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20172021
most citedEstimating Fault Friction from Seismic Signals in the Laboratory

107 citations · 254 across the 11 of their papers we have counts for

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physics.geo-ph2020

Tremor Waveform Denoising and Automatic Location with Neural Network Interpretation

Claudia Hulbert, Romain Jolivet, Blandine Gardonio +3

Active faults release tectonic stress imposed by plate motion through a spectrum of slip modes, from slow, aseismic slip, to dynamic, seismic events. Slow earthquakes are often ass…

physics.geo-ph2019★ 51 cited

Machine Learning Reveals the Seismic Signature of Eruptive Behavior at Piton de la Fournaise Volcano

C. X. Ren, A. Peltier, V. Ferrazzini +3

Volcanic tremor is key to our understanding of active magmatic systems but, due to its complexity, there is still a debate concerning its origins and how it can be used to characte…

physics.geo-ph2019★ 40 cited

Machine Learning Reveals the State of Intermittent Frictional Dynamics in a Sheared Granular Fault

C. X. Ren, O. Dorostkar, B. Rouet-Leduc +5

Seismogenic plate boundaries are presumed to behave in a similar manner to a densely packed granular medium, where fault and blocks systems rapidly rearrange the distribution of fo…

physics.geo-ph2019★ 49 cited

From Stress Chains to Acoustic Emission

Ke Gao, Robert Guyer, Esteban Rougier +2

A numerical scheme using the combined finite-discrete element methods (FDEM) is employed to study a model of an earthquake system comprising a granular layer embedded in a formatio…

physics.geo-ph2018★ 4 cited

Estimating the Physical State of a Laboratory Slow Slipping Fault from Seismic Signals

Claudia Hulbert, Bertrand Rouet-Leduc, Christopher X. Ren +4

Over the last two decades, strain and GPS measurements have shown that slow slip on earthquake faults is a widespread phenomenon. Slow slip is also inferred from correlated small a…

physics.geo-ph2017★ 107 cited

Estimating Fault Friction from Seismic Signals in the Laboratory

Bertrand Rouet-Leduc, Claudia Hulbert, David C. Bolton +5

Nearly all aspects of earthquake rupture are controlled by the friction along the fault that progressively increases with tectonic forcing, but in general cannot be directly measur…