EB
Member Since 1995
Emily E. Brodsky
Professor, University of California Santa Cruz
AGU Research
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Understanding the Relationship Between Precursory Locking, Earthquake Nucleation, Slip, and Asperities Using a Novel Laboratory Fault
RUPTURE AND DEFORMATION PROCESSES, FROM SLOW TO FAST AND FROM MICRO TO MACRO III POSTER
mineral and rock physics | 15 december 2023
Will Steinhardt, Emily E. Brodsky
The relationship between the nucleation behavior of an earthquake, the location of stress asperities, and the final, resultant event is a critical ele...
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Earthquake Triggering Using Continuous Waveform of a Dense Network: A Case Study in Southern California
EARTHQUAKE MONITORING: RECENT DEVELOPMENTS AND CHALLENGES IN NETWORK SEISMOLOGY AND GEODESY III ORAL
seismology | 15 december 2023
Huiyun Guo, Emily E. Brodsky, Masatoshi Miyazawa
Establishing statistically significant triggering rates necessitates the analysis of a large population of earthquakes. The availability of high-quali...
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Field deployment of new borehole instruments to track fault hydrogeological response to earthquakes
FAULT ZONE FLUID MIGRATION AND INDUCED SEISMICITY POTENTIAL IN GEOENERGY TECHNOLOGIES I POSTER
hydrology | 15 december 2023
Craig Ulrich, Yves Guglielmi, Michelle Robertson, ...
Co-seismic hydrological responses following earthquakes have been documented in a large number of cases over the last decade. Observations suggest tha...
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Induced Seismicity and Surface Deformation Associated with Long-term and Abrupt Relative Flow Rate Changes in Blue Mountain Geothermal Reservoir.
GEOENERGY-INDUCED SEISMICITY: DETECTION, MANAGEMENT, AND MITIGATION II ORAL
seismology | 15 december 2023
Roshan Koirala, Emily E. Brodsky, Grzegorz Kwiatek...
Injection and extraction of fluids from geothermal reservoirs can result in stress perturbations sufficient to trigger seismic activity and ground def...
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To heal or not to heal?: The moment-recurrence time behavior of repeating earthquakes in the 2011 Prague, Oklahoma aftershock sequence is consistent with laboratory healing rates
DERISKING INDUCED AND TRIGGERED EARTHQUAKES: ADVANCES IN THEORY, MONITORING, AND FORECAST MODELING II ORAL
seismology | 15 december 2023
Kristina Okamoto, Heather M. Savage, Emily E. Brod...
The competition between fault healing (i.e., re-strengthening) and fault loading determine the seismic cycle. Therefore, understanding how faults stre...
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First contact: defining contact asperities in the spatial structure of fault roughness
FRACTURE ROUGHNESS ANALYSIS AND INFLUENCE OF FAULT STRUCTURAL MATURITY ON EARTHQUAKE BEHAVIOR II ORAL
tectonophysics | 13 december 2023
James D. Kirkpatrick, Emily E. Brodsky, Will Stein...
Developing a comprehensive description of fault surface roughness is critical to understanding the physics of fault slip since surface roughness dicta...
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Frictional properties of the San Andreas Fault at the northern transition zone, San Juan Bautisa, CA
BRIDGING FIELD AND LABORATORY STUDIES TO UNVEIL THE MECHANISMS OF UNSTABLE FAULT SLIP II POSTER
tectonophysics | 13 december 2023
Julia E. Krogh, Heather M. Savage, Emily E. Brodsk...
The San Andreas Fault is functionally divided into three regions: the northern and southern locked sections, which are capable of producing large eart...
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Can low-frequency earthquakes help forecast earthquakes?
STATISTICAL SEISMOLOGY EXPANDED: OBSERVATION, MODELING, TESTING, AND FORECASTING I POSTER
seismology | 13 december 2023
Gaspard Farge, Kelian Dascher-Cousineau, Emily E. ...
Low-frequency earthquakes (LFEs) and affiliated seismic phenomena (tremor, very-low frequency earthquakes) occur around the regions of faults that pr...
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