The geophysics, geology and mechanics of slow fault slip
R Bürgmann - Earth and Planetary Science Letters, 2018 - Elsevier
Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …
Slow earthquake scaling reconsidered as a boundary between distinct modes of rupture propagation
The scaling law for slow earthquakes, which is a linear relationship between seismic
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …
A review of shallow slow earthquakes along the Nankai Trough
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough.
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Slow slip events in the roots of the San Andreas fault
Episodic tremor and accompanying slow slip are observed at the down-dip edge of
subduction seismogenic zones. While tremors are the seismic signature of this …
subduction seismogenic zones. While tremors are the seismic signature of this …
Self-similarity of low-frequency earthquakes
Low-frequency earthquakes are a particular class of slow earthquakes that provide a unique
source of information on the physical processes along a subduction zone during the …
source of information on the physical processes along a subduction zone during the …
[HTML][HTML] Seismic energy radiation and along-strike heterogeneities of shallow tectonic tremors at the Nankai Trough and Japan Trench
Shallow slow earthquakes have been documented along shallow plate interfaces near
trenches. Recent geophysical observation networks located offshore of Japan enable us to …
trenches. Recent geophysical observation networks located offshore of Japan enable us to …
Fault zone heterogeneities explain depth-dependent pattern and evolution of slow earthquakes in Cascadia
Y Luo, Z Liu - Nature Communications, 2021 - nature.com
Slow earthquakes including tremor and slow-slip events are recent additions to the
conventional earthquake family and have a close link to megathrust earthquakes. Slow …
conventional earthquake family and have a close link to megathrust earthquakes. Slow …
Moment‐duration scaling of low‐frequency earthquakes in Guerrero, Mexico
Low‐frequency earthquakes (LFEs) are detected within tremor, as small, repetitive,
impulsive low‐frequency (1–8 Hz) signals. While the mechanism causing this depletion of …
impulsive low‐frequency (1–8 Hz) signals. While the mechanism causing this depletion of …
Observing and modeling the spectrum of a slow slip event
JC Hawthorne, NM Bartlow - Journal of Geophysical Research …, 2018 - Wiley Online Library
We estimate and model the normalized moment rate power spectrum of large slow slip
events in Cascadia. We estimate the spectrum using data from GPS‐derived slip inversions …
events in Cascadia. We estimate the spectrum using data from GPS‐derived slip inversions …
Revisiting seismic energy of shallow tremors: Amplifications due to site and propagation path effects near the Nankai Trough
S Takemura, K Emoto, S Yabe - Journal of Geophysical …, 2024 - Wiley Online Library
We investigated the effects of the propagation path and site amplification of shallow tremors
along the Nankai Trough. Using far‐field S‐wave propagation from intraslab earthquake …
along the Nankai Trough. Using far‐field S‐wave propagation from intraslab earthquake …