Results 11 to 20 of about 25,655 (271)
Tidal modulation of slow slip in Cascadia [PDF]
Several studies have shown that the seismic tremor in episodic tremor and slip is tidally modulated, suggesting a sensitivity to the rather small tidal stresses. We address whether the slip rate in slow slip events is also tidally modulated by examining data from six borehole strainmeters in northwest Washington and southern Vancouver Island.
Jessica C Hawthorne, Allan M Rubin
exaly +6 more sources
Slow slip and the transition from fast to slow fronts in the rupture of frictional interfaces. [PDF]
Significance Relative motion between solids in frictional contact is known to start progressively, with a slipping zone growing along the interface. The propagation of the front separating the stuck and slipping zones is usually very fast, but it can also slow down considerably. This transition is not yet understood. Using a multiscale model,
Trømborg JK +5 more
europepmc +7 more sources
The slow slip of viscous faults [PDF]
AbstractWe examine a simple mechanism for the spatiotemporal evolution of transient, slow slip. We consider the problem of slip on a fault that lies within an elastic continuum and whose strength is proportional to sliding rate. This rate dependence may correspond to a viscously deforming shear zone or the linearization of a nonlinear, rate‐dependent ...
Robert C. Viesca, Pierre Dublanchet
core +6 more sources
Slow slip events are regular earthquakes [PDF]
Abstract Slow slip events usually occur downdip of seismogenic zones in subduction megathrusts and crustal faults, with rupture speeds much slower than earthquakes. The empirical moment-duration scaling relation can help constrain the physical mechanism of slow slip events, yet it is still debated whether this scaling is linear or cubic and a ...
Weng, Huihui
openaire +2 more sources
Slow slip source characterized by lithological and geometric heterogeneity. [PDF]
Slow slip events on subduction megathrusts are linked to subduction of rough crust and heterogeneous fault rock properties.
Barnes PM +53 more
europepmc +10 more sources
Slow slip modulates low-frequency seismicity on the Parkfield segment of the San Andreas Fault [PDF]
Understanding how slow slip events (SSEs) influence fault behavior is essential for characterizing the fault slip spectrum and its role in earthquake generation.
Zahra Zali +3 more
doaj +2 more sources
Is There Slow Slip on the Wasatch Fault?
To accurately determine the earthquake hazard posed by a fault, we need to understand both strain accumulation and release along the fault. Strain accumulates during aseismic periods but it is released during fault slip events that can be either seismic or aseismic.
Jeppson, Tamara N.
openaire +4 more sources
Global subduction slow slip events and associated earthquakes. [PDF]
Three decades of geodetic monitoring have established slow slip events (SSEs) as a common mode of fault slip, sometimes linked with earthquake swarms and in a few cases escalating to major seismic events. However, the connection between SSEs and earthquake hazard has been difficult to quantify and contextualize beyond regional studies.
Dascher-Cousineau K, Bürgmann R.
europepmc +3 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
The Ocean's Impact on Slow Slip Events
We test the hypothesis that ocean seafloor pressures impart stresses that alter the initiation or termination of transient slow slip events (SSEs) on shallow submarine and near‐coastal faults, using simulated seafloor pressures and a new catalog of SSEs ...
J. Gomberg +4 more
doaj +2 more sources

