Results 41 to 50 of about 3,058,004 (213)
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
doaj +1 more source
Random stress and Omori's law [PDF]
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
Omori's law in the Internet traffic [PDF]
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
openaire +2 more sources
Influence of Rock Watering on Post-Seismic Activity: A Study on the Khibiny Massif
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]
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
Mainshocks are aftershocks of conditional foreshocks: How do foreshock statistical properties emerge from aftershock laws [PDF]
The inverse Omori law for foreshocks discovered in the 1970s states that the rate of earthquakes prior to a mainshock increases on average as a power law ~ 1/(t_c-t)^p' of the time to the mainshock occurring at t_c.
Abercrombie +88 more
core +5 more sources
Sub-critical and Super-critical Regimes in Epidemic Models of Earthquake Aftershocks [PDF]
We present an analytical solution and numerical tests of the epidemic-type aftershock (ETAS) model for aftershocks, which describes foreshocks, aftershocks and mainshocks on the same footing.
Abercrombie +84 more
core +3 more sources
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
Creep rupture as a non-homogeneous Poissonian process [PDF]
Creep rupture of heterogeneous materials occurring under constant sub-critical external loads is responsible for the collapse of engineering constructions and for natural catastrophes.
Danku, Zsuzsa, Kun, Ferenc
core +2 more sources
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

