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Structural barriers control the spatial extent of slow earthquake slip [PDF]
Recent seismological and geodetic observations have revealed shallow slow earthquakes on subduction megathrusts, offering an opportunity to explore the factors controlling megathrust slip.
Takeshi Akuhara +18 more
doaj +2 more sources
A Brownian walk model for slow earthquakes [PDF]
Along some subduction plate boundaries, slow deformation is observable as seismically detected deep low‐frequency tremor and geodetically detected slow slip events. These phenomena are considered as different manifestations of slow earthquakes characterized by fairly constant seismic moment rate.
Satoshi Ide
exaly +2 more sources
Errata to "Characteristic activities of slow earthquakes in Japan". [PDF]
Obara K.
europepmc +4 more sources
Spontaneous complexity in the dynamics of slow laboratory earthquakes
Rock deformation experiments play a key role in our understanding of earthquake physics and friction constitutive laws. These laws commonly describe the response of analogue laboratory faults as a simple and homogeneous system, without accounting for the
G. Pozzi +5 more
doaj +3 more sources
Fast and slow earthquakes are predominantly generated along faults constituting active plate boundaries. Characterized by repeated devastating earthquakes and frequent slow slip events and tremors, the Alaska megathrust presents a chance to understand ...
Rui Qu +4 more
doaj +1 more source
Frictional and Lithological Controls on Shallow Slow Slip at the Northern Hikurangi Margin
Slow slip events (SSEs) have been identified at subduction zones globally as an important link in the continuum between elastodynamic ruptures and stable creep.
Srisharan Shreedharan +5 more
doaj +1 more source
A review of tidal triggering of global earthquakes
Earthquake prediction remains a challenging and difficult task for scientists all over the world. The tidal triggering of earthquakes is being proven by an increasing number of investigations, most of which have shown that earthquakes are positively ...
Ruyu Yan +4 more
doaj +1 more source
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 the upper surface of the subducted Philippine Sea Plate.
Shunsuke Takemura +7 more
doaj +1 more source
The tidal triggering of earthquakes has been studied for many years. The discovery of slow earthquakes in the early 2000s, including slow slip, has urged scientists to investigate the tidal responses of these earthquakes due to their sensitivity to weak ...
Yoshiyuki Tanaka +3 more
doaj +1 more source
Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution monitoring of slow earthquakes is necessary to understand tectonic conditions.
Satoru Baba +7 more
doaj +1 more source

