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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-2021-12-3s-0551</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1260</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>ФРАКЦИОННЫЙ АНАЛИЗ СКРЕТЧ-ШЛАМА ДЛЯ ОПРЕДЕЛЕНИЯ УГЛА ВНУТРЕННЕГО ТРЕНИЯ ГОРНЫХ ПОРОД ОСАДОЧНОГО ЧЕХЛА КОВЫКТИНСКОГО МЕСТОРОЖДЕНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>ANALYSIS OF FRACTION CONTENTS IN ROCK SCRATCH TESTS FOR ESTIMATING THE ANGLE OF INTERNAL FRICTION FOR THE SEDIMENTARY COVER OF THE KOVYKTA FIELD</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>Торопецкий</surname><given-names>К. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Toropetsky</surname><given-names>K. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Лаврентьева, 6/1</p></bio><bio xml:lang="en"><p>Konstantin V. Toropetsky</p><p>6-1 Lavrentiev Ave, Novosibirsk 630090</p></bio><email xlink:type="simple">ktoropetsky@gmail.com</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>Борисов</surname><given-names>Г. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Borisov</surname><given-names>G. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Лаврентьева, 6/1</p></bio><bio xml:lang="en"><p>6-1 Lavrentiev 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>Смирнов</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Smirnov</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>625000, Тюмень, ул. Герцена, 70</p></bio><bio xml:lang="en"><p>70 Herzen St, Tyumen 625000</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>Носиков</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Nosikov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>625019, Тюмень ул. Воровского, 2</p></bio><bio xml:lang="en"><p>2 Vorovsky St, Tyumen 625019</p></bio><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ООО «НовосибирскНИПИнефть»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>NovosibirskNIPIneft LLC</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ООО «Газпром Недра»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Gazprom Nedra LLC</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>ООО «Газпром ВНИИГАЗ»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Gazprom VNIIGAZ LLC</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>19</day><month>10</month><year>2021</year></pub-date><volume>12</volume><issue>3S</issue><fpage>748</fpage><lpage>753</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Торопецкий К.В., Борисов Г.А., Смирнов А.С., Носиков А.В., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Торопецкий К.В., Борисов Г.А., Смирнов А.С., Носиков А.В.</copyright-holder><copyright-holder xml:lang="en">Toropetsky K.V., Borisov G.A., Smirnov A.S., Nosikov A.V.</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/1260">https://www.gt-crust.ru/jour/article/view/1260</self-uri><abstract><p>В работе показана возможность использования гранулометрического анализа шлама, образующегося при контролируемом царапании горных пород, для прогноза угла внутреннего трения.</p><p>Объект исследования – Ковыктинское газоконденсатное месторождение (ГКМ), которое занимает значительную территорию, охватывающую юго-восточную часть Иркутского амфитеатра Сибирской платформы, и по особенностям геологического строения и значительному объему углеводородов является уникальным. Осадочный чехол рассматриваемого объекта сложен венд-нижнепалеозойскими и частично рифейскими образованиями, суммарная толщина которых более 6000 м по новым данным сейсморазведки [Vakhromeev et al., 2019].</p><p>Методы исследования осадочного чехла Ковыктинского ГКМ базируются на наземных и скважинных геофизических исследованиях, дистанционных и геолого-структурных способах в сочетании с тектонофизическим подходом [Seminsky et al., 2018], основу которого составляют данные бурения, в том числе стандартные и специальные исследования кернового материала.</p></abstract><trans-abstract xml:lang="en"><p>The article describes the possibility of using the granulometric analysis of rock cuttings formed in controlled core scratching tests to estimate the angle of internal friction.</p><p>The study object is the Kovykta gas-condensate field (GCF) that occupies a wide area in the southeastern part of the Irkutsk amphitheater of the Siberian platform. This uniquely complex geological structure holds significant reserves of hydrocarbons. Its sedimentary cover is composed of the Vendian – lower Paleozoic and partly Riphean formations. Their total thickness exceeds 6000 m, as estimated from the new seismic survey data [Vakhromeev et al., 2019].</p><p>The sedimentary cover of the Kovykta GCF has been studied by surface and borehole geophysical techniques, remote sensing and geostructural methods, in combination with the tectonophysical approach [Seminsky et al., 2018] based on drilling data, including standard and special core sampling data.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>метод контролируемого царапания</kwd><kwd>скретч-тест</kwd><kwd>гранулометрический анализ</kwd><kwd>геомеханические свойства</kwd><kwd>угол внутреннего трения</kwd><kwd>корреляционный анализ</kwd><kwd>Ковыктинское месторождение</kwd></kwd-group><kwd-group xml:lang="en"><kwd>controlled core scratching</kwd><kwd>scratch test</kwd><kwd>granulometric analysis</kwd><kwd>geomechanical properties</kwd><kwd>angle of internal friction</kwd><kwd>correlation analysis</kwd><kwd>Kovykta field</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">Almenara J.R., Detournay E., Hudson J.A., 1992. 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