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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-2022-13-1-0570</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1422</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>ДОЛГОВРЕМЕННЫЕ ИЗМЕНЕНИЯ ДВИЖЕНИЙ И ДЕФОРМАЦИЙ ЗЕМНОЙ КОРЫ ДО И ВО ВРЕМЯ СЕРИИ ЗЕМЛЕТРЯСЕНИЙ КУМАМОТО (2016 Г., ЯПОНИЯ)</article-title><trans-title-group xml:lang="en"><trans-title>LONG-TERM CHANGES IN CRUSTAL MOVEMENTS AND DEFORMATIONS BEFORE AND DURING THE 2016 KUMAMOTO EARTHQUAKE SEQUENCE</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>Кафтан</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Kaftan</surname><given-names>V. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119296, Москва, ул. Молодежная, 3</p></bio><bio xml:lang="en"><p>Vladimir I. Kaftan</p><p>3 Molodezhnaya St, Moscow 119296</p></bio><email xlink:type="simple">kaftan@geod.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>Татаринов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Tatarinov</surname><given-names>V. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119296, Москва, ул. Молодежная, 3</p></bio><bio xml:lang="en"><p>3 Molodezhnaya St, Moscow 119296</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>Шевчук</surname><given-names>Р. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Shevchuk</surname><given-names>R. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119296, Москва, ул. Молодежная, 3</p></bio><bio xml:lang="en"><p>3 Molodezhnaya St, Moscow 119296</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геофизический центр РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geophysical Center of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>22</day><month>03</month><year>2022</year></pub-date><volume>13</volume><issue>1</issue><fpage>570</fpage><lpage>570</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кафтан В.И., Татаринов В.Н., Шевчук Р.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Кафтан В.И., Татаринов В.Н., Шевчук Р.В.</copyright-holder><copyright-holder xml:lang="en">Kaftan V.I., Tatarinov V.N., Shevchuk R.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/1422">https://www.gt-crust.ru/jour/article/view/1422</self-uri><abstract><p>На острове Кюсю, как и на всем Японском архипелаге, функционирует густая перманентная сеть GPS (GEONET), которая позволяет отслеживать движения и деформации земной поверхности на многолетних временных интервалах. В настоящем исследовании по суточным определениям координат станций GPS анализируются долгопериодические тенденции накопления движений и деформаций на значительной территории о-ва Кюсю перед серией землетрясений Кумамото (14–16 апреля 2016 г.) с целью выявления деформационных предвестников и поиска неподвижных «запертых» зон разломов. Для изучения сейсмодеформационного процесса использованы данные непрерывных GPS-наблюдений 70 непрерывнодействующих станций за период 2009–2016 гг.</p><p>Выявленные особенности движений и деформаций характеризуют кинематику осевой зоны юго-западной части островной дуги Японского архипелага. Сочетание косейсмических сжатия и подъема в центре образованной триады экстремумов деформации и согласованность опусканий с растяжениями на ее краях демонстрируют механизм роста центральной области островной дуги в условиях сжатия и роль вулканизма. Наибольший интерес в отношении развития движений и деформаций в процессе подготовки землетрясений Кумамото представляет поведение минимальных модулей смещений пунктов глобальных навигационных спутниковых систем (ГНСС). Анализ их кинематики показывает образование области минимальных смещений, в которой были локализованы последующие сильные сейсмические события. Показано, что достаточно плотные и обширные сети ГНСС станций позволяют наблюдать и изучать сейсмодеформационный процесс на стадиях сейсмической подготовки, разрядки и релаксации, представляя тем самым эмпирическую основу для разработки моделей прогнозирования крупных и сильных сейсмических событий.</p></abstract><trans-abstract xml:lang="en"><p>The Kyushu Island, as well as whole Japanese archipelago, is equipped with dense GPS network (GEONET). It allows us to track the movements and deformations of the earth’s surface over long-term time intervals. In this study, based on daily determinations of the coordinates of GPS stations, analysis has been made on long-term trends in the accumulation of movements and deformations in large areas of the Kyushu Island before the series of April 14–16, 2016 Kumamoto earthquakes to identify deformation precursors and locked, immobile fault zones. The study of the seismic deformation process was performed using the data from 70 continuous permanent GPS stations for the period 2009–2016.</p><p>The movement and deformation features found characterize the kinematics of the axial zone of the southwestern part of the island arc of the Japanese archipelago. The combination of coseismic compression and uplift in the center of the formed triad of deformation extrema and the consistency between subsidence and extensions at its edges demonstrate the mechanism of growth of the central region of the island arc under compression and the role of volcanism. Of particular interest in the context of the development of movements and deformations during the generation of the Kumamoto earthquakes is the behavior of the minimum displacement moduli of the GNSS sites. Analysis of their kinematics shows the formation of a zone of minimum displacements, in which subsequent strong seismic events were localized. It is shown that rather dense and extensive GNSS networks allow observing and studying the seismic-deformation process at the stages of seismic generation, discharge and relaxation, thereby providing an empirical basis for the development of models for predicting large seismic events.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>деформация земной поверхности</kwd><kwd>GPS</kwd><kwd>запирание разлома</kwd><kwd>дефицит смещения</kwd><kwd>прогноз землетрясений</kwd></kwd-group><kwd-group xml:lang="en"><kwd>earth’s surface deformation</kwd><kwd>GPS</kwd><kwd>fault locking</kwd><kwd>slip deficit</kwd><kwd>earthquake prediction</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках государственного задания Геофизического центра РАН, утвержденного Минобрнауки РФ.</funding-statement><funding-statement xml:lang="en">This work was conducted in the framework of budgetary funding for the Geophysical Center of RAS, approved by the Ministry of Science and Higher Education of the Russian Federation.</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">Active Fault Database of Japan, 2021. 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