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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-2023-14-1-0681</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1623</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>ГЛУБИННОЕ СТРОЕНИЕ ГОРНОГО АЛТАЯ И СОВРЕМЕННЫЕ МОДЕЛИ ГРАВИТАЦИОННОГО ПОЛЯ</article-title><trans-title-group xml:lang="en"><trans-title>DEEP STRUCTURE OF THE ALTAI MOUNTAINS AND MODERN GRAVITY FIELD MODELS</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>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>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><email xlink:type="simple">ardyukovdg@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>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"><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>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><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>1 Academician Koptyug Ave, Novosibirsk 630090,</p><p>3 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, 1, </p><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>1 Academician Koptyug Ave, Novosibirsk 630090,</p><p>3 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>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-4"/></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-4"/></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>Институт автоматики и электрометрии СО РАН;&#13;
Институт нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Automation and Electrometry of the Siberian Branch of the Russian Academy of Sciences;&#13;
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-4"><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 of the Siberian Branch of the 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>16</day><month>02</month><year>2023</year></pub-date><volume>14</volume><issue>1</issue><fpage>681</fpage><lpage>681</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Тимофеев В.Ю., Ардюков Д.Г., Голдобин Д.Н., Тимофеев А.В., Носов Д.А., Сизиков И.С., Калиш Е.Н., Стусь Ю.Ф., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Тимофеев В.Ю., Ардюков Д.Г., Голдобин Д.Н., Тимофеев А.В., Носов Д.А., Сизиков И.С., Калиш Е.Н., Стусь Ю.Ф.</copyright-holder><copyright-holder xml:lang="en">Timofeev V.Y., Ardyukov D.G., Goldobin D.N., Timofeev A.V., Nosov D.A., Sizikov I.S., Kalish E.N., Stus Y.F.</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/1623">https://www.gt-crust.ru/jour/article/view/1623</self-uri><abstract><p>Результаты наземных измерений в районах Горного Алтая, полученные методами абсолютной гравиметрии и космической геодезии, рассматривались совместно с моделью геопотенциала EIGEN-6C4 (модель рельефа ETOPO1), построенной по спутниковым данным. Анализировались различные виды данных: модельные величины вертикальной составляющей силы тяжести, значения силы тяжести в редукциях Буге, Фая, вариации вертикального градиента силы тяжести и изменения высот пунктов. С использованием модели EIGEN-6C4 в редукции Буге построен график мощности земной коры по линии Новосибирск (юг Западной Сибири) – плато Укок (Горный Алтай) длиной 800 км. Глубина границы Мохоровичича увеличивается от 40 км на северо-западе территории до 51 км на юго-востоке. Для модели однородной коры получено распределение глубин по поверхности Мохоровичича в Горном Алтае и его предгорьях.</p><p>Анализируя результаты построений в редукциях Буге и Фая, данные о высотах квазигеоида и соотношение высоты рельефа и аномалий Буге, следует сделать вывод, что в целом территория Горного Алтая изостатически скомпенсированна. Являются нескомпенсированными отдельные межгорные впадины, например Курайская и Чуйская долины.</p></abstract><trans-abstract xml:lang="en"><p>The results of the ground-based absolute gravity and space geodetic measurements for the Altai Mountains were considered in combination with EIGEN-6C4 Global Geopotential Model (ETOPO1 Global Relief Model) generated from the satellite data. Analysis was made on different kinds of data: model values for the vertical component of gravity, values of Bouguer and Faye gravity reductions, variations of the vertical gravity gradient, and changes in altitude of the measurement sites. With EIGEN-6C4 model for Bouguer reduction, the crustal thickness curve was drawn along the Novosibirsk (southern West Siberia) – Ukok Plateau (Altai Mountains) line with a length of 800 km. The Moho depth increases from 40 km in the northwest of the area to 51 km in the southeast. For the homogeneous crust model, there was obtained the Moho depth distribution in the Altai Mountains and their foothills.</p><p>The analysis of the results of modeling Bouguer and Faye reductions, the data on quasigeoid heights and the relationship between relief height and Bouguer anomalies implies that the Altai Mountains area as a whole is isostatically compensated. Non-compensated are some intermountain basins, such as, for example, the Kurai and Chuya valleys.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>спутниковые и наземные гравиметрические данные</kwd><kwd>абсолютная гравиметрия</kwd><kwd>космическая геодезия</kwd><kwd>граница Мохоровичича</kwd><kwd>Горный Алтай</kwd><kwd>редукции Буге и Фая</kwd><kwd>изостазия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>satellite and ground-based gravimetry data</kwd><kwd>absolute gravimetry</kwd><kwd>space geodesy</kwd><kwd>Moho</kwd><kwd>Altai Mountains</kwd><kwd>Bouguer and Faye reductions</kwd><kwd>isostasy</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена по проекту НИР ИНГГ СО РАН (FWZZ-2022-0019)</funding-statement><funding-statement xml:lang="en">The research was done as part of the project of the INGG SB RAS (FWZZ-2022-0019)</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">Алексеев А.С., Глинский Б.М., Геза Н.И., Еманов А.Ф., Кашун В.Н., Ковалевский В.В., Манштейн А.К., Селезнев В.С. и др. 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