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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-2025-16-1-0811</article-id><article-id custom-type="edn" pub-id-type="custom">muebpv</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1987</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>УТОЧНЕНИЕ ХАРАКТЕРА ТИПОВЫХ ПРЕДВЕСТНИКОВЫХ АНОМАЛИЙ ДЛЯ РАЗНОГЛУБИННЫХ ЗЕМЛЕТРЯСЕНИЙ КУРИЛО-КАМЧАТСКОГО РЕГИОНА</article-title><trans-title-group xml:lang="en"><trans-title>CLARIFICATION OF THE NATURE OF TYPICAL PRECURSOR ANOMALIES FOR DIFFERENT-DEPTH EARTHQUAKES IN THE KURIL-KAMCHATKA REGION</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>Родкин</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Rodkin</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Москва, ул. Профсоюзная, 84/32; 693022, Южно-Сахалинск, ул. Науки, 1Б</p></bio><bio xml:lang="en"><p>84-32 Profsoyuznaya St, Moscow 117997; 1B Nauki St, Yuzhno-Sakhalinsk 693022</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>Андреева</surname><given-names>М. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Andreeva</surname><given-names>M. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>693022, Южно-Сахалинск, ул. Науки, 1Б</p></bio><bio xml:lang="en"><p>1B Nauki St, Yuzhno-Sakhalinsk 693022</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт теории прогноза землетрясений и математической геофизики РАН; &#13;
Институт морской геологии и геофизики ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Earthquake Prediction Theory and Mathematical Geophysics, Russian Academy of Sciences; &#13;
Institute of Marine Geology and Geophysics, Far Eastern 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 морской геологии и геофизики ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Marine Geology and Geophysics, Far Eastern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>19</day><month>02</month><year>2025</year></pub-date><volume>16</volume><issue>1</issue><fpage>811</fpage><lpage>811</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Родкин М.В., Андреева М.Ю., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Родкин М.В., Андреева М.Ю.</copyright-holder><copyright-holder xml:lang="en">Rodkin M.V., Andreeva M.Y.</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/1987">https://www.gt-crust.ru/jour/article/view/1987</self-uri><abstract><p>Ставится задача исследования возможности построения нового алгоритма прогноза землетрясений на основе набора предвестниковых эффектов, ранее надежно выявленных по мировым данным в результате построения обобщенной окрестности сильного землетрясения, сформированной масштабированным объединением данных по большому числу фор- и афтершоковых областей отдельных сильных землетрясений. Применительно к региону Камчатка – Северные Курилы решение этой задачи на первом этапе предусматривает уточнение регионального характера осредненных предвестниковых эффектов на основе наиболее полного и однородного регионального каталога. Отмечено более позднее начало аномалий изменения интенсивности потока событий и наклона графика повторяемости для среднеглубоких землетрясений. Для глубоких землетрясений доминирует тенденция не уменьшения, а увеличения глубины слабых событий в окрестности сильных. Уточненные особенности осредненного предвестникового поведения будут использованы как типовые паттерны для прогноза разноглубинных землетрясений Курило-Камчатского региона.</p></abstract><trans-abstract xml:lang="en"><p>The task was set on investigation of the possibility of constructing a new algorithm for earthquake prediction based on a set of precursor effects that had been reliably identified from the world data as a result of constructing the generalized vicinity of a strong earthquake from a scaled combination of the data on a large number of foreshock and aftershock areas of individual strong earthquakes. In relation to the Kamchatka-Northern Kurils region, the first-stage solution of this task lies in clarification of the regional character of the averaged precursor effects on the basis of the most complete and homogeneous regional catalogue. There has been a later onset of anomalous changes in the intensity of flow of events and in the slope of the recurrence diagram for intermediate-depth earthquakes. The deep-seated earthquakes show a dominant trend of increased rather than decreased depth of weak events in the vicinity of strong events. The specified features of the averaged precursor behavior will be used as typical patterns to predict different-depth earthquakes in the Kuril-Kamchatka region.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>афтершоковые и форшоковые аномалии</kwd><kwd>прогноз землетрясений</kwd><kwd>физика сейсмического разрушения</kwd></kwd-group><kwd-group xml:lang="en"><kwd>aftershock and foreshock anomalies</kwd><kwd>earthquake prediction</kwd><kwd>physics of earthquake faulting</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена по программе госзадания ИМГиГ ДВО РАН и при поддержке РНФ (проект № 23-27-00395 «Комплекс аномалий в обобщенной окрестности сильного землетрясения; физика процесса и использование в целях прогноза»).</funding-statement><funding-statement xml:lang="en">The work was carried out as part of the state assignment of the IMGG FEB RAS and with the support of the Russian Science Foundation (project 23-27-00395 "Complex anomalies in the generalized vicinity of a strong earthquake; physics of the process and use for forecasting purposes").</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">Aki K., 1965. 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