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Recognizing Foreshocks from the 1 April 2014 Chile Earthquake

Science (American Association for the Advancement of Science), 2014-05, Vol.344 (6185), p.700-702

2014

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Coseismic Rupture Process of the Large 2019 Ridgecrest Earthquakes From Joint Inversion of Geodetic and Seismological Observations

Geophysical research letters, 2019-11, Vol.46 (21), p.11820-11829

2019

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Anthropogenic Seismicity Rates and Operational Parameters at the Salton Sea Geothermal Field

Science (American Association for the Advancement of Science), 2013-08, Vol.341 (6145), p.543-546

2013

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Fault Roughness Promotes Earthquake‐Like Aftershock Clustering in the Lab

Geophysical research letters, 2023-04, Vol.50 (8), p.n/a

2023

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Using Deep Learning for Flexible and Scalable Earthquake Forecasting

Geophysical research letters, 2023-09, Vol.50 (17), p.n/a

2023

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Roughness of fault surfaces over nine decades of length scales

Journal of Geophysical Research: Solid Earth, 2012-08, Vol.117 (B8), p.n/a

2012

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Laboratory evidence for particle mobilization as a mechanism for permeability enhancement via dynamic stressing

Earth and planetary science letters, 2014-04, Vol.392, p.279-291

2014

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Changes in permeability caused by transient stresses: Field observations, experiments, and mechanisms

Reviews of geophysics (1985), 2012-06, Vol.50 (2), p.np-n/a

2012

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The Uses of Dynamic Earthquake Triggering

Annual review of earth and planetary sciences, 2014-01, Vol.42 (1), p.317-339

2014

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Regional and stress drop effects on aftershock productivity of large megathrust earthquakes

Geophysical research letters, 2016-12, Vol.43 (23), p.12,012-12,020

2016

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Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments

Science (American Association for the Advancement of Science), 2013-12, Vol.342 (6163), p.1211-1214

2013

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Laboratory observations of permeability enhancement by fluid pressure oscillation of in situ fractured rock

Journal of Geophysical Research, 2011-02, Vol.116 (B2), p.n/a, Article B02311

2011

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Faults smooth gradually as a function of slip

Earth and planetary science letters, 2011-02, Vol.302 (1-2), p.185-193

2011

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Connecting near-field and far-field earthquake triggering to dynamic strain

Journal of Geophysical Research: Solid Earth, 2010-07, Vol.115 (B7), p.n/a

2010

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Geometric and rheological asperities in an exposed fault zone

Journal of Geophysical Research - Solid Earth, 2009-02, Vol.114 (B2), p.B02301-n/a

2009

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Gravity‐Independent Grain Size Segregation in Experimental Granular Shear Flows as a Mechanism of Layer Formation

Geophysical research letters, 2018-08, Vol.45 (16), p.8136-8144

2018

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Continuous Permeability Measurements Record Healing Inside the Wenchuan Earthquake Fault Zone

Science (American Association for the Advancement of Science), 2013-06, Vol.340 (6140), p.1555-1559

2013

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Seismological Stress Drops for Confined Ruptures Are Invariant to Normal Stress

Geophysical research letters, 2023-05, Vol.50 (9), p.n/a

2023

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Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake

Science (American Association for the Advancement of Science), 2013-12, Vol.342 (6163), p.1208-1211

2013

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Fault rock injections record paleo-earthquakes

Earth and planetary science letters, 2012-06, Vol.335-336, p.154-166

2012

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The correlation between run‐up and repose times of volcanic eruptions

Geophysical journal international, 2012-03, Vol.188 (3), p.1025-1045

2012

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Distinguishing between rheophysical regimes of fluid-saturated granular-flows using dilatancy and acoustic emission measurements

Granular matter, 2021-05, Vol.23 (2), Article 44

2021

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Long-range triggered earthquakes that continue after the wave train passes

Geophysical research letters, 2006-08, Vol.33 (15), p.L15313-n/a

Brodsky, Emily E.

2006

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Rupture‐Depth‐Varying Seismicity Patterns for Major and Great (Mw ≥ 7.0) Megathrust Earthquakes

Geophysical research letters, 2017-10, Vol.44 (19), p.9663-9671

2017

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Deep low-frequency tremor that correlates with passing surface waves

Journal of Geophysical Research - Solid Earth, 2008-01, Vol.113 (B1), p.B01307-n/a

2008

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Recognizing Foreshocks from the 1 April 2014 Chile Earthquake

Coseismic Rupture Process of the Large 2019 Ridgecrest Earthquakes From Joint Inversion of Geodetic and Seismological Observations

Anthropogenic Seismicity Rates and Operational Parameters at the Salton Sea Geothermal Field

Fault Roughness Promotes Earthquake‐Like Aftershock Clustering in the Lab

Using Deep Learning for Flexible and Scalable Earthquake Forecasting

Roughness of fault surfaces over nine decades of length scales

Laboratory evidence for particle mobilization as a mechanism for permeability enhancement via dynamic stressing

Changes in permeability caused by transient stresses: Field observations, experiments, and mechanisms

The Uses of Dynamic Earthquake Triggering

Regional and stress drop effects on aftershock productivity of large megathrust earthquakes

Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments

Laboratory observations of permeability enhancement by fluid pressure oscillation of in situ fractured rock

Faults smooth gradually as a function of slip

Connecting near-field and far-field earthquake triggering to dynamic strain

Geometric and rheological asperities in an exposed fault zone

Gravity‐Independent Grain Size Segregation in Experimental Granular Shear Flows as a Mechanism of Layer Formation

Continuous Permeability Measurements Record Healing Inside the Wenchuan Earthquake Fault Zone

Seismological Stress Drops for Confined Ruptures Are Invariant to Normal Stress

Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake

Fault rock injections record paleo-earthquakes

The correlation between run‐up and repose times of volcanic eruptions

Distinguishing between rheophysical regimes of fluid-saturated granular-flows using dilatancy and acoustic emission measurements

Long-range triggered earthquakes that continue after the wave train passes

Rupture‐Depth‐Varying Seismicity Patterns for Major and Great (Mw ≥ 7.0) Megathrust Earthquakes

Deep low-frequency tremor that correlates with passing surface waves

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