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A New Fault Slip Mode Unveiled in the Regional Dynamic Triggering of the 2023 Turkey Kahramanmaraş Earthquake Sequence
AGU ADVANCES
23 february 2025
Heng Luo, Yijian Zhou, zeyan zhao, Mehmet Kokum, T...
Faults can slip at vastly different rates, generating both high‐stress‐drop regular earthquakes and low‐stress‐drop slow sl...
Are creep and seismicity along nearby faults modulated by the poroelastic transients from the Geysers geothermal field in Northern California?
ADVANCES IN UNDERSTANDING TRIGGERING MECHANISMS OF INDUCED SEISMICITY III POSTER
seismology | 13 december 2024
Sui Tung, Roland Burgmann, Manoochehr Shirzaei, Ti...
The Geyser geothermal field has been producing energy since 1960. There are several faults, namely, the Rodgers Creek Fault (RCF), Maacama Fault (MF),...
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US West Coast Surface Deformation With Wide-swath L-Band ALOS-2 PALSAR-2
CLIMATE CHANGE STUDY AND DISASTER RESPONSE USING L BAND SAR MISSIONS BY JAPAN AND THE UNITED STATES II ORAL
global environmental change | 13 december 2024
saoussen Belhadj aissa, Eric J. Fielding, Danielle...
Under a JAXA-NASA agreement, JAXA has acquired over 451 scenes in the wide-swath ScanSAR mode over the West Coast USA and provided them to NASA and ot...
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How does aseismic slip communicate with M6 events in a collision zone?
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS V POSTER
seismology | 12 december 2024
Kate H. Chen, Wei Peng, Roland Burgmann
Recognizing where and when the slow slips occurred during earthquake cycle is critical for earthquake forecasting and hazard assessment. Abundant M≥6 ...
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Coseismic Shallow Slip Deficit Accounted for by Diffuse Off‐Fault Deformation
GEOPHYSICAL RESEARCH LETTERS
12 december 2024
Solène L Antoine, Yann Klinger, Kang Wang, Roland ...
Earthquake ruptures produce fault slip and kilometer‐wide diffuse deformation of the host rocks. However, the origin of the diffuse deformati...
Temporal and Spatial Creep Variability: Detecting Decadal Changes in Fault Behavior in Northern California
SHALLOW FAULT ZONE DEFORMATION OVER THE EARTHQUAKE CYCLE: OBSERVATIONS, EXPERIMENTS, AND MODELS III ORAL
tectonophysics | 12 december 2024
Danielle Lindsay, Taka'aki Taira, Roland Burgmann
Earthquake potential along faults is not constant through time, but rather a time-dependent process whereby changes in strain accumulation over short ...
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Satellite- and airborne-based SAR and optical data reveal the stable-to-unstable sliding transition of the 2017 Mud Creek Landslide
LANDSLIDE LIFE CYCLE: FROM HAZARD ANALYSIS TO RISK ASSESSMENT IV ORAL
natural hazards | 11 december 2024
Alexander L. Handwerger, Pascal Lacroix, Andrew F....
A primary goal in landslide remote sensing is to provide information on the timing, behavior and extent of landslides in advance of failure. This info...
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GPS Analysis of Spatio-temporal Variability of Deformation at Slumgullion Landslide
GEOPHYSICAL CHARACTERIZATION AND MONITORING OF NATURAL HAZARDS I POSTER
near surface geophysics | 11 december 2024
Louisa Kaplan, Yuankun Xu, Roland Burgmann, Roger ...
Although less dramatic than catastrophic slope failures, slow-moving landslides can cause frequent infrastructure damage and progressively shape the h...
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