Results 51 to 60 of about 5,588,675 (211)
Dependence of the Omori‐Utsu law parameters on main shock magnitude: Observations and modeling [PDF]
Journal of Geophysical Research: Solid Earth, 2008 We examine the dependence on main shock magnitudemof thepandχparameters appearing in Omori‐Utsu formulaλ(t,m) =χ× (t+c)−prelating the rate of aftershocksλat timetafter a main shock. Observations point out to a significant increase ofpwithm, along with a scaling relationship of the formχ∼ 10αm.
Hainzl, S., Marsan, David
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Variations in precursory slip behavior resulting from frictional heterogeneity
Progress in Earth and Planetary Science, 2018 Precursory seismicity is often observed before a large earthquake. Small foreshocks occur within the mainshock rupture area, which cannot be explained by simple models that assume homogeneous friction on the entire fault.
Suguru Yabe, Satoshi Ide
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Earth's Future, Volume 14, Issue 8, August 2026.Abstract Statistical earthquake forecasting models, such as the Epidemic‐type Aftershock Sequence (ETAS), embed decades of empirical knowledge and assumptions about earthquake triggering, clustering, and catalog completeness. In contrast, neural spatio‐temporal point process (STPP) models often treat seismicity as generic spatiotemporal data without ...
Weixi Tian +3 more
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Aftershock Hazard Magnitude, Time, and Location Probability Forecasting
Terrestrial, Atmospheric and Oceanic Sciences, 2014 This study combines branching aftershock sequence (BASS) and modified Omori¡¦s law to develop a predictive model for forecasting the magnitude, time, and location of aftershocks of magnitude Mw ≥ 5.00 in large earthquakes.
Kuei-Pao Chen +3 more
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Aftershock Rate Changes at Different Ocean Tide Heights
Frontiers in Earth Science, 2020 The differential probability gain approach is used to estimate quantitatively the change in aftershock rate at various levels of ocean tides relative to the average rate model.
P. N. Shebalin, A. A. Baranov
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Geometric Moment Modulated and Maximum Entropy Informed Earthquake + Afterslip Sequences
Journal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.Abstract Synthetic earthquake sequences may be of interest for comparisons with seismicity and afterslip evolution from instrumental observations and deeper time paleoseismic event histories, as well as for forecasting purposes. Here, we describe a constructed method, independent of continuum mechanics, for generating long‐duration earthquake and ...
Brendan Meade
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Omori‐like decay of postseismic velocities following continental earthquakes
Geophysical Research Letters, 2017 Various mechanisms have been proposed to explain the transient, enhanced surface deformation rates following earthquakes. Unfortunately, these different mechanisms can produce very similar surface deformation patterns leading to difficulty in ...
T. Ingleby, T. J. Wright
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The Analysis of the Aftershock Sequences of the Recent Mainshocks in Alaska
Applied Sciences, 2022 The forecasting of the evolution of natural hazards is an important and critical problem in natural sciences and engineering. Earthquake forecasting is one such example and is a difficult task due to the complexity of the occurrence of earthquakes. Since
Mohammadamin Sedghizadeh +1 more
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Journal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.Abstract Temporal changes in seismicity rates can be conceptually understood as a response and consequence of stress changes. Dieterich (1994, https://doi.org/10.1029/93JB02581) formalized this relationship using empirically derived rate‐and‐state friction laws, and Heimisson and Segall (2018, https://doi.org/10.1029/2018JB015656) later generalized the
Y. Jiang, D. T. Trugman, P. J. González
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Residual Strain Mechanism of Aftershocks and Exponents of the Modified Omori's Law [PDF]
Journal of Geophysical Research: Solid Earth, 2019 AbstractThe rate of aftershocks caused by residual stresses left after a major seismic event or material failure is considered. It is assumed that the local (or “micro” with respect to the scale of the major event) failures registered as aftershocks are produced by static fatigue (delayed fracture).
A. V. Dyskin, E. Pasternak
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