Long-term slow slip event detected beneath the Shima Peninsula, central Japan, from GNSS data
Long-term slow slip events (SSEs), the largest events among slow earthquakes, occur repeatedly along the Nankai Trough, southwest Japan. Their locations, near the locked zones of the plate interface responsible for great megathrust earthquakes in the ...
Akio Kobayashi, Takahiro Tsuyuki
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Features of seismicity triggered by ripple-fired explosions at the Korobkovskoye iron ore deposit
Intensification of mining activities often lead to nucleation of strong earthquakes and fault-slip bursts in areas that were previously thought to be aseismic or of low seismicity.
Ostapchuk Aleksey +5 more
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Experimental evidence of seismic ruptures initiated by aseismic slip
Seismic faults release the stress accumulated during tectonic movement through rapid ruptures or slow-slip events. The role of slow-slip events is crucial as they impact earthquakes occurrence.
Yohann Faure, Elsa Bayart
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Fault zone heterogeneities explain depth-dependent pattern and evolution of slow earthquakes in Cascadia. [PDF]
Luo Y, Liu Z.
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Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone
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
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3-D thermal regime and dehydration processes around the regions of slow earthquakes along the Ryukyu Trench. [PDF]
Suenaga N, Yoshioka S, Ji Y.
europepmc +1 more source
Getting to the Bottom of Slow-Motion Earthquakes
For close to 20 years, slow-motion earthquakes have been an enigma. Core samples provide new clues to their origins.
openaire +1 more source
Comparison of statistical low-frequency earthquake activity models
Slow earthquakes are slow fault slip events. Quantifying and monitoring slow earthquake activity characteristics are important, because they may change before large earthquakes occur.
Tomoaki Nishikawa
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Megathrust and slow earthquakes are known to occur in the area off Kumano, along the eastern part of the Nankai Trough, Japan. Pore fluids along the fault surface play an important role in earthquake occurrence, but the detailed fluid distribution ...
Manaka Kuroda +6 more
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Similarities and Differences Between Natural and Simulated Slow Earthquakes
We investigate similarities and differences between natural and simulated slow earthquakes using nonlinear dynamical system tools. We use spatio‐temporal slip potency rate data derived from Global Navigation Satellite System (GNSS) position time series ...
A. Gualandi +3 more
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