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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-2026-17-3-0891</article-id><article-id custom-type="edn" pub-id-type="custom">AVLTGX</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-2291</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>МОЩНОСТЬ ЗЕМНОЙ КОРЫ БАЙКАЛЬСКОГО РЕГИОНА И МОНГОЛИИ НА ОСНОВЕ ИНТЕРПРЕТАЦИИ СПУТНИКОВОЙ МОДЕЛИ ГРАВИТАЦИОННОГО ПОЛЯ</article-title><trans-title-group xml:lang="en"><trans-title>CRUSTAL THICKNESS IN THE BAIKAL REGION AND MONGOLIA BASED ON INTERPRETATION OF THE SATELLITE GRAVITY MODEL</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-6029-7801</contrib-id><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>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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-3089-7114</contrib-id><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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-7664-7244</contrib-id><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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2678-7636</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Голдобин</surname><given-names>Д. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Goldobin</surname><given-names>D. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630108, Новосибирск, ул. Плахотного, 10 </p></bio><bio xml:lang="en"><p>10 Plakhotny St, Novosibirsk 630108 </p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5442-5969</contrib-id><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-3"/></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>Сибирский государственный университет геосистем и технологий</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Siberian State University Geosystems and Technology</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><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><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>18</day><month>06</month><year>2026</year></pub-date><volume>17</volume><issue>3</issue><fpage>891</fpage><lpage>891</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Тимофеев В.Ю., Ардюков Д.Г., Тимофеев А.В., Голдобин Д.Н., Валитов М.Г., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Тимофеев В.Ю., Ардюков Д.Г., Тимофеев А.В., Голдобин Д.Н., Валитов М.Г.</copyright-holder><copyright-holder xml:lang="en">Timofeev V.Y., Ardyukov D.G., Timofeev A.V., Goldobin D.N., Valitov M.G.</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/2291">https://www.gt-crust.ru/jour/article/view/2291</self-uri><abstract><p>Для Байкальского региона, его окружения и Монголии рассмотрено глубинное строение земной коры. Карта положения границы Мохо построена по гравиметрической спутниковой модели EIGEN-6C4 для территории от 43 до 61° с.ш. и от 88 до 120° в.д. При интерпретации гравиметрических материалов использованы известные сейсмические данные. Интерпретация данных модели EIGEN-6C4 в редукции Буге выполнена в рамках двухслойной модели кора – мантия при разности плотности 0.5·103 кг/м3. В результате для Западно-Сибирской плиты и Сибирской платформы граница Мохо находится на глубине 40–45 км при слабых латеральных вариациях. В области байкальских впадин глубина уменьшается до 34–38 км. Южнее границы по Главному Саянскому разлому в горных районах получены значительные латеральные вариации глубины поверхности Мохо. В областях активного горообразования (Монгольский Алтай, Гоби-Алтай, Хангай) мощность коры достигает 55–60 км. Для Котловины Больших Озер мощность уменьшается до 45 км. Становое нагорье, пустыня Гоби и Большой Хинган отличаются глубиной от 45 до 50 км. На крайнем юго-западе территории в районе Джунгарии, Тянь-Шаня и Турфанской впадины наблюдаются максимальные перепады глубины Мохо (от 40 до 70 км). Ошибка определения глубины поверхности Мохо составляет от 2 до 4 км. Полученные оценки для Среднесибирского плоскогорья и байкальских впадин в целом соответствуют сейсмическим данным. Оценки, сделанные гравиметрическим методом по наземным данным, не противоречат нашим результатам. Аномальное поведение высоты квазигеоида, полученного для геопотенциала EIGEN-6C4, относительно эллипсоида WGS84 отмечено на северо-западной границе Амурской плиты. Северная граница плиты четко проявляется в латеральном распределении аномалий Буге и мощности коры.</p></abstract><trans-abstract xml:lang="en"><p>The article discusses deep Earth crustal structure in the Baikal region, neighboring territory and Mongolia. The EIGEN-6C4 satellite gravity model-based Moho depth map was drawn for the territory with coordinates 43 to 61° N, 88 to 120° E. Gravity data interpretation was performed using seismic results obtained. The Bouguer EIGEN-6C4 model data interpretation was performed within the two-layer crust – mantle model with density diference 0.5·103 kg/m3. According to interpretation, Moho depth of the West Siberian Plate and Siberian Platform was estimated at 40–45 km with slight lateral variations, The depth decreases to 34–38 km near the Baikal basins. Strong lateral variations in Moho depth were obtained in mountainous areas south of the boundary going along the Main Sayan fault. The crustal thickness reaches 55–60 km in the area of active orogens (Mongolian Altai, Gobi Altai, Hangai) and decreases to 45 km in the Great Lakes Basin. The Stanovoi Range, Gobi Desert and Big Hingan have Moho depths ranging from 45 to 50 km. The southwesternmost part of the territory near Dzungaria, Tien Shan and Tuffan basin show the maximum drop of Moho from a depth of 40 km to 70 km. The Moho depth estimation error is from 2 to 4 km. The depths obtained for the Central Siberian Plateau and the Baikal basins generally correspond to the seismic data. The ground-based gravity data estimations do not contradict our results. The height anomalies of the quasigeoid model for the EIGEN-6C4 geopotential model relative to the WGS84 ellipsoid are found on the northwestern boundary of the Amur plate. The northern boundary of the Amur plate is clearly defined in the lateral distribution of the Bouguer anomalies and crustal thickness.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>гравиметрические спутниковые модели</kwd><kwd>аномалии Буге</kwd><kwd>граница Мохо</kwd><kwd>Монгольский Алтай</kwd><kwd>Гоби-Алтай</kwd><kwd>Байкальский рифт</kwd><kwd>Сибирская платформа</kwd></kwd-group><kwd-group xml:lang="en"><kwd>satellite gravity models</kwd><kwd>Bouguer anomalies</kwd><kwd>Moho</kwd><kwd>Mongolian Altai</kwd><kwd>Gobi Altai</kwd><kwd>Baikal rift</kwd><kwd>Siberian Platform</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование проведено в рамках госзадания ИНГГ СО РАН (тема НИР № FWZZ-2026-0051).</funding-statement><funding-statement xml:lang="en">The study was carried out on the state assignment of the IPGG SB RAS (research topic No. FWZZ-2026-0051).</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">Bonvalot S., Briais A., Kuhn M., Peyrefitte A., Vales N., Biancale R., Gabalda G., Moreaux G., Reinquin F., Sarrailh M., 2012. 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