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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">10.18303/2619-1563-2021-3-41</article-id><article-id custom-type="elpub" pub-id-type="custom">geophystech-159</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>Электрическая анизотропия терригенных отложений: краткий обзор подходов к ее определению по данным электрокаротажа в вертикальных скважинах</article-title><trans-title-group xml:lang="en"><trans-title>Electrical anisotropy of terrigenous deposits: a brief overview of approaches to its determination from electrical logging data in vertical wells</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>Сухорукова</surname><given-names>К. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Suhorukova</surname><given-names>K. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Доктор технических наук, главный научный сотрудник лаборатории многомасштабной геофизики ИНГГ СО РАН. Область научных интересов: количественная интерпретация комплекса данных скважинной электрометрии в вертикальных и субгоризонтальных скважинах.630090, Новосибирск, просп. Акад. Коптюга, 3</p></bio><bio xml:lang="en"><p>Koptyug Ave., 3, Novosibirsk, 630090</p></bio><email xlink:type="simple">SuhorukovaKV@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>Петров</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Petrov</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кандидат технических наук, научный сотрудник лаборатории многомасштабной геофизики ИНГГ СО РАН. Область научных интересов: количественная интерпретация данных зондирующих методов скважинной электрометрии.630090, Новосибирск, просп. Акад. Коптюга, 3</p></bio><bio xml:lang="en"><p>Koptyug Ave., 3, Novosibirsk, 630090</p></bio><email xlink:type="simple">PetrovAM@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<country>Россия</country></aff><aff xml:lang="en">Trofimuk Institute of Petroleum Geology and Geophysics SB RAS<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>28</day><month>01</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><fpage>41</fpage><lpage>66</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Сухорукова К.В., Петров А.М., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Сухорукова К.В., Петров А.М.</copyright-holder><copyright-holder xml:lang="en">Suhorukova K.V., Petrov A.M.</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/159">https://www.rjgt.ru/jour/article/view/159</self-uri><abstract><p>Кратко рассмотрены некоторые публикации по определению анизотропии электрического сопротивления горных пород, прежде всего осадочного генезиса, по сигналам методов скважинной электрометрии. По российским публикациям приведены сведения об основных причинах возникновения микро- и макроанизотропии песчано-глинистых отложений, по российским и зарубежным статьям – история развития модельного подхода к описанию анизотропии УЭС. Проведен анализ основных подходов к оценке вертикального сопротивления. Рассмотрены как новые аппаратурные приемы, направленные на непосредственное измерение чувствительных к анизотропии компонент электромагнитного поля, так и методические способы к извлечению этой информации из сигналов "классических" электрокаротажных зондов. Технические решения – это многокомпонентные измерения наклонными и перпендикулярными оси прибора катушками, а также соосными прибору тороидальными катушками. К методическим способам относится комплексирование данных, измеренных зондами с разным типом возбуждения среды, например, индуктивным и гальваническим. В ряде статей предлагается двухэтапная схема: первым шагом определять горизонтальное сопротивление по сигналам многозондового индукционного каротажа, вторым шагом – вертикальное сопротивление по сигналам фокусированных зондов бокового каротажа. Подобные схемы реализуются с применением алгоритмов численной инверсии, в некоторых случаях – построения трансформант. Введение в интерпретационную модель анизотропии базируется на априорных данных (исследование керна, данные микрокаротажа), а при отсутствии таковых – на основании принципиальной невозможности согласования параметров изотропных моделей, построенных независимо по сигналам зондов с разным типом возбуждения. Особый акцент в обзоре уделен развитию теории метода бокового каротажного зондирования (БКЗ) советскими и российскими учеными и истории исследования влияния электрической анизотропии на сигналы градиент-зондов. Ввиду повсеместного использования метода на территории СССР эта тематика представлена в ряде публикаций, раскрывающих результаты теоретических исследований анизотропных геоэлектрических моделей, численного и физического моделирования сигналов БКЗ и методических разработок для их интерпретации.</p></abstract><trans-abstract xml:lang="en"><p>The article briefly reviews a number of publications on the problem of determining rocks electrical resistivity anisotropy (primarily of sedimentary genesis) using downhole resistivity logs. We provide the information on the main causes of sandy-clay sediments micro- and macroanisotropy according to Russian papers and the history of the model-based approaches to the resistivity anisotropy description according to Russian and foreign articles. We analyze the main approaches to the vertical resistivity estimation. Both new hardware solutions aimed at direct measurement of electromagnetic field components sensitive to anisotropy and methodological techniques for extracting this information from the signals of "conventional" resistivity logging tools are considered according to published studies. The hardware solutions are multicomponent measurements with inclined and perpendicular (to the tool axis) coils, as well as with coaxial toroidal coils. Methodological techniques include combining data measured by tools with different types of medium excitation, for example, induction and galvanic. A number of papers suggest a two-step scheme: the first step is to determine the horizontal resistivity using induction arrays data, and the second step is to determine the vertical resistivity using focused lateral logs. Such schemes are implemented using numerical inversion algorithms and in some cases by inventing transformations of measured signals. Adding anisotropy to the interpretational model is based on a priori data (core studies, microresistivity logs). In the absence of a priori data, anisotropy is added when it is impossible to reconcile the parameters of isotropic models built independently based on logs with different type of excitation. A special focus of the review is on the development of the theory of unfocused lateral logging (BKZ) method by Soviet and Russian scientists and on the history of research on the electrical anisotropy influence on the signals of gradient probes. Due to the widespread use of the method in the USSR, this topic is presented in a number of papers revealing the results of anisotropic geoelectric models theoretical studies, numerical and physical modeling of BKZ logs and methodological developments for their interpretation.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Удельное электрическое сопротивление</kwd><kwd>анизотропия</kwd><kwd>электрокаротажное зондирование</kwd><kwd>терригенные коллекторы</kwd><kwd>осадочные породы</kwd><kwd>геоэлектрическая модель</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Resistivity</kwd><kwd>anisotropy</kwd><kwd>logging</kwd><kwd>terrigenous reservoirs</kwd><kwd>clastic rocks</kwd><kwd>geoelectrical model</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Александров Б.Л. 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