Results 71 to 80 of about 353 (168)
Short term afterslip in the 1994 Sanriku‐Haruka‐Oki Earthquake
Geophysical Research Letters, 1997 The Sanriku‐Haruka‐Oki earthquake, that occurred on December 28, 1994 at the Japan Trench as a typical interplate thrust event, was followed by year‐long afterslip as large as the slip in the high‐speed rupture [Heki et al., 1997]. Here we report on the transition between these, inferred from crustal movements during the five days interval before and ...
Kosuke Heki, Yoshiaki Tamura
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Remote SensingThe Mw = 7.1 Wushi earthquake is the second-largest digitally recorded earthquake in the Tianshan seismic zone and provides an opportunity to explore the structural characteristics of the Tianshan seismic zone.
Xiaoran Lv +4 more
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Heterogeneous rheology controlled postseismic deformation of the 2011 Tohoku‐Oki earthquake
Geophysical Research Letters, 2016 Using two‐dimensional finite element modeling, we reproduced the observed postseismic deformation of the 2011 Tohoku‐Oki earthquake. Our model, which accounts for the lithosphere‐asthenosphere boundary and weak zones beneath volcanoes, was able to ...
Jun Muto +6 more
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Implications of rate and state dependent friclion for creep on shallow faults
Annals of Geophysics, 1994 The aseismic sliding on shallow strike-slip faults, under the assumption of a non linear constitutive equation (velocity strengthening), is here treated as a two-dimensional quasi-static crack problem whose equations are solved numerically (boundary ...
M. E. Belardinelli
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Geophysical Research LettersSlow slip events (SSEs) release tectonic strain without causing sudden ground shaking. SSEs have been observed at many subduction zones, some dynamically triggered by stress changes due to the passage of seismic waves.
Guoli Li +3 more
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Postseismic deformation model of the 2024 Noto Peninsula earthquake, central Japan
Earth, Planets and SpaceWe investigated the characteristics and mechanism of postseismic deformation following the 2024 Noto Peninsula earthquake (M7.6), which occurred on January 1, 2024, in the Noto Peninsula, Japan.
Hisashi Suito
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Reactivated afterslip induced by a large regional earthquake, Fiordland, New Zealand
Geophysical Research Letters, 2016 AbstractThe evaluation of seismic hazard along active faults requires knowledge of the long term slip rate, the portions of the fault which are accumulating strain, and the magnitude, number, and location of past earthquakes. Aseismic slip will lower the long‐term seismic potential, but the distribution of seismic versus aseismic slip along faults is ...
I. J. Hamling, S. Hreinsdóttir
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Sub-parallel fault afterslip and weak zone relaxation after the 2024 Noto earthquake
Communications Earth & EnvironmentPostseismic deformation carries valuable information about the complex fault system and deep rheological structure. We analyzed ~6 months of postseismic deformation following the 2024 moment magnitude 7.5 Noto earthquake using InSAR and GNSS data ...
Zhangfeng Ma +4 more
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Applied SciencesOn 22 May 2021, an earthquake (98.3° E and 34.59° N) struck Maduo town in Qinghai province, occurring along a relatively obscure secondary fault within the block.
Yang He +5 more
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Rapid shallow megathrust afterslip from the 2021 M8.2 Chignik, Alaska earthquake revealed by seafloor geodesy. [PDF]
Sci Adv, 2023 Brooks BA +13 more
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