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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">geophystech</journal-id><journal-title-group><journal-title xml:lang="ru">Геофизические технологии</journal-title><trans-title-group xml:lang="en"><trans-title>Russian Journal of Geophysical Technologies</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2619-1563</issn><publisher><publisher-name>IPGG SB RAS</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.18303/2619-1563-2022-2-129</article-id><article-id custom-type="elpub" pub-id-type="custom">geophystech-249</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>Статьи</subject></subj-group></article-categories><title-group><article-title>Учет наклонной электрической анизотропии при численном моделировании и интерпретации данных скважинной электрометрии (аналитический обзор по материалам отечественной и зарубежной литературы)</article-title><trans-title-group xml:lang="en"><trans-title>Accounting for tilted electrical anisotropy in numerical simulation and interpretation of resistivity logging data (analytical review based on national and foreign literature)</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>Москаев</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Moskaev</surname><given-names>I. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Младший научный сотрудник лаборатории многомасштабной геофизики Института нефтегазовой геологии и геофизики СО РАН. Основные научные интересы: прямые и обратные задачи электромагнитных зондирований, обоснование новых методов исследования скважин, новые способы интерпретации, разработка программного обеспечения для моделирования и инверсии данных.</p></bio><email xlink:type="simple">MoskaevIA@ipgg.sbras.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН&lt;br&gt;&#13;
630090, Новосибирск, просп. Акад. Коптюга, 3<country>Россия</country></aff><aff xml:lang="en">Trofimuk Institute of Petroleum Geology and Geophysics SB RAS&lt;br&gt;&#13;
Koptyug Ave., 3, Novosibirsk, 630090<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>29</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><fpage>129</fpage><lpage>143</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Москаев И.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Москаев И.А.</copyright-holder><copyright-holder xml:lang="en">Moskaev I.A.</copyright-holder><license 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.rjgt.ru/jour/article/view/249">https://www.rjgt.ru/jour/article/view/249</self-uri><abstract><p>Рассмотрены особенности и основные выводы публикаций, посвященных исследованию трансверсально-изотропных геоэлектрических моделей среды, характеризующихся наклоном оси электрической анизотропии относительно скважинного прибора. Такие модели могут описываться как горизонтальным и вертикальным удельными электропроводностями (либо обратными им величинами – удельными сопротивлениями) с ненулевым зенитным углом наклона каротажного прибора, так и тензором удельной электропроводности с наклоном главных осей.</p></abstract><trans-abstract xml:lang="en"><p>Features and main conclusions of publications devoted to the study of medium transverse-isotropic geoelectric models which are characterized by inclination of the electrical anisotropy axis relative to a logging tool are reviewed in this article. Such models can be defined either by horizontal and vertical conductivities (or their reciprocals, called resistivities) with a non-zero dip of a logging tool or by the conductivity tensor with the tilt of the principal axes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Удельное электрическое сопротивление</kwd><kwd>удельная электропроводность</kwd><kwd>электромагнитный каротаж</kwd><kwd>электрический каротаж</kwd><kwd>трансверсально-изотропная модель</kwd><kwd>относительный наклон оси электрической анизотропии</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Resistivity</kwd><kwd>conductivity</kwd><kwd>electromagnetic logging</kwd><kwd>electric logging</kwd><kwd>transverse-isotropic model</kwd><kwd>relative tilt of the electrical anisotropy axis</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Научно-исследовательские работы выполнены в рамках проекта FWZZ-2022-0026 «Инновационные аспекты электродинамики в задачах разведочной и промысловой геофизики».</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">Каринский А.Д. 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