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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2022-13-2s-0626</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1451</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>СОВРЕМЕННАЯ ГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RECENT GEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>КОСЕЙСМИЧЕСКИЕ ЭФФЕКТЫ ХУБСУГУЛЬСКОГО ЗЕМЛЕТРЯСЕНИЯ В МОНГОЛИИ 11 ЯНВАРЯ 2021 г</article-title><trans-title-group xml:lang="en"><trans-title>COSEISMIC EFFECTS OF THE 11 JANUARY 2021 HOVSGOL, MONGOLIA, EARTHQUAKE</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лухнев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lukhnev</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p></bio><email xlink:type="simple">loukhnev@crust.irk.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лухнева</surname><given-names>О. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Lukhneva</surname><given-names>O. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Саньков</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Sankov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мирошниченко</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Miroshnichenko</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth's Crust, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>18</day><month>04</month><year>2022</year></pub-date><volume>13</volume><issue>2</issue><fpage>626</fpage><lpage>626</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лухнев А.В., Лухнева О.Ф., Саньков В.А., Мирошниченко А.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лухнев А.В., Лухнева О.Ф., Саньков В.А., Мирошниченко А.И.</copyright-holder><copyright-holder xml:lang="en">Lukhnev A.V., Lukhneva O.F., Sankov V.A., Miroshnichenko A.I.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://www.gt-crust.ru/jour/article/view/1451">https://www.gt-crust.ru/jour/article/view/1451</self-uri><abstract><p>Приведен пример обработки временных рядов GPS-наблюдений для оперативного исследования горизонтальных косейсмических смещений при Хубсугульском землетрясении в Монголии 11 января 2021 г. (М=6.7). Разработан методический подход для изучения косейсмических смещений в момент землетрясения. В работе представлены результаты определения значений горизонтальных косейсмических смещений, которые в зоне сочленения Хубсугульской и Тункинской впадин составляют 0.6 мм, а для районов Сибирского блока и Забайкалья – сотые доли миллиметра. Для станций, расположенных на южной окраине Сибирского блока, и станций Забайкалья, косейсмические смещения направлены на запад. Рассчитанные векторы смещений близлежащих к эпицентру станций (MNDY и BADG) направлены на юго-восток. </p></abstract><trans-abstract xml:lang="en"><p>The research provides an example of the GPS time series processing for monitoring of horizontal coseismic displacements during the 11 January 2021 M 6.7 Hovsgol earthquake, Mongolia. There has been developed a methodological approach to the study of coseismic displacements at the time of the earthquake. This paper presents the results of determining the values of horizontal coseismic displacements which are 0.6 mm in the junction zone between the Hovsgol and Tunka depressions and hundredths of a millimeter for the Siberian block and Transbaikalia areas. For stations located on the southern margin of the Siberian block and stations in Transbaikalia, the vectors of coseismic displacements are directed to the west. The calculated displacement vectors of the stations near the epicenter (MNDY and BADG) are directed to the southeast. </p></trans-abstract><kwd-group xml:lang="ru"><kwd>GPS</kwd><kwd>тектонические деформации</kwd><kwd>землетрясение</kwd><kwd>амплитуда</kwd><kwd>косейсмические смещения</kwd></kwd-group><kwd-group xml:lang="en"><kwd>GPS</kwd><kwd>tectonic deformations</kwd><kwd>earthquake</kwd><kwd>amplitude</kwd><kwd>coseismic displacements</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">В работе частично задействовалось оборудование ЦКП «Геодинамика и геохронология» Института земной коры СО РАН (грант № 075-15-2021-682) и ЦКП «Ангара» ИСЗФ СО РАН.</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Afraimovich E.L., Palamartchouk K.S., Perevalova N.P., Chernukhov V.V., Lukhnev A.V., Zalutsky V.T., 1998. 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