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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-2022-13-3-0633</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1537</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>ГЕОМЕТРИЯ ЗОНЫ СОВРЕМЕННЫХ РАЗРЫВОВ НА МЫСЕ РЫТОМ ПО ДАННЫМ ГЕОРАДИОЛОКАЦИИ (СЕВЕРО-ЗАПАДНОЕ ПОБЕРЕЖЬЕ ОЗ. БАЙКАЛ)</article-title><trans-title-group xml:lang="en"><trans-title>GEOMETRY OF RECENT RUPTURE ZONE AT СAPE RYTYI BASED ON GROUND PENETRATING RADAR (NORTHWESTERN COAST OF LAKE BAIKAL)</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>Лунина</surname><given-names>О. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lunina</surname><given-names>O. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p> 664033, Иркутск, ул. Лермонтова, 128, Россия </p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033, Russia </p></bio><email xlink:type="simple">lounina@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>Денисенко</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Denisenko</surname><given-names>I. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p> 664033, Иркутск, ул. Лермонтова, 128, Россия </p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033, Russia </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>Гладков</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Gladkov</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p> 664033, Иркутск, ул. Лермонтова, 128, Россия </p><p> 664043, г. Иркутск, ул. Сергеева, 5/6, Россия </p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033, Russia </p><p> 5-6 Sergeev St, Irkutsk 664043, Russia </p></bio><xref ref-type="aff" rid="aff-2"/></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><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт земной коры СО РАН;&#13;
ГАУ ДО ИО «Центр развития дополнительного образования детей», детский технопарк «Кванториум Байкал»</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;
Supplementary Education Center for Children, Ministry of Education of Irkutsk Region</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>21</day><month>09</month><year>2022</year></pub-date><volume>13</volume><issue>3</issue><fpage>633</fpage><lpage>633</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лунина О.В., Денисенко И.А., Гладков А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лунина О.В., Денисенко И.А., Гладков А.А.</copyright-holder><copyright-holder xml:lang="en">Lunina O.V., Denisenko I.A., Gladkov A.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/1537">https://www.gt-crust.ru/jour/article/view/1537</self-uri><abstract><p>Представлены результаты георадиолокационного изучения современной зоны разрывов, обнаруженной авторами ранее в периферийной части дельты р. Рита, впадающей в оз. Байкал. Работы проведены с целью прослеживания геометрии дислокаций на глубину при помощи георадара ОКО-2 в комплекте с антенным блоком АБДЛ Тритон. В результате вкрест простирания зоны разрывов охарактеризовано шесть профилей протяженностью от 73 до 197 м. Все разрывы, видимые на материалах аэрофотосъемки, выделяются на радарограммах по наклонной оси синфазности, которая образуется за счет понижения амплитуды сигнала. По простиранию зона нарушений разделяется на два крупных сегмента: северо-восточный и субмеридиональный. Первый от второго отличается большей шириной зоны, числом разрывов, более пологими углами их падения и меньшими амплитудами подвижек. Особенности деформирования могут быть обусловлены разным количеством пластичного суглинистого заполнителя грубообломочных отложений в разных частях дельты, что косвенно подтверждается более слабыми амплитудами сигналов на радарограммах северо-восточного сегмента. По результатам этих и предыдущих исследований высказано предположение о том, что землетрясение 13.08.1962 г. с M=5.2 в оз. Байкал могло запустить процесс гравитационного опускания на окраине дельты р. Рита, который на одном сегменте реализуется в основном путем оседания по пологим нарушениям, на другом – по крутым. Необходимо выявление и мониторинг подобных деформаций для предотвращения развития чрезвычайных ситуаций, связанных с обрушением побережий крупных водоемов.</p></abstract><trans-abstract xml:lang="en"><p>In here, we present the results of the GPR study of the modern rupture zone discovered earlier in the periphery of the Rita River delta flowing into Lake Baikal. The research was aimed at subsurface imaging of dislocation geometry using the Logis-Geotech OKO-2 radar equipped with the ABDL Triton antenna. As a result, the characterizations have been obtained for six 73 to 197 m long profiles across the rupture zone. All disturbances visible on the aerial photography materials are highlighted on the radargrams by the oblique reflection event due to a decrease in the signal amplitude. The rupture zone has two large segments – northeastern and submeridional, – which differ in zone width, number of discontinuities, dip angles, and displacement amounts. The deformation features can be attributed to different amounts of a plastic loamy aggregate of coarse deposits in different parts of the Rita River delta that is indirectly confirmed by weaker signal amplitudes on the northeastern segment. Based on present and previous studies, we proposed that the M=5.2 earthquake occurred on August 13, 1962, in Lake Baikal initiated the gravitational sinking in the Rita river delta edge by subsidence along gently sloped rupture surfaces on one segment and along steeply sloped ones on the other. It is necessary to identify and monitor such phenomena to prevent the development of emergencies associated with the collapse of the coasts of large water reservoirs.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>зона</kwd><kwd>разрыв</kwd><kwd>смещение</kwd><kwd>оседание</kwd><kwd>дельта</kwd><kwd>георадиолокация</kwd></kwd-group><kwd-group xml:lang="en"><kwd>zone</kwd><kwd>rupture</kwd><kwd>displacement</kwd><kwd>subsidence</kwd><kwd>delta</kwd><kwd>ground penetrating radar</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено за счет гранта Российского научного фонда № 22-27-00064 (https://rscf.ru/project/22-27-00064/).</funding-statement><funding-statement xml:lang="en">The study was funded by Russian Science Foundation grant 22-27-00064 (https://rscf.ru/project/22-27-00064/).</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">Барац Н.И. 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