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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">resar</journal-id><journal-title-group><journal-title xml:lang="ru">Природные ресурсы Арктики и Субарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Subarctic Natural Resources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2618-9712</issn><issn pub-type="epub">2686-9683</issn><publisher><publisher-name>Академия наук Республики Саха (Якутия)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31242/2618-9712-2021-26-3-64-74</article-id><article-id custom-type="elpub" pub-id-type="custom">resar-133</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>Науки о Земле. Инженерная геология, мерзлотоведение и грунтоведение</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Earth sciences. Engineering geology, permafrost and soil science</subject></subj-group></article-categories><title-group><article-title>Метод микроморфологического анализа рыхлых отложений и его применение для реконструкции палеогеографической обстановки в криолитозоне</article-title><trans-title-group xml:lang="en"><trans-title>The method of micromorphological analysis of loose sediments and its application for the reconstruction of paleogeographic settings in the cryolithozone</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7970-9124</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Куть</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kut’</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>КУТЬ Анна Алексеевна, кандидат геолого-минералогических наук, научный сотрудник</p><p>677007, Якутск, ул. Мерзлотная, 36</p><p>Researcher ID: E-2780-2018</p></bio><bio xml:lang="en"><p>KUT’, Anna Alekseevna, Cand. Sci. (Geology and Mineralogy), Researcher</p><p>36 Merzlotnaya st., Yakutsk 677010</p><p>Researcher ID: E-2780-2018</p></bio><email xlink:type="simple">ann.urban@mail.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/0000-0002-7910-9441</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мельников</surname><given-names>А. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Melnikov</surname><given-names>A. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>МЕЛЬНИКОВ Андрей Евгеньевич, кандидат геолого-минералогических наук, старший научный сотрудник</p><p>677007, Якутск, ул. Мерзлотная, 36</p><p>Researcher ID: O-4081-2017, Scopus ID: 57208581176</p></bio><bio xml:lang="en"><p>MELNIKOV, Andrey Evgen’evich, Cand. Sci. (Geology and Mineralogy), Senior Researcher</p><p>36 Merzlotnaya st., Yakutsk 677010</p><p>Researcher ID: O-4081-2017, Scopus ID: 57208581176</p></bio><email xlink:type="simple">melnikowdron@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт мерзлотоведения им. П.И. Мельникова СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Melnikov Permafrost Institute, SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>16</day><month>09</month><year>2021</year></pub-date><volume>26</volume><issue>3</issue><fpage>64</fpage><lpage>74</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Куть А.А., Мельников А.Е., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Куть А.А., Мельников А.Е.</copyright-holder><copyright-holder xml:lang="en">Kut’ A.A., Melnikov A.E.</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://resar.elpub.ru/jour/article/view/133">https://resar.elpub.ru/jour/article/view/133</self-uri><abstract><p>В статье приведены сведения об истории развития метода микроморфологического анализа рыхлого материала. Описаны существующие методики диагностики отложений, рассмотрены основные проблемы, связанные с их применением и корреляцией результатов. Проанализировано современное положение микроморфологического анализа в комплексе литолого-фациальных исследований. Подчеркнуто, что становлению метода способствовал технический прогресс в XX в. Применение электронной микроскопии вывело рассматриваемый метод на совершенно новый уровень. Метод в свое время был разработан для реконструкции обстановки переноса и накопления четвертичных отложений вне области криолитозоны. Однако с 1970-х годов исследование поверхности зерен начали применять для изучения особенностей проявления криогенеза в осадочных отложениях. На современном этапе начинают внедрять современные методы исследований поверхности частиц с использованием компьютерной томографии. Это значительно расширяет область применения метода микроморфологического анализа рыхлых отложений для различных целей. Приводится набор диагностических элементов, выделенных в результате применения данного метода для Кызыл-Сырского дюнного массива в бассейне р. Вилюй и разреза Абалахской поверхности в среднем течении р. Лена.</p></abstract><trans-abstract xml:lang="en"><p>The data on the history of the morphological analysis of loose materials are presented. The existing procedures of sediment diagnostics are described, the major problems related to their application and correlation of the results are considered. The modern status of micromorphological analysis in the set of lithological-facial investigations is analyzed. The development of the method was promoted by the technological advancement in the 20th century. The application of electron microscopy has brought the method under consideration to a brand new level. The method was originally developed to recover the settings of transport and accumulation of Quaternary sediments outside the boundaries of the cryolithozone. However, since the 1970-s, investigation of grain surfaces started to be applied to study the features of cryogenesis manifestations in sedimentary deposits. At the modern stage, up-to-date methods to study particle surface with the help of computer tomography are under introduction. This broadens the area of the application of micromorphological analysis of loose sediments for various purposes. A set of diagnostic elements allocated as a result of the application of this method for the Kyzyl-Syr dune area in the basin of the Vilyuy river and for the section of the Abalakh surface in the middle reach of the Lena river is presented.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>микроморфологический анализ</kwd><kwd>исторический обзор</kwd><kwd>становление метода</kwd><kwd>обстановка осадконакопления</kwd><kwd>криогенез</kwd></kwd-group><kwd-group xml:lang="en"><kwd>micromorphological analysis</kwd><kwd>historical survey</kwd><kwd>establishment of the method</kwd><kwd>sedimentation environment</kwd><kwd>cryogenesis</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке РФФИ в рамках научного проекта № 20-55-53006 «Криогипергенез грунтовых массивов Южной Якутии России и Северо-Восточного Китая: механизм и особенность».</funding-statement><funding-statement xml:lang="en">The research was carried out with support from the Russian Foundation for Basic Research (Project number 20-55-53006 «Cryogenesis of ground massifs of Southern Yakutia, Russia, and North-Eastern China: mechanism and specificity»).</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">Sorby H.C. 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