ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA

The study is focused on earthquake migrations along active faults in seismic zones of Mongolia. The earthquake migrations are interpreted as a result of the influence of deformational waves. Vector velocities and other parameters of the deformational waves are studied. Based on data from largescale...

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Main Author: M. G. Mel’nikov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Series:Геодинамика и тектонофизика
Subjects:
Online Access:https://www.gt-crust.ru/jour/article/view/23
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author M. G. Mel’nikov
author_facet M. G. Mel’nikov
author_sort M. G. Mel’nikov
collection DOAJ
description The study is focused on earthquake migrations along active faults in seismic zones of Mongolia. The earthquake migrations are interpreted as a result of the influence of deformational waves. Vector velocities and other parameters of the deformational waves are studied. Based on data from largescale maps, local faults are compared, and differences and similarities of parameters of waves related to faults of different ranks are described.
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institution Kabale University
issn 2078-502X
language English
publishDate 2015-09-01
publisher Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
record_format Article
series Геодинамика и тектонофизика
spelling doaj-art-403129c4ccf241459f60f21bee26ca392025-08-20T03:37:07ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2015-09-0141698110.5800/GT-2013-4-1-009223ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIAM. G. Mel’nikov0Institute of the Earth’s Crust, SB RAS, Irkutsk, RussiaThe study is focused on earthquake migrations along active faults in seismic zones of Mongolia. The earthquake migrations are interpreted as a result of the influence of deformational waves. Vector velocities and other parameters of the deformational waves are studied. Based on data from largescale maps, local faults are compared, and differences and similarities of parameters of waves related to faults of different ranks are described.https://www.gt-crust.ru/jour/article/view/23deformational wavesearthquakeseismic zoneactive faultsmongolia
spellingShingle M. G. Mel’nikov
ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
Геодинамика и тектонофизика
deformational waves
earthquake
seismic zone
active faults
mongolia
title ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
title_full ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
title_fullStr ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
title_full_unstemmed ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
title_short ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
title_sort about the wave mechanism of activation of faults in seismic zones of the lithosphere in mongolia
topic deformational waves
earthquake
seismic zone
active faults
mongolia
url https://www.gt-crust.ru/jour/article/view/23
work_keys_str_mv AT mgmelnikov aboutthewavemechanismofactivationoffaultsinseismiczonesofthelithosphereinmongolia