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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-2021-12-4-0562</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1373</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>МЕХАНИЗМЫ ОЧАГОВ ЗЕМЛЕТРЯСЕНИЙ ЮГА БАЙКАЛЬСКОГО РЕГИОНА И СЕВЕРНОЙ МОНГОЛИИ</article-title><trans-title-group xml:lang="en"><trans-title>FOCAL MECHANISMS OF EARTHQUAKES OF SOUTHERN BAIKAL REGION AND NORTHERN MONGOLIA</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>Радзиминович</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Radziminovich</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128, </p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия</p></bio><bio xml:lang="en"><p>Natalia A. Radziminovich</p><p>128 Lermontov St, Irkutsk 664033,</p><p>6а Sakhyanova St, Ulan-Ude 670047, Buryatian Republic</p></bio><email xlink:type="simple">nradzim@crust.irk.ru</email><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;&#13;
Бурятский филиал ФИЦ ЕГС 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;&#13;
Buryat Branch of the Federal Research Center of the Geophysical Survey, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>14</day><month>12</month><year>2021</year></pub-date><volume>12</volume><issue>4</issue><fpage>902</fpage><lpage>908</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Радзиминович Н.А., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Радзиминович Н.А.</copyright-holder><copyright-holder xml:lang="en">Radziminovich N.A.</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/1373">https://www.gt-crust.ru/jour/article/view/1373</self-uri><abstract><p>В статье представлены не опубликованные ранее решения механизмов очагов землетрясений для территории Южного Прибайкалья, Забайкалья, Тувы и Северной Монголии, определенные по знакам вступлений продольных волн на станциях Байкальской, Бурятской, Алтае-Саянской сетей Геофизической службы РАН и Монгольской национальной сети.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents previously unpublished earthquake focal mechanism solutions for earthquakes which occurred in South Pribaikalye, Transbaikalia, Tuva and Northern Mongolia derived from the first-motion polarities of P-waves recorded by the Baikal, Buryat, Altai-Sayan networks of the Geophysical Survey RAS and Mongolian national network.</p><p> </p></trans-abstract><kwd-group xml:lang="ru"><kwd>землетрясение</kwd><kwd>механизм очага</kwd><kwd>Забайкалье</kwd><kwd>Южное Прибайкалье</kwd><kwd>Тува</kwd><kwd>Монголия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>earthquake</kwd><kwd>focal mechanism</kwd><kwd>Transbaikalia</kwd><kwd>South Pribaikalye</kwd><kwd>Tuva</kwd><kwd>Mongolia</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при поддержке: 1. Минобрнауки РФ (в рамках государственного задания № 075-01304-20) и с использованием данных, полученных на уникальной научной установке «Сейсмоинфразвуковой комплекс мониторинга Арктической криолитозоны и комплекс непрерывного сейсмического мониторинга Российской Федерации, сопредельных территорий и мира». 2. РФФИ (проект 20-05-00357а). 3. В работе задействовалось оборудование УНУ «Южно-Байкальский инструментальный комплекс для мониторинга опасных геодинамических процессов», входящий в состав ЦКП «Геодинамика и геохронология» Института земной коры СО РАН в рамках гранта № 075-15-2021-682.</funding-statement><funding-statement xml:lang="en">The work was supported by Ministry of Education and Science of Russia. 1. The data used in the work were obtained with large-scale research facilities «Seismic infrasound array for monitoring Arctic cryolitozone and continuous seismic monitoring of the Russian Federation, adjacent territories and the world». 2. The research was supported by the Russian Foundation for Basic Research, project 20-05-00357a. 3. This work involved the South Baikal instrumental complex for monitoring hazardous geodynamic processes in frame of the Centre of Geodynamics and Geochronology at the Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences (grant 075-15-2021-682).</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">Arzhannikova A., Arzhannikov S., Jolivet M., Vassallo R., Chauvet A., 2011. Pliocene to Quaternary deformation in South East Sayan (Siberia): Initiation of the Tertiary Compressive Phase in the Southern Termination of the Baikal Rift System. 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