Results 91 to 100 of about 9,765 (206)
Aging in coherent noise models and natural time
Event correlation between aftershocks in the coherent noise model is studied by making use of natural time, which has recently been introduced in complex time-series analysis.
B. Gutenberg +5 more
core +1 more source
Residual Strain Mechanism of Aftershocks and Exponents of the Modified Omori's Law [PDF]
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
openaire +1 more source
Unsupervised Likelihood Inference of the b‐Value via Magnitude Differences
Abstract Estimating the Gutenberg–Richter b‐value from seismic catalogs is critical for earthquake forecasting and hazard assessment. However, traditional approaches rely on predefined magnitude thresholds and are highly sensitive to catalog incompleteness, limiting their applicability in automated or real‐time settings.
C. Godano, E. Lippiello, G. Petrillo
wiley +1 more source
Universal mean moment rate profiles of earthquake ruptures
Earthquake phenomenology exhibits a number of power law distributions including the Gutenberg-Richter frequency-size statistics and the Omori law for aftershock decay rates.
Amit P. Mehta +17 more
core +1 more source
The mechanisms of spatial and temporal earthquake clustering
The number of earthquakes as a function of magnitude decays as a power law. This trend is usually justified using spring-block models, where slips with the appropriate global statistics have been numerically observed.
A. B. Kolton +74 more
core +1 more source
Abstract The b‐value from the Gutenberg‐Richter law is a crucial parameter in the assessment of seismic hazard. Its temporal variations may also bring useful insights on the processes driving seismicity at depth, even if not yet fully understood. In this paper, we focus on the temporal evolution of the b‐value in the Ubaye Region (French Western Alps ...
Marion Baques +4 more
wiley +1 more source
Reduced seismic activity after mega earthquakes
Mainshocks are often followed by increased earthquake activity (aftershocks). According to the Omori-Utsu law, the rate of aftershocks decays as a power law over time.
Yongwen Zhang +3 more
doaj +1 more source
Aftershocks following crash of currency exchange rate: The case of RUB/USD in 2014
The dynamical behavior of the currency exchange rate after its large-scale catastrophe is discussed through a case study of the rate of Russian rubles to US dollars after its crash in 2014.
Abe, Sumiyoshi +2 more
core +1 more source
Signatures of criticality in turning avalanches of schooling fish
Moving animal groups transmit information through propagating waves or behavioral cascades, exhibiting characteristics akin to systems near a critical point from statistical physics. Using data from freely swimming schooling fish in an experimental tank,
Andreu Puy +4 more
doaj +1 more source
Scale-invariant statistics of period in directed earthquake network
A new law regarding structure of the earthquake networks is found. The seismic data taken in California is mapped to a growing directed network. Then, statistics of period in the network, which implies that after how many earthquakes an earthquake ...
Abe +11 more
core +2 more sources

