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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-2024-15-1-0744</article-id><article-id custom-type="edn" pub-id-type="custom">VCLECE</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1796</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>СООТНОШЕНИЕ РАДОНОВОЙ И СЕЙСМИЧЕСКОЙ АКТИВНОСТИ В БАЙКАЛЬСКОЙ РИФТОВОЙ ЗОНЕ ПО ДАННЫМ ЭМАНАЦИОННОГО МОНИТОРИНГА</article-title><trans-title-group xml:lang="en"><trans-title>CORRELATION OF RADON AND SEISMIC ACTIVITY IN THE BAIKAL RIFT ZONE ACCORDING TO EMANATION MONITORING DATA</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7607-0417</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Семинский</surname><given-names>К. Ж.</given-names></name><name name-style="western" xml:lang="en"><surname>Seminsky</surname><given-names>K. Zh.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-4405-6132</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Бобров</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bobrov</surname><given-names>А. А.</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>2024</year></pub-date><pub-date pub-type="epub"><day>16</day><month>02</month><year>2024</year></pub-date><volume>15</volume><issue>1</issue><fpage>744</fpage><lpage>744</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Семинский К.Ж., Бобров А.А., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Семинский К.Ж., Бобров А.А.</copyright-holder><copyright-holder xml:lang="en">Seminsky K.Z., Bobrov А.А.</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/1796">https://www.gt-crust.ru/jour/article/view/1796</self-uri><abstract><p>Длинные ряды эманационного мониторинга, организованного на станциях «Тырган» (2018–2023 гг.), «Бугульдейка» (2020–2023 гг.) и «Максимиха» (2022–2023 гг.) в центральной части Прибайкалья (Восточная Сибирь), изучены с целью выявления связи объемной активности подпочвенного радона (ОАР) с сейсмичностью Байкальской рифтовой зоны (БРЗ). Сопоставление осредненных за неделю значений ОАР на разных станциях и степени зависимости данного параметра от логарифма суммарной энергии землетрясений (LgΣE) показало, что в периоды сейсмических активизаций воздействие тектонических сил вносит значимые коррективы в характер эманаций, который в целом определяется нетектоническими факторами. Установлено, что сейсмическим активизациям, представленным достаточно сильными для Прибайкалья землетрясениями с К≥13.3, соответствуют интервалы нарушения синхронности вариаций ОАР на разных станциях мониторинга, а также совпадение максимальных величин логарифма суммарной энергии землетрясений с локальными максимумами коэффициента корреляции связи между параметрами ОАР и LgΣE. Область, включающая эпицентры землетрясений, генерировавших подобный эманационный отклик на станциях мониторинга, имеет форму эллипса, вытянутого в северо-восточном направлении – вдоль главных разломных структур БРЗ. Полученные результаты, кроме подтверждения предложенной ранее модели формирования поля радона в Прибайкалье под воздействием внешних и внутренних сил, представляют основу для выявления в дальнейшем устойчивых предвестников сильных землетрясений на базе комплексного анализа данных разветвленной сети эманационного мониторинга.</p></abstract><trans-abstract xml:lang="en"><p>Long series of the emanation monitoring organized at Tyrgan (2018–2023), Buguldeika (2020–2023) and Maksimikha (2022–2023) stations in the central part of the Baikal Region (the Eastern Siberia) are studied to reveal the relationship of the subsurface radon volumetric activity (RVA) with the seismicity of the Baikal rift zone (BRZ). The comparison of the weekly averaged RVA values at different stations and the degree of dependence of this parameter on the logarithm of the total earthquakes energy (LgΣE) showed that during the periods of seismic activity the impact of tectonic forces makes significant corrections in the character of emanations, which in general is determined by non-tectonic factors. It has been established that seismic activity represented by the enough strong for the Baikal Region earthquakes with K≥13.3 correspond to synchronicity intervals of RVA at different monitoring stations, as well as coincidence of maximum values of the logarithm of the total earthquakes energy with local maximums of the correlation coefficient between RVA and LgΣE parameters. The area, including the earthquake epicenters that generated such an emanation response at monitoring stations, is in the form of an ellipse extended in the northeastern direction – along the main fault structures of the BRZ. The obtained results, besides confirming the previously proposed model of radon field formation in the Baikal Region under the influence of external and internal forces, provide the for the identification of further stable precursors of strong earthquakes based on a comprehensive analysis of data from a branched emanation monitoring network.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>радон</kwd><kwd>землетрясения</kwd><kwd>мониторинг</kwd><kwd>Байкальский рифт</kwd></kwd-group><kwd-group xml:lang="en"><kwd>radon</kwd><kwd>earthquakes</kwd><kwd>monitoring</kwd><kwd>Baikal rift</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работы выполнены в рамках госзадания ИЗК СО РАН на 2021–2025 гг. «Современная геодинамика, механизмы деструкции литосферы и опасные геологические процессы в Центральной Азии» с использованием оборудования и инфраструктуры Уникальной научной установки «Южно-Байкальский инструментальный комплекс для мониторинга опасных геодинамических процессов» ЦКП «Геодинамика и геохронология » ИЗК СО РАН по гранту 075-15-2021-682.</funding-statement><funding-statement xml:lang="en">The work was carried out as a part of the state assignment of IEC SB RAS for 2021–2025. "Modern geodynamics, mechanisms of lithosphere destruction and dangerous geological processes in Central Asia" using the Large-Scale Research Facilities "South-Baikal instrumental complex for monitoring of hazardous geodynamic processes" of the Centre for Geodynamics and Geochronology at the IEC SB RAS (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">Адушкин В.В., Спивак А.А., Рыбнов Ю.С., Харламов В.А. Приливные волны и вариации давления в атмосфере Земли // Геофизические исследования. 2017. Т. 18. № 3. С. 67–80. https://doi.org/10.21455/gr2017.3-6.</mixed-citation><mixed-citation xml:lang="en">Adushkin V.V., Spivak A.A., Rybnov Yu.S., Kharlamov V.A., 2017. Tidal Waves and Pressure Variations in the Earth’s Atmosphere. 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