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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-2021-12-3s-0554</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1263</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>НЕКОТОРЫЕ ОСОБЕННОСТИ СОВРЕМЕННЫХ ТЕХНОГЕННЫХ ДВИЖЕНИЙ ЗЕМНОЙ КОРЫ</article-title><trans-title-group xml:lang="en"><trans-title>SOME FEATURES OF CURRENT TECHNOGENIC MOVEMENTS OF THE EARTH’S CRUST</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>Тимофеев</surname><given-names>В. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Timofeev</surname><given-names>V. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>Vladimir Yu. Timofeev</p><p>3 Academician Koptyug Ave, Novosibirsk 630090</p></bio><email xlink:type="simple">timofeevvy@ipgg.sbras.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>Ардюков</surname><given-names>Д. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Ardyukov</surname><given-names>D. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</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>Тимофеев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Timofeev</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</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>Бойко</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Boyko</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</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>Валитов</surname><given-names>М. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Valitov</surname><given-names>M. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>690041, Владивосток, ул. Балтийская, 43</p></bio><bio xml:lang="en"><p>43 Baltiyskaya St, Vladivostok 690041</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>Калиш</surname><given-names>Е. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Kalish</surname><given-names>E. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 1</p></bio><bio xml:lang="en"><p>1 Academician Koptyug Ave, Novosibirsk 630090</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>Стусь</surname><given-names>Ю. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Stus</surname><given-names>Yu. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 1</p></bio><bio xml:lang="en"><p>1 Academician Koptyug Ave, Novosibirsk 630090</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>Носов</surname><given-names>Д. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Nosov</surname><given-names>D. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 1</p></bio><bio xml:lang="en"><p>1 Academician Koptyug Ave, Novosibirsk 630090</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>Сизиков</surname><given-names>И. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Sizikov</surname><given-names>I. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Trofimuk Institute of Petroleum Geology and Geophysics, 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>Тихоокеанский океанологический институт им. В.И. Ильичева ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт автоматики и электрометрии СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Automation and Electrometry, Siberian Branch of the 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>19</day><month>10</month><year>2021</year></pub-date><volume>12</volume><issue>3S</issue><fpage>776</fpage><lpage>791</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Тимофеев В.Ю., Ардюков Д.Г., Тимофеев А.В., Бойко Е.В., Валитов М.Г., Калиш Е.Н., Стусь Ю.Ф., Носов Д.А., Сизиков И.С., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Тимофеев В.Ю., Ардюков Д.Г., Тимофеев А.В., Бойко Е.В., Валитов М.Г., Калиш Е.Н., Стусь Ю.Ф., Носов Д.А., Сизиков И.С.</copyright-holder><copyright-holder xml:lang="en">Timofeev V.Y., Ardyukov D.G., Timofeev A.V., Boyko E.V., Valitov M.G., Kalish E.N., Stus Y.F., Nosov D.A., Sizikov I.S.</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/1263">https://www.gt-crust.ru/jour/article/view/1263</self-uri><abstract><p>В работе рассматриваются зарегистрированные авторами техногенные эффекты, связанные с эксплуатацией крупных водохранилищ и месторождений полезных ископаемых в Сибири. Рассмотрена история измерений смещений и деформаций и связанных с ними явлений с помощью различных методов. Начало таких исследований связано с классическими методами – нивелированием и высокоточной наклонометрией. В настоящее время мониторинг современных процессов выполняется методами космической геодезии и абсолютной гравиметрии, что позволяет как получать кинематические характеристики (скорость опускания или подъема, скорость и величину горизонтального смещения поверхности), так и отслеживать движение флюида в земной коре, а это дает возможность регулировать процесс добычи полезных ископаемых. Анализируются современные техногенные явления в районе Усть-Балыкского и Заполярного нефтегазовых месторождений Западной Сибири, в зоне водохранилища Саяно-Шушенской гидроэлектростанции (СШГЭС) и шахт Кузбасса. Представлены полученные скорости движений земной коры в зонах эксплуатации крупных техногенных объектов в отдельные эпохи измерений. По нашим наблюдениям, для гидротехнических сооружений они достигают 5 мм/год. В зоне эксплуатации нефтегазовых месторождений на севере Западной Сибири в начале 2000-х гг. скорость опускания составила 20–25 мм/год, что подтверждается высокоточными абсолютными измерениями силы тяжести, показывающими увеличение значения на 6–7 микрогал/год. Обсуждается возможность триггерного эффекта для возникновения слабой сейсмичности, связанного с высокой скоростью накопления напряжений (1 КПа/час) в зоне водохранилища СШГЭС, расположенной в Западно-Саянском регионе. В работе проанализирована связь земного прилива и техногенных событий. Результаты наблюдений, выполненных в сентябре 2017 г., свидетельствуют о том, что подземные ядерные взрывы в КНДР не приводят к значимым смещениям земной поверхности на юге Приморья.</p></abstract><trans-abstract xml:lang="en"><p>We describe the history of studying the current crustal movements by various methods and discuss technogenic effects recorded at large water-reservoir zones and mineral deposits in Siberia. Initially, classical surveying techniques aimed to obtain high-accuracy ground-based measurements of height, tilt and direction. Modern geodesy techniques and methods for measuring absolute gravity are now available to investigate displacement, deformation, tilt and other phenomena taking place on the Earth’s surface. These methods are used to estimate kinematic parameters of the crust areas (e.g. rates of subsidence and horizontal movements) and to monitor fluid motions in mineral deposits. Such data are critical for ensuring a proper management of the mineral deposits. In this article, we analyse technogenic processes observed in the Ust Balyk oil-gas field, the Zapolyarny gas deposit, the water-reservoir zone at the Sayano-Shushenskaya hydroelectric power station (SSHPS) on the Yenisei river, and large open-pit mines in the Kuzbass basin. Our analysis is based on surface displacement rates estimated from the data collected in different periods of observations at large man-made facilities. In the study of the hydro technical objects, we estimated the displacement rates at 5.0 mm per year. In the northern areas of the West Siberian petroleum basin, subsidence rates amounted to 20–25 mm per year in the early 2000s. These estimates were supported by the high-accuracy gravity measurements showing an increase up to 6–7 microGal per year in the oil-gas field development areas. We assess a possibility of triggering effects related to weak seismicity due to a high stress accumulation rate (1 KPa per hour) in the SSHPS area. A connection between earth tides and catastrophic events, such as gas emissions in high amounts on mining sites, is discussed. Having analysed the surface monitoring records taken in South Primorye in September 2017, we conclude that underground nuclear explosions in North Korea in this period did not cause any significant displacement of the surface in this most southerly region of the Russian Far East territories.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>смещения и наклоны земной поверхности</kwd><kwd>нивелирование</kwd><kwd>космическая геодезия</kwd><kwd>гравиметрия</kwd><kwd>техногенная нагрузка</kwd><kwd>опускание земной поверхности</kwd><kwd>скорость накопления напряжений</kwd><kwd>землетрясение</kwd><kwd>триггерный эффект</kwd></kwd-group><kwd-group xml:lang="en"><kwd>displacement and tilt of the earth’s surface</kwd><kwd>leveling</kwd><kwd>space geodesy</kwd><kwd>gravimetry</kwd><kwd>technogenic load</kwd><kwd>surface subsidence</kwd><kwd>stress accumulation rate</kwd><kwd>earthquake</kwd><kwd>trigger effect</kwd></kwd-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., Турунтаев С.Б. 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