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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">geology</journal-id><journal-title-group><journal-title xml:lang="ru">Известия высших учебных заведений. Геология и разведка</journal-title><trans-title-group xml:lang="en"><trans-title>Proceedings of higher educational establishments. Geology and Exploration</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0016-7762</issn><issn pub-type="epub">2618-8708</issn><publisher><publisher-name>Sergo Ordzhonikidze Russian State University for Geological Prospecting</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.32454/0016-7762-2023-65-3-28-41</article-id><article-id custom-type="elpub" pub-id-type="custom">geology-918</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>ГЕОЭКОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOECOLOGY</subject></subj-group></article-categories><title-group><article-title>Землетрясения в Турции и Сирии 2023 года и геодинамика Кавказско-Анатолийского региона</article-title><trans-title-group xml:lang="en"><trans-title>Earthquakes in Turkey and Syria in 2023 and geodynamics of the Caucasus-Anatolian region</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5597-2438</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Свалова</surname><given-names>В. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Svalova</surname><given-names>V. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Валентина Борисовна Свалова, кандидат физико-математических наук, в. н. с.</p><p>101000</p><p>13, Уланский переулок, стр. 2</p><p>362002</p><p>93а, ул. Маркова</p><p>Москва</p><p>Владикавказ</p><p>тел.: +7 (916) 206-41-47</p></bio><bio xml:lang="en"><p>Valentina B. Svalova, Cand. of Sci. (Phys. and Math.), Leading scientist</p><p>101000</p><p>13, bld. 2 Ulansky lane</p><p>362002</p><p>93a, Markova str.</p><p>Moscow</p><p>Vladikavkaz</p><p>tel.: +7 (916) 206-41-47</p></bio><email xlink:type="simple">v-svalova@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФГБУН «Институт геоэкологии им. Е. М. Сергеева Российской академии наук»; Геофизический институт Владикавказского научного центра Российской академии наук</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences; Geophysical Institute, Vladikavkaz Scientific Center, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>01</day><month>09</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>28</fpage><lpage>41</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Свалова В.Б., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Свалова В.Б.</copyright-holder><copyright-holder xml:lang="en">Svalova V.B.</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.geology-mgri.ru/jour/article/view/918">https://www.geology-mgri.ru/jour/article/view/918</self-uri><abstract><sec><title>   Введение</title><p>   Введение. Активизация природных катаклизмов в мире требует разработки новых подходов к изучению геологических процессов, в частности, на границах литосферных плит, характеризующихся землетрясениями, повышенной сейсмичностью, вулканизмом, повышенным тепловым потоком, геотермическими проявлениями, оползневыми процессами, цунами и другими опасными природными процессами и явлениями. Кавказско-Анатолийско-Аравийский регион представляет собой сложную высоконапряженную геодинамическую структуру, характеризующуюся повышенным тепловым потоком, высокой сейсмичностью, магматизмом и вулканизмом. Геодинамика Кавказско-Анатолийско-Аравийского региона определяется столкновением Евразийской и Аравийской литосферных плит, а также сложной историей развития Альпийско-Гималайского пояса и прилегающих территорий. Землетрясение магнитудой 7,8 произошло на юго-востоке Турции и северо-западе Сирии 6 февраля 2023 года. Землетрясение магнитудой 7,8 является крупнейшим в Турции после землетрясения в Эрзинджане 1939 года и вторым по силе в стране после землетрясения в Северной Анатолии 1668 года. Подтверждено более 52 800 смертей: более 46 100 в Турции и более 6700 в Сирии. Это самое смертоносное стихийное бедствие в современной истории Турции. Землетрясения нанесли ущерб на сумму более 100 миллиардов долларов США.</p></sec><sec><title>   Цель</title><p>   Цель. Основная цель работы — построение геодинамических моделей глубинного строения районов стихийных бедствий, что является важным вкладом в изучение активных континентальных окраин и необходимо для предсказания и прогнозирования землетрясений, оценки геоэкологических рисков и подготовки действий населения в случае стихийных бедствий и катастроф.</p></sec><sec><title>   Материалы и методы</title><p>   Материалы и методы. Решение задач формирования и эволюции геологических структур в различных сложных геодинамических обстановках, а также прогноза и предсказания природных опасностей требует анализа всех имеющихся геолого-геофизических данных, а такжепостановки и решения задач механического и математического моделирования.</p></sec><sec><title>   Результаты</title><p>   Результаты. Построены геодинамические модели районов опасных природных процессов с целью прогнозирования и предотвращения стихийных бедствий и катастроф. Предложен алгоритм создания систем мониторинга.</p></sec><sec><title>   Заключение</title><p>   Заключение. Землетрясение под Стамбулом можно ждать через несколько лет (1—10 лет). Можно прогнозировать, что если сильное землетрясение в Восточно-Анатолийском разломе не произойдет через 1—2 года, то случится только через 100 лет.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>   Background</title><p>   Background. The intensification of natural disasters all over the world requires the development of new approaches to the study of geological processes. This particularly concerns the areas at the boundaries of lithospheric plates, which are characterized by earthquakes, increased seismicity, volcanism, intensive heat flows, geothermal manifestations, landslide processes, tsunamis, and other dangerous natural processes and hazards. The Caucasus-Anatolian-Arabian region is a complex highly-stressed geodynamic structure, characterized by an increased heat flow, seismicity, magmatism, and volcanism. The geodynamics of this region is determined by the collision of the Eurasian and Arabian lithosphere plates, as well as by the evolution of the Alpine-Himalayan belt and surrounding areas. A 7.8 magnitude earthquake hit the South-East Turkey and North-West Syria on February 6, 2023. This was the largest earthquake in Turkey since the 1939 Erzincan earthquake, and the second-strongest since the 1668 North Anatolia earthquake. More than 52,800 deaths were confirmed, with about 46,100 in Turkey and 6,700 in Syria. It is the deadliest natural disaster in Turkey’s modern history with the estimated damage of over $100 billion.</p></sec><sec><title>   Aim</title><p>   Aim. To construct geodynamic models for the deep structure of natural hazard regions, which can contribute to the study of active continental margins. This information is necessary for earthquake forecasting and prognosis, as well as for assessing geoecological risks and preparing the population in the event of natural disasters and catastrophes.</p></sec><sec><title>   Materials and methods</title><p>   Materials and methods. The formation and evolution processes of geological structures in complex geodynamic settings, as well as the forecasting and prognosis of natural hazards, required an analysis of all available geological and geophysical data. The methods of mechanical and mathematical modeling were used to formulate and solve the research problems.</p></sec><sec><title>   Results</title><p>   Results. Geodynamic models of the regions of hazardous natural processes were constructed with the purpose of forecasting and preventing natural disasters and catastrophes. An algorithm for creating monitoring systems was proposed.</p></sec><sec><title>   Conclusion</title><p>   Conclusion. In several years (1–10 years), another earthquake near Istanbul can be expected. In the case that no large earthquake occurs in the East Anatolian fault in 1–2 years, this event is likely to occur in 100 years only.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>геотермия</kwd><kwd>сейсмичность</kwd><kwd>геодинамика</kwd><kwd>Кавказ</kwd><kwd>Турция</kwd><kwd>моделирование</kwd><kwd>сейсмотомография</kwd></kwd-group><kwd-group xml:lang="en"><kwd>geothermy</kwd><kwd>seismicity</kwd><kwd>geodynamics</kwd><kwd>Caucasus</kwd><kwd>Turkey</kwd><kwd>modeling</kwd><kwd>seismotomography</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Статья подготовлена в раках выполнения госзадания № 122022400105-9 по теме «Прогноз, моделирование и мониторинг эндогенных и экзогенных геологических процессов для снижения уровня их негативных последствий»</funding-statement><funding-statement xml:lang="en">The article was prepared in response to a government assignment No. 122022400105-9 on the topic “Forecast, modeling and monitoring of endogenous and exo genous geological processesto reduce their negative consequences”</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">Гончаров М.А., Короновский Н.В., Разницин Ю.Н. 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