References

gtcrust

Геодинамика и тектонофизика

Geodynamics & Tectonophysics

2078-502X

Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch

10.5800/GT-2018-9-3-0369

gtcrust-623

Research Article

ТЕКТОНОФИЗИКА

TECTONOPHYSICS

ПРЕДСКАЗАНИЕ И НАБЛЮДЕНИЕ ДЕФОРМАЦИОННЫХ ВОЛН ЗЕМЛИ

PREDICTION AND OBSERVATION OF STRAIN WAVES IN THE EARTH

https://orcid.org/0000-0002-0637-0112

Быков

В. Г.

Bykov

V. G.

Виктор Геннадьевич Быков, докт. физ.-мат. наук680000, Хабаровск, ул. Ким Ю Чена, 65

Victor G. Bykov, Doctor of Physics and Mathematics65 Kim Yu Chen Street, Khabarovsk 680000

bykov@itig.as.khb.ru

Институт тектоники и геофизики им. Ю.А. Косыгина ДВО РАНРоссияYu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch of RASRussian Federation

2018

08102018

93721754

2018

Быков В.Г.

Bykov V.G.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://www.gt-crust.ru/jour/article/view/623

Теоретическое открытие деформационных волн Земли – одно из наиболее важных событий в геофизике последней трети XX века – послужило мотивацией к развитию физических основ математической теории распространения этих волн и поиску методов их экспериментального обнаружения. В статье кратко представлена история развития концепции деформационных волн Земли, методы наблюдения и свойства деформационных волн, основные типы геологических структур, генерирующих эти волны. Приведены наиболее значительные результаты теоретических, лабораторных и натурных исследований медленной миграции деформаций. В перспективе концепция деформационных волн Земли может кардинально изменить существующие представления о сейсмическом процессе.

The theoretical prediction of strain waves in the Earth is one of the most significant achievements in geophysics of the last third of the 20th century. Using the strain wave theory, the physical foundations were developed for the mathematical theory of strain wave propagation, and the search for methods that could detect the strain waves in experiment and simulation has commenced. This article provides an overview of the history of the strain wave theory and describes the observation methods, the main types of geological structures generating strain waves, and the properties of strain waves. It presents the most important results of the theoretical, laboratory and field studies of slow migration of strain. Future studies based on the strain wave theory may initiate a fundamental revision of the current concepts of the seismic process.

миграция землетрясенийдеформационные волнылитосферауравнение sin-Гордонауединенные волнынеустойчивое скольжение

migration of earthquakesstrain waveslithospheresine-Gordon equationsolitary wavesunstable sliding

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The authors declare that there are no conflicts of interest present.