Results 21 to 30 of about 9,671 (264)
The Transient and Intermittent Nature of Slow Slip
To first order, faults are locked while stress builds up to a devastating earthquake. However, we know that faults also slip slowly. After decades of geophysical observation, slow slip is now recognized as part of a continuum of transient deformation ...
R. Jolivet, W. B. Frank
doaj +2 more sources
Subdaily Slow Fault Slip Dynamics Captured by Low‐Frequency Earthquakes [PDF]
Geodetic positioning is the geophysical record of reference for slow slip events, but typical daily solutions limit studies of the evolution of slow slip to its long‐term dynamics.
Caroline Mouchon +4 more
doaj +2 more sources
Slow Slip Events in New Zealand: Irregular, yet Predictable? [PDF]
Current earthquake forecasting approaches are mainly based on probabilistic assumptions, as earthquakes seem to occur randomly. Such apparent randomness can however be caused by deterministic chaos, rendering deterministic short‐term forecasts possible ...
S. Truttmann +4 more
doaj +2 more sources
Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone [PDF]
Slow earthquakes are now increasingly recognised to occur at plate boundaries globally. Here, the authors examine seafloor observational data from the Nankai trough and find that very-low-frequency events and slow-slip events frequently occur together ...
Masaru Nakano +4 more
doaj +2 more sources
Secondary acceleration of slip fronts driven by slow slip event coalescence in subduction zones [PDF]
Abstract The coalescence of slow slip events (SSEs) in subduction zones has been proposed as a potential precursor to large earthquakes, yet the physical conditions under which SSE fronts coalesce remain poorly understood. Here, we investigate coalescing SSEs along the Cascadia subduction zone. Using Global Navigation Satellite System
Ji Wang +7 more
openaire +3 more sources
Origin of slow earthquake statistics in low-friction soft granular shear [PDF]
Slow earthquakes differ from regular earthquakes in their slower moment release and size distribution dominated by smaller events. However, the physical origin of these slow earthquake statistics remains controversial.
Yuto Sasaki, Hiroaki Katsuragi
doaj +2 more sources
Near Real-Time Cascadia Slow Slip Events
Slow Slip Events (SSEs) play an important role in the seismic cycle, participating in the moment budget of active faults. SSEs can be monitored via space geodesy (e.g., Global Navigation Satellite System, GNSS). One of the major challenges when studying geodetic data is that they record the deformation due to many active sources (e.g., tectonic ...
Adriano Gualandi, Matthieu Darcy
core +5 more sources
Monitoring and predicting fault slip behaviors in subduction zones is essential for understanding earthquake cycles and assessing future earthquake potential. We developed a data assimilation method for fault slip monitoring and the short-term prediction
Masayuki Kano +4 more
doaj +2 more sources
Slow slip events and flank instability at Mt. Etna volcano (Italy) [PDF]
Highlights • A set of slow slip events occurred at Mt. Etna volcano is analyzed. • Two distinct families of slow slip events have been detected. • Most of the deformation affecting the eastern flank occurs aseismically.
Calcaterra, Stefano +4 more
core +2 more sources
Effects of episodic slow slip on seismicity and stress near a subduction-zone megathrust
Large slow slip earthquakes and tremor occur in subduction zones near the locked megathrust. Combined analysis of changes in slab seismicity and stress field near the times of such slow slip events highlights the role of fluid in promoting slow slip.
Saeko Kita +6 more
doaj +1 more source

