Results 161 to 170 of about 5,137,744 (297)
Can earthquake size be controlled by the initial seconds of rupture?
It has been argued that the dominant period T_p derived from the initial seconds of a seismogram, hence only depending on the initial phases of earthquake rupture, seems to scale with the final size of the earthquake.
Nielsen, S.
core +1 more source
Abstract Slow slip events (SSEs) represent an aseismic transient slip mode that repeats quasi‐periodically, near or partially overlapping with the megathrust earthquake zone. However, the process of stress interaction between SSEs and earthquake zones is not clearly understood.
Luhong Lu, Yajing Liu
wiley +1 more source
Earthquake-triggered cascading hazards under Arctic amplification. [PDF]
de Melo GWS +11 more
europepmc +1 more source
Peak Ground Velocity Constrains the Scaling and Variability of Seismic Radiated Energy
Abstract Seismic radiated energy is fundamental to earthquake physics, yet its scaling remains debated. Two conflicting views—magnitude‐invariant apparent stress and systematically increasing apparent stress—have persisted partly because source spectral estimates are poorly constrained.
S. Shimmoto, F. Cotton
wiley +1 more source
Pacific tsunami records suggest similar rupture locations of two great Kamchatka earthquakes only 73 years apart. [PDF]
Carvajal M +4 more
europepmc +1 more source
Abstract Quantifying earthquake size across scales requires linking physical source parameters to empirical magnitude measures, especially for microearthquakes where attenuation, scattering, and instrumental limitations complicate source characterization.
Zaiwang Liu +4 more
wiley +1 more source
Shallow creep and confined ruptures in frictionally unstable mica schist. [PDF]
Güvercin SE +5 more
europepmc +1 more source
Abstract Geodetic and seismic observations before the 2011 Mw 9.0 Tohoku‐oki earthquake indicate decadal‐scale acceleration of aseismic slip along the northern Japan Trench, but the mechanism remains debated. We show that this transient can be explained by creep‐front propagation that progressively erodes heterogeneously locked asperities.
Kaj M. Johnson, Eric D. Burton
wiley +1 more source
Modeling Long-Term Postseismic Deformation Following the 2020 Mw 7.0 Samos Earthquake Using Campaign and Continuous GNSS Observations. [PDF]
Solak Hİ +13 more
europepmc +1 more source
Abstract To understand what governs earthquake size, we investigated the 2021 Mw 7.0 Japan Trench earthquake, which began near a nest of repeating earthquakes. High‐precision hypocenter relocation and P‐waveform correlation show that the mainshock initiated nearly identically to Mw 3.8 repeaters.
Keisuke Yoshida, Satoshi Ide, Yihe Huang
wiley +1 more source

