Results 11 to 20 of about 9,765 (206)
ON PROPER TIME OF THE SOURCE OF A STRONG EARTHQUAKE
Геодинамика и тектонофизика, 2023 The physics of earthquakes was contriubuted to by the concept of proper time of the source of a strong earthquake, which is different from universal (calendar) time. The earlier idea of proper time was implicit and has been considered only in relation to
A. V. Guglielmi +3 more
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Applied Sciences, 2022 The 27 September 2021 damaging mainshock (Mw6.0) close to Arkalochori village is the strongest earthquake that was recorded during the instrumental period of seismicity in Central Crete (Greece).
Filippos Vallianatos +5 more
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Earth, Planets and Space, 2020 We infer the postseismic deformation mechanisms following the 2011 Tohoku megathrust earthquake via an analysis of onshore geodetic observations. We focus on the temporal decay characteristics of postseismic deformation using continuous time-series data ...
Shunsuke Morikami, Yuta Mitsui
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Bayesian analysis of the modified Omori law [PDF]
Journal of Geophysical Research: Solid Earth, 2012 In order to examine variations in aftershock decay rate, we propose a Bayesian framework to estimate the {K, c, p}‐values of the modified Omori law (MOL), λ(t) = K(c + t)−p. The Bayesian setting allows not only to produce a point estimator of these three parameters but also to assess their uncertainties and posterior dependencies with respect to the ...
Holschneider, M. +4 more
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Random stress and Omori's law [PDF]
Geophysical Journal International, 2011 We consider two statistical regularities that were used to explain Omori's law of the aftershock rate decay: the Levy and Inverse Gaussian (IGD) distributions. These distributions are thought to describe stress behavior influenced by various random factors: post-earthquake stress time history is described by a Brownian motion.
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Dynamical scaling and generalized Omori law [PDF]
Geophysical Research Letters, 2007 The power law decay of the aftershocks rate is observed only after a characteristic time scale c. The dependence of c on the mainshock magnitude MM and on the lower cut‐off magnitude MI is well established. By considering ten sequences recorded in the California Catalog we show that the aftershock number distribution becomes independent of both MM and ...
LIPPIELLO, Eugenio +3 more
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Omori's law in the Internet traffic [PDF]
Europhysics Letters (EPL), 2003 The Internet is a complex system, whose temporal behavior is highly nonstationary and exhibits sudden drastic changes regarded as main shocks or catastrophes. Here, analyzing a set of time series data of round-trip tim measured in echo experiment with the Ping Command, the property of "aftershocks" (i.e., catastrophes of smaller scales) after a main ...
Abe, Sumiyoshi, Suzuki, Norikazu
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Influence of Rock Watering on Post-Seismic Activity: A Study on the Khibiny Massif
Russian Journal of Earth Sciences, 2023 The article is devoted to the study of the influence of watering of the rock environment on post-seismic activity in the deposits of the Khibiny mountains.
Baranov Sergey +4 more
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Comprehensive analysis of tornado statistics in comparison to earthquakes: intensity and temporal behaviour [PDF]
Nonlinear Processes in Geophysics, 2013 Tornadoes and earthquakes are characterised by a high variability in their properties concerning intensity, geometric properties and temporal behaviour. Earthquakes are known for power-law behaviour in their intensity (Gutenberg–Richter law) and temporal
L. Schielicke, P. Névir
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Frontiers in Earth Science, 2022 Strong to great earthquakes considerably weaken the structural strength of the subsurface strata and civil constructions. The occurrence of Mw ≥ 5 aftershocks further contributes to the loss of human lives and damage to property.
Harsh K. Gupta, Rajesh Rekapalli
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