1International Institute of Earthquake Prediction Theory and Mathematical Geophysics,
Russian Academy of Sciences, Warshavskoe sh. 79, korp. 2, 113556 Moscow, Russia …

The Omori formula n (t)= K (t+ c)-1 and its modified form n (t)= K (t+ c)-P have been
successfully applied to many aftershock sequences since the former was proposed just 100 …

Earthquake prediction ADS Classic is now deprecated. It will be completely retired in October
2019. This page will automatically redirect to the new ADS interface at that point. SAO/NASA …

An earthquake of magnitude M and linear source dimension L (M) is preceded within a few
years by certain patterns of seismicity in the magnitude range down to about (M-3) in an …

There is accumulating evidence that distributed seismicity is a problem in statistical physics.
Seismicity is taken to be a type example of self-organized criticality. This association has …

Distributed seismicity appears to fit the definition of a self-organized, critical phenomenon. In
this paper a cellular-automata model is presented as an analog to distributed seismicity. We …

Earthquakes are a direct consequence of the deformation of the Earth's crust. Parts of the
crust are brittle, and significant deformation requires fractures to develop. Deformation …

The frequency-magnitude statistics of earthquakes have long been known to satisfy the
Gutenberg-Richter relation; it is easy to show that this relation is fractal with D= l. 8-2. Since it …

This article explores the problem of short-term earthquake prediction based on spatio-
temporal variations of seismicity. Previous approaches to this problem have used precursory …

A catalog of shallow Mexican earthquakes (depth≤ 60 Km) is presented for a region
bounded by north latitude and west longitude, covering the period from January, 1806 to …