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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
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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
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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
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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
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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
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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
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SEJSMICZNOŚĆ, TRZĘSIENIA ZIEMI I LINGWISTYKA [PDF]
The general mechanism of earthquakes has been known for over a hundred years. The stresses accumulated over the years around the fault – the effect of tectonic plates movement relative to each other and deforming – must be released from time to time by ...
Piotr Senatorski
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Slow slip events (SSEs) along subduction zones play an important role in accommodating relative plate motion. SSEs interplay with large megathrust earthquakes and other slow earthquakes, including low frequency and very low frequency earthquakes.
Takuya Nishimura
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Very Low Frequency Earthquakes in Between the Seismogenic and Tremor Zones in Cascadia?
Megathrust earthquakes and their associated tsunamis cause some of the worst natural disasters. In addition to earthquakes, a wide range of slip behaviors are present at subduction zones, including slow earthquakes that span multiple orders of spatial ...
Wenyuan Fan +6 more
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Ocean-bottom and surface seismometers reveal continuous glacial tremor and slip
Anomalously slow earthquakes play a critical role in the earthquake cycle and fault sliding. Here, the authors detect continuous seismic radiation from a glacier sliding over its bed and show persistent coastal shaking to represent an addition to the ...
Evgeny A. Podolskiy +3 more
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