Results 21 to 30 of about 5,920,802 (202)

Random stress and Omori's law [PDF]

open access: yesGeophysical 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.
openaire   +3 more sources

Influence of Rock Watering on Post-Seismic Activity: A Study on the Khibiny Massif

open access: yesRussian 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
doaj   +1 more source

Comprehensive analysis of tornado statistics in comparison to earthquakes: intensity and temporal behaviour [PDF]

open access: yesNonlinear 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
doaj   +1 more source

Mw ≥ 5 aftershocks of the 2008 Sichuan earthquake: Analysis of temporal variation of Omori Law p-value

open access: yesFrontiers 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
doaj   +1 more source

Interpretation of the Omori law [PDF]

open access: yesIzvestiya, Physics of the Solid Earth, 2016
5 pages.
openaire   +2 more sources

Omori law for sliding of blocks on inclined rough surfaces [PDF]

open access: yesPhysica A: Statistical Mechanics and its Applications, 2001
Long sequences of slidings of solid blocks on an inclined rough surface submitted to small controlled perturbations are examined and scaling relations are found for the time distribution of slidings between pairs of large events as well as after and before the largest events. These scaling laws are similar to the Omori law in seismology but the scaling
Parteli, E. J. R.   +3 more
openaire   +2 more sources

Transient postseismic slip and aftershock triggering: A case study of the 2008 MW7.9 Wenchuan Earthquake, China[Key points]

open access: yesEarthquake Science, 2023
In this study, we investigate how a stress variation generated by a fault that experiences transient postseismic slip (TPS) affects the rate of aftershocks.
Mengyu Xie, Baoping Shi, Lingyuan Meng
doaj   +1 more source

Bridging aero-fracture evolution with the characteristics of the acoustic emissions in a porous medium

open access: yesFrontiers in Physics, 2015
The characterization and understanding of rock deformation processes due to fluid flow is a challenging problem with numerous applications. The signature of this problem can be found in Earth Science and Physics, notably with applications in natural ...
Semih eTurkaya   +7 more
doaj   +1 more source

“Aftershock Faults” and What They Could Mean for Seismic Hazard Assessment [PDF]

open access: yesThe Seismic Record, 2023
We study stress‐loading mechanisms for the California faults used in rupture forecasts. Stress accumulation drives earthquakes, and that accumulation mechanism governs recurrence.
Tom Parsons   +2 more
doaj   +1 more source

Phenomenology of aftershocks: Once more on the Omori Law

open access: yes, 2022
Omori Law describes the evolution of the aftershocks of a strong earthquake. Established at the end of the century before last, it is characterized by the beauty of its form, quite definite clarity, as a result of which it still attracts considerable attention of the geophysical community. In recent years, we have accumulated considerable experience in
Guglielmi, A. V.   +3 more
openaire   +2 more sources

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