-
Emily Brodsky
University of California Santa CruzMeeting roles in:
Lithology or Geometry? Frictional properties of fault gouges in the northern transition region of the San Andreas Fault highlight the importance of local effective stress
The seismic consequences of being a leaky fault
Seismological Observations of the 2011 Nabro, Eritrea Eruption: Implications for Eruptive Processes and Volcano-Tectonic Interactions
Earthquake Forecasting Using Single-Station Waveform Detection
How Do Earthquakes Get Big?
Multi-Scale Observations and Modeling of a Slow-Moving Landslide Controlled by Frictional Heterogeneity and Pore Fluid Pressure
Multi-Scale Observations and Modeling of a Slow-Moving Landslide Controlled by Frictional Heterogeneity and Pore Fluid Pressure
SZ4D: Steady Progress in Shifting Landscapes
The change of friction and compaction of shearing granular flow under acoustic vibration
The SZ4D Experiment: Comparing Subduction Zone Processes Across Three Margins I Oral
Probing the organization of stress in the slow-slipping megathrust
The SZ4D Experiment: Comparing Subduction Zone Processes Across Three Margins II Poster
Why do foreshocks occur where they do?
How Stress Distributes Across Different Granular Flow Regimes?
Enter Note
Go to previous page in this tab
Author/Chair
