Results 81 to 90 of about 880,168 (206)
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 spatial-temporal evolution of structures in the sample.
Giacomo Pozzi +5 more
openaire +2 more sources
The earthquake, the tsunami and the nuclear meltdown in Japan [PDF]
Bergmann JR. The earthquake, the tsunami and the nuclear meltdown in Japan. ZiF-Mitteilungen.
Bergmann, Jörg R.
core
Observations of the 2019 magnitude 7.1 Ridgecrest, California, earthquake indicate a relatively slow rupture (∼2 km/s). The fault is surrounded by sedimentary rocks and low‐velocity damage zones, which can amplify ground motions but also slow down ...
Elif Oral +2 more
doaj +1 more source
The role of epsilon for the identification of groups of earthquake inputs of given hazard
Response spectra have been used in the years not only to obtain estimations of the seismic response for given dynamic system in response spectral analysis, but also as a useful reference for the identification of design time-history inputs (when time ...
GASPARINI, GIADA +2 more
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Relationship of preseismic, coseismic, and postseismic fault ruptures of two large interplate aftershocks of the 2011 Tohoku earthquake with slow-earthquake activity. [PDF]
Kubo H, Nishikawa T.
europepmc +1 more source
Estimating Consumer Valuation of Earthquake Risk: Evidence from Japanese Housing Markets [PDF]
The relationships between seismic risk and rental and owner- occupied housing prices in the whole of Japan are examined. The empirical results from hedonic regressions with earthquake risk indices suggest that: (1) earthquake occurrence probability has a
Michio Naoi, Kazuto Sumita, Miki Seko
core
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 +1 more source
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
doaj +1 more source
The 2010 Chile Earthquake: a five-year reflection
At 3:34AM local time, on February 27th, 2010, a moment magnitude Mw 8.8 megathrust earthquake struck offshore the coast of Chile. The earthquake ruptured a 540 by 200 km mature seismic gap of the underlying subduction pacific plate interlocking mechanism.
Vásquez P., Jorge +6 more
core
Understanding the cause of spatial variations in seismicity is crucial for comprehending the physics governing earthquake activity. Off Iwate, in the northern Japan Trench subduction zone, the plate boundary can be divided into three distinct zones based
Yuta Ito +4 more
doaj +1 more source

