): 327-357
View details for DOI 10.1016/j.jmps.2004.07.003
View details for Web of Science ID 000226555700004
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Evidence for a supershear transient during the 2002 Denali fault earthquake
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
2004; 94 (6): S256-S268
View details for Web of Science ID 000227331100017
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A supershear transition mechanism for cracks
SCIENCE
2003; 299 (5612): 1557-1559
Abstract
Seismic data indicate that fault ruptures follow complicated paths with variable velocity because of inhomogeneities in initial stress or fracture energy. We report a phenomenon unique to three-dimensional cracks: Locally stronger fault sections, rather than slowing ruptures, drive them forward at velocities exceeding the shear wave speed. This supershear mechanism differentiates barrier and asperity models of fault heterogeneity, which previously have been regarded as indistinguishable. High strength barriers concentrate energy, producing potentially destructive pulses of strong ground motion.
View details for Web of Science ID 000181367900032
View details for PubMedID 12624262