EB
Member Since 1995
Emily E. Brodsky
Professor, University of California Santa Cruz
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The Influence of Fault Geometrical Complexity on Surface Rupture Length
GEOPHYSICAL RESEARCH LETTERS
16 october 2024
Alba Mar Rodriguez Padilla, Emily E. Brodsky, Keli...
Propagating earthquakes must overcome geometrical complexity on fault networks to grow into large, surface rupturing events. We map step‐over...
Characteristics of the Fault Damage Zone From High‐Resolution Seismic Imaging Along the Palos Verdes Fault, California
AGU ADVANCES
03 july 2024
Travis Alongi, Emily E. Brodsky, Jared Kluesner, D...
The distribution and intensity of fault damage zones provides insight into fault activity and its relationship to fluid flow in the crust. Presentl...
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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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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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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