Omori law for foreshocks and aftershocks in a realistic earthquake model
, 2019 We study a physical model for earthquakes which extends the standard spring-block model. It is able to quantitatively describe the observations which detect differences between the statistics of foreshocks and aftershocks and the properties of main ...
O. M. Braun, M. Peyrard
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A matched-filter technique with an objective threshold. [PDF]
Sci Rep, 2022 Hirano S, Kawakata H, Doi I.
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Two end-member earthquake preparations illuminated by foreshock activity on a meter-scale laboratory fault. [PDF]
Nat Commun, 2021 Yamashita F +5 more
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Probing the evolution of fault properties during the seismic cycle with deep learning. [PDF]
Nat CommunLaurenti L +5 more
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Foreshock-induced slip transients set mainshock nucleation timing. [PDF]
NatureFryer B +3 more
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Seismic moment efficiency reveals the potential for larger earthquakes after M6-class events. [PDF]
Sci RepMatsumoto S, Aizawa K, Matsushima T.
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Frequency-Magnitude Statistics of Laboratory Foreshocks Vary With Shear Velocity, Fault Slip Rate, and Shear Stress. [PDF]
J Geophys Res Solid Earth, 2021 Bolton DC +3 more
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, 1979 The earthquake swarms occurred at seven areas distributed in the Kanto district and foreshocks preceding the Izu-Oshima-kinkai earthquake (M=7.0) of 1978 are studied through the analysis of waveform.
Tsujiura Masaru, 辻浦 賢
core
Dynamics of non-self-similar earthquakes illuminated by a controlled fault asperity. [PDF]
Nat CommunOkubo K, Yamashita F, Fukuyama E.
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Machine learning predicts meter-scale laboratory earthquakes. [PDF]
Nat CommunNorisugi R, Kaneko Y, Rouet-Leduc B.
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