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20062026
most citedImpact of the earth's oscillations on the earthquakes

10 citations · 28 across the 22 of their papers we have counts for

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physics.geo-ph2026

On four representations of the law of aftershock evolution

A. V. Guglielmi, O. D. Zotov

The relaxation of the earthquake source following the main shock has been investigated both theoretically and experimentally, based on data regarding the evolution of aftershocks.…

physics.geo-ph2026

On the classification of triggers of dynamic processes in geophysics

A. V. Guglielmi, A. D. Zavyalov, O. D. Zotov

In geophysics, the problem of classifying triggers of dynamic processes in the lithosphere, hydrosphere, atmosphere, ionosphere and magnetosphere has arisen and needs to be solved.…

physics.geo-ph2025

Relativity of Time in Earthquake Physics

A. V. Guglielmi, O. D. Zotov

In this paper we develop an understanding of the proper time of the Tohoku earthquake source. The paper is dedicated to the 120th anniversary of Einstein's theory of relativity, bu…

physics.geo-ph2025

Evolution of the Tohoku earthquake aftershocks in the framework of the phenomenological theory of aftershocks

O. D. Zotov, A. V. Guglielmi

The aftershocks of the Tohoku earthquake are analyzed in light of the phenomenological theory of aftershocks. The theory is based on the concept of an earthquake source as a dynami…

physics.geo-ph2025

On the three laws of earthquake physics

A. V. Guglielmi, A. D. Zavyalov, O. D. Zotov +1

The paper provides a synoptic overview of a series of works carried out by a group of researchers at the Institute of Physics of the Earth RAS with the aim of finding new approache…

physics.geo-ph2025

On the elementary theory of earthquake aftershocks

A. V. Guglielmi, O. D. Zotov

The elementary theory of aftershocks, being relatively simple mathematically, belongs to the basics of earthquake physics. The paper briefly outlines the concepts and ideas of the…

physics.geo-ph2024

Classification of earthquakes main shocks

A. V. Guglielmi, O. D. Zotov

The concept of a triad of tectonic earthquakes as a natural trinity of foreshocks, main shock and aftershocks is introduced. The basis for classifying the main shocks is the belong…

physics.geo-ph2024

Around-the-world seismic echo as a trigger for aftershocks and the main shock of an earthquake

A. V. Guglielmi, O. D. Zotov

The essence of the cumulative effect of a round-the-world seismic echo is that the echo can serve as a trigger for a second tremors in the epicentral zone of the earthquake that ga…

physics.geo-ph2024★ 1 cited

Energy flows in the earthquake source before and after the main shock

A. V. Guglielmi, O. D. Zotov

We proceeded from general physical concepts based, on the one hand, on the Umoff-Poynting theorem, and on the other, on the phenomenological theory of earthquakes, and formulated t…

physics.geo-ph2023

About the aftershocks, the Omori law, and the Utsu formula

Anatol Guglielmi, Alexey Zavyalov, Oleg Zotov +1

After the main shock of an earthquake, a stream of aftershocks that does not subside for a long time is usually observed. Fusakichi Omori found that the frequency of aftershocks de…

physics.geo-ph2023★ 1 cited

Bifurcation of the earthquake source at the end of the Omori epoch

A. Guglielmi, O. Zotov

The earthquake source after the main shock can theoretically be represented as a black box without an entrance. At the output, there is a signal in the form of aftershocks, the fre…

physics.geo-ph2023

Omori Law. To the 100th anniversary of death of the famous Japanese seismologist

A. Guglielmi, B. Klain, A. Zavyalov +1

One hundred years ago, Fusakichi Omori died. Our paper is dedicated to his memory. Omori made an outstanding contribution to the physics of earthquakes. In 1894 he formulated the l…

physics.geo-ph2022★ 2 cited

About the waiting time for a strong earthquake

A. V. Guglielmi, O. D. Zotov

As an object of study, we chose the global activity of strong earthquakes (M > 7). The subject of the study is the waiting time for the next strong earthquake. The purpose of the s…

physics.geo-ph2022★ 2 cited

On the proper time of the earthquake source

A. V. Guglielmi, O. D. Zotov

The concept of proper time, which is different from universal time, has been introduced into the physics of earthquakes. The global activity of strong earthquakes was chosen as the…

physics.geo-ph2022★ 2 cited

On generalized models of earthquake evolution by the example of classical and mirror triads

A. V. Guglielmi, O. D. Zotov

The analysis of the classical and mirror triads of the sequence of earthquakes has been carried out in order to find the equations of evolution of foreshocks and aftershocks. The d…

physics.geo-ph2022

Phenomenology of aftershocks: Once more on the Omori Law

A. V. Guglielmi, B. I. Klain, A. D. Zavyalov +1

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…

physics.geo-ph2021★ 1 cited

Mirror triad of tectonic earthquakes

O. D. Zotov, A. V. Guglielmi

It is natural to call the trinity of foreshocks, main shock and aftershocks a classical triad. The magnitude of the main shock is always greater than the maximum magnitudes of fore…

physics.geo-ph2021★ 5 cited

Dependence of the source deactivation factor on the earthquake magnitude

A. V. Guglielmi, O. D. Zotov

Three fundamental laws of the physics of earthquakes, bearing the names of their discoverers Omori, Gutenberg, Richter and Bath, are widely used in original, review, monographic, a…

physics.geo-ph2020★ 1 cited

Aftershocks of the 2013 deep Okhotsk earthquake

Anatol V. Guglielmi, Oleg D. Zotov

Strong deep earthquakes occurred in the Sea of Okhotsk, May 24, 2013 at 05:44 UTC. The magnitude of the earthquake is M = 8.3, the depth of the hypocenter is 629 km. The earthquake…

physics.geo-ph2020★ 1 cited

Three New Fundamental Problems in Physics of the Aftershocks

Anatol V. Guglielmi, Alexey D. Zavyalov, Oleg D. Zotov

Recently, the physics of aftershocks has been enriched by three new problems. We will conditionally call them dynamic, inverse, and morphological problems. Dynamic problem is to se…

physics.geo-ph2012★ 10 cited

Impact of the earth's oscillations on the earthquakes

A. Guglielmi, O. Zotov

In this work we have discovered that the global seismic activity undergoes a modulation with the period of 54 min. We assume that the modulation is caused by the fundamental sphero…