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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-2022-13-2-0588</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1489</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>Статьи</subject></subj-group></article-categories><title-group><article-title>НОВЫЙ ПОДХОД К ПРОГНОЗУ СИЛЬНЫХ ЗЕМЛЕТРЯСЕНИЙ В ЮЖНО-БАЙКАЛЬСКОМ РЕГИОНЕ НА ОСНОВЕ ДАННЫХ МОНИТОРИНГА ДЕФОРМАЦИИ ГОРНЫХ ПОРОД: МЕТОДОЛОГИЯ И РЕЗУЛЬТАТЫ</article-title><trans-title-group xml:lang="en"><trans-title>NEW APPROACH TO STRONG EARTHQUAKE PREDICTION IN THE SOUTH BAIKAL REGION ON THE BASIS OF ROCK DEFORMATION MONITORING DATA: METHODOLOGY AND RESULTS</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>Борняков</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bornyakov</surname><given-names>S. 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 contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Встовский</surname><given-names>Г. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Vstovsky</surname><given-names>G. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Москва, ул. Архитектора Власова, 49</p></bio><bio xml:lang="en"><p>49 Architect Vlasov St, Moscow, 117997</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Синцов</surname><given-names>А. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Sintsov</surname><given-names>A. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>109147 Москва, ул. Таганская, 34А</p></bio><bio xml:lang="en"><p>34А Taganskaya St, Moscow, 109147</p></bio><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Салко</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Salko</surname><given-names>D. 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><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><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ЗАО «ЦНИИПСК им. Мельникова»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>CJSC Melnikov Central Research and Design Institute of Construction Metal Structures</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>АО ВО «Безопасность»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>JSC Foreign Trade Organization "Security"</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>14</day><month>06</month><year>2022</year></pub-date><volume>13</volume><issue>2</issue><fpage>588</fpage><lpage>588</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Борняков С.А., Мирошниченко А.И., Встовский Г.В., Синцов А.Е., Салко Д.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Борняков С.А., Мирошниченко А.И., Встовский Г.В., Синцов А.Е., Салко Д.В.</copyright-holder><copyright-holder xml:lang="en">Bornyakov S.A., Miroshnichenko A.I., Vstovsky G.V., Sintsov A.E., Salko D.V.</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/1489">https://www.gt-crust.ru/jour/article/view/1489</self-uri><abstract><p>Южное Прибайкалье (ЮП) находится в пределах активно развивающейся Байкальской рифтовой зоны (БРЗ), обладающей значительным сейсмическим потенциалом. Здесь периодически происходят землетрясения с магнитудой более 7 и с интенсивностью сотрясений в эпицентрах до 10 баллов. В условиях высокой степени урбанизации ЮП и активного развития в его пределах промышленных кластеров и транспортных систем существенно повышается актуальность проблемы прогноза сильных землетрясений. В ИЗК СО РАН для решения этой проблемы проводится комплекс исследований по разным направлениям. Одно из них связано с инструментальным изучением современных движений литосферы на больших базах посредством GPS-геодезии и деформаций горных пород на малых базах штанговыми тензометрическими датчиками. Существующе пункты GPS и деформационных измерений объединены в уникальную научную установку «Южно-Байкальский инструментальный комплекс для мониторинга опасных геодинамических процессов» (УНУ «ЮБИК»), входящую в состав ЦКП «Геодинамика и геохронология».</p><p>В статье рассмотрены методические вопросы деформационного мониторинга на малых базах. Описаны его концептуальная основа, техническая база и методы обработки получаемого фактического материла. На примере произошедших в последнее время в ЮП трех сильных землетрясений – Култукского (27.08.2008 г.), Быстринского (21.09.2020 г.) и Кударинского (10.12.2020 г.) – показаны предшествующие им особенности развития деформаций горных пород, а также влияние на них структурно-геодинамических условий в местах расположения пунктов мониторинга и пространственного положения этих пунктов относительно готовящегося очага землетрясения.</p></abstract><trans-abstract xml:lang="en"><p>The Southern Baikal is located within the actively developing Baikal rift zone (BRZ) that is characterized by a significant seismic potential, and M&gt;7 earthquakes occur periodically with intensive shaking in the epicenters (up to 10 units). The problem of prediction and forecasting of strong earthquakes has always been critical for this region, considering its increasing urbanization, industrial clusters and transport systems. The article describes the methodology based on rock deformation monitoring data, which aims at developing a technology capable of efficient prediction and forecasting of strong earthquakes. In the Institute of Earth’s Crust SB RAS a set of studies is carried out in order to solve this problem, including those associated with the instrumental study of current movements of the lithosphere through GPS geodesy and deformations of rocks by strain gauges. The existing GPS sites and deformation measurements are combined into the Large-Scale Research Facilities "South Baikal instrumental complex for monitoring hazardous geodynamic processes" in frame of the Shared Research Facilities "Geodynamics and Geochronology" at the Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Science.</p><p>In this article, the deformation monitoring methodology is described in application to the monitoring sites installed in the study area. The description includes the details of its conceptual basis, technical support and data processing methods. The discussion focuses on the instrumental measurements of rock deformation related to three strong events in the study area – Kultuk (August 27, 2008), Bystrinskoe (September 21, 2020), and Kudara (December 10, 2020) earthquakes. The features of the deformation process before these seismic events are given special attention with account of the structural-geodynamic settings and positions of local monitoring sites relative to the earthquake epicenters.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>мониторинг деформаций горных пород</kwd><kwd>землетрясение</kwd><kwd>предвестник</kwd><kwd>прогноз</kwd></kwd-group><kwd-group xml:lang="en"><kwd>rock deformation monitoring</kwd><kwd>earthquake</kwd><kwd>precursor</kwd><kwd>prediction</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при финансовой поддержке РФФИ (проект № 21-55-53019) с использованием УНУ «Южно-Байкальский инструментальный комплекс для мониторинга опасных геодинамических процессов», входящей в состав ЦКП «Геодинамика и геохронология» Института земной коры СО РАН.</funding-statement><funding-statement xml:lang="en">rock deformation monitoring; earthquake; precursor; prediction</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">Bak P., Tang C., 1989. 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