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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">aari</journal-id><journal-title-group><journal-title xml:lang="ru">Проблемы Арктики и Антарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Antarctic Research</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0555-2648</issn><issn pub-type="epub">2618-6713</issn><publisher><publisher-name>Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.30758/0555-2648-2020-66-3-381-395</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-296</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>ГЕОЛОГИЯ И ГЕОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOLOGY AND GEOPHYSICS</subject></subj-group></article-categories><title-group><article-title>Особенности распределения псефитового материала в верхнечетвертичных отложениях северной части Баренцева моря</article-title><trans-title-group xml:lang="en"><trans-title>Features of the coarse clasts (psephites) distribution in the Upper Quaternary sediments of the northern Barents Sea</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>Крылов</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Krylov</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</p></bio><email xlink:type="simple">akrylow@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>Малышев</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Malyshev</surname><given-names>S. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</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>Богин</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bogin</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</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>Захаров</surname><given-names>В. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Zakharov</surname><given-names>V. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</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>Гусев</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Gusev</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</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>Макаров</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Makarov</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФГБУ «ВНИИОкеангеология»; Санкт-Петербургский государственный университет, Институт Наук о Земле; ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>FGBU VNIIOkeangeologia; St. Petersburg State University, Institute of Earth Sciences; State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ФГБУ «ВНИИОкеангеология»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>FGBU VNIIOkeangeologia</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>29</day><month>09</month><year>2020</year></pub-date><volume>66</volume><issue>3</issue><fpage>381</fpage><lpage>395</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Крылов А.А., Малышев С.А., Богин В.А., Захаров В.Ю., Гусев Е.А., Макаров А.С., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Крылов А.А., Малышев С.А., Богин В.А., Захаров В.Ю., Гусев Е.А., Макаров А.С.</copyright-holder><copyright-holder xml:lang="en">Krylov A.A., Malyshev S.A., Bogin V.A., Zakharov V.Y., Gusev E.A., Makarov A.S.</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.aaresearch.science/jour/article/view/296">https://www.aaresearch.science/jour/article/view/296</self-uri><abstract><p>В работе приведена характеристика псефитового (донно-каменного) материала, отобранного в северной части желоба Франц-Виктория в экспедиции «Трансарктика-2019». Показано, что основная масса псефитов представлена неокатанными или плохоокатанными разностями. Преобладают изометричные и уплощенные формы обломков. Петрографический состав преимущественно карбонатный (известняки и доломиты) и песчаный. Основной механизм доставки псефитов — айсберговый разнос в период последней дегляциации на рубеже плейстоцен-голоцен. Источниками айсбергов являлись Земля Франца-Иосифа и район островов Белый — Виктория. Породы Земли Франца-Иосифа представлены, главным образом, меловым габбро-базальтовым комплексом и триасовыми песчаниками и алевролитами. На западе изученной площади (район островов Белый — Виктория) залегают верхнепалеозойские терригенные и карбонатные породы, а также протерозойские метаморфиты. Айсберги из обоих источников направлялись на север в сторону котловины Нансена через желоб Франц-Виктория, причем айсберги со стороны Земли Франца-Иосифа практически не доходили до западного борта желоба.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents the characteristics of the coarse clasts (psephites, larger than 1 cm) sampled in the northern part of the Franz Victoria Trough (Barents Sea) during the “Transarktika-2019” expedition. The studied sedimentary section was formed during the transition from the last deglaciation environments to the marine Holocene settings. The amount of psephites in deglacial sediments is much higher than the one in Holocene sediments. The petrographic composition of the psephites, their roundness (according to Waddell and Khabakov classifications) and shape (according to Zingg classification) were studied in detail. It is shown that the majority of psephites is represented by non-rounded or poorly rounded varieties. Isometric and disc-type shapes are predominating among coarse clasts. Isometric psephites prevail in “deglacial sediments”, while disc-shaped, bladed, and rodlike, as a rule, are current in marine Holocene sediments. The petrographic composition of psephites is mostly represented with carbonate (limestone and dolomite) and sandstones. The amount of carbonates increases from the Holocene to the deglacial part of the sediment section. Other rocks found in smaller quantities are represented by quartzites, cherts, shales, basalts, crystalline schists, gneisses, granites, pyrite. During the last deglaciation at the Late Pleistocene the iceberg rafting was the main mechanism of psephites delivery to the sampling points. The major sources of the icebergs were Franz Josef Land and the Belyi — Victoria Islands region. Rocks of Franz Josef Land are represented mainly by Cretaceous gabbro-basalt complex and Triassic sandstones and siltstones. Upper Paleozoic terrigenous and carbonate rocks, as well as Proterozoic metamorphites, occur in the west of the studied area (the area of the Belyi — Victoria Islands). The results of studying the petrographic composition of psephites allow us to conclude that during the last deglaciation icebergs from both sources were heading north towards the Nansen Basin through the Franz Victoria Trough. Both streams of icebergs failed to reach the opposite sides of the Franz Victoria Trough, mixing with each other approximately in the axial part of the trough and leaving it in northern directions.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>айсберговый разнос</kwd><kwd>Баренцево море</kwd><kwd>дегляциация</kwd><kwd>желоб Франц-Виктория</kwd><kwd>псефиты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Barents Sea</kwd><kwd>coarse clasts</kwd><kwd>deglatiation</kwd><kwd>Franc-Victoria Trough</kwd><kwd>iceberg rafting</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа поддержана субсидией Минобрнауки России (RFMEFI61619X0108).</funding-statement><funding-statement xml:lang="en">This work was funded by a subsidy from the Ministry of Education and Science of Russia (RFMEFI61619X0108).</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">Гусев Е.А. 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