Remotely sensing stress evolution in elastic media: a passive approach to earthquake monitoring
Nader Shakibay Senobari

TL;DR
This paper introduces a passive seismic method to remotely monitor stress evolution in elastic media, linking laboratory experiments to large-scale earthquake observations for real-time fault mechanics tracking.
Contribution
A novel frequency-domain transform that passively detects stress changes using ambient seismic noise across different scales and earthquake events.
Findings
Consistently detects stress-cycle patterns in natural fault systems.
Reveals precursory stress trajectories before major earthquakes.
Bridges laboratory rock physics with large-scale seismology.
Abstract
Stress evolution governs material failure across scales, from microscopic fractures to large earthquakes, yet direct observation of its dynamics in natural systems has remained elusive. Laboratory experiments using active ultrasonic measurements have shown that seismic velocity and attenuation are sensitive to stress, but such monitoring has not previously been achievable remotely or passively. Here we introduce a stress-sensitive frequency-domain transform that enables passive monitoring of stress evolution using ambient seismic or acoustic noise. The method quantifies relative energy shifts between adjacent frequency bands, capturing subtle changes in wave-propagation properties linked to evolving shear and normal stress. Applied across scales, from laboratory stick-slip and slow-slip experiments to natural fault systems including the 2018 Kilauea collapse, Cascadia slow-slip…
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Taxonomy
Topicsearthquake and tectonic studies · Seismic Waves and Analysis · High-pressure geophysics and materials
