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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-2022-13-1-0576</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1429</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>ПАЛЕОГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>PALEOGEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>ТЕРРИГЕННО-КАРБОНАТНЫЙ РАЗРЕЗ СРЕДНЕГО ТЕЧЕНИЯ Р. ВИТИМ: КОРРЕЛЯЦИЯ, ВОЗРАСТНОЕ И ГЕОДИНАМИЧЕСКОЕ ПОЛОЖЕНИЕ</article-title><trans-title-group xml:lang="en"><trans-title>TERRIGENOUS-CARBONATE CROSS-SECTION IN THE MIDDLE COURSE OF THE VITIM RIVER: CORRELATION, AGE, AND GEODYNAMICS</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>Станевич</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Stanevich</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Arkady M. Stanevich</p><p>128 Lermontov St, Irkutsk 664033</p></bio><email xlink:type="simple">stan@crust.irk.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>22</day><month>03</month><year>2022</year></pub-date><volume>13</volume><issue>1</issue><fpage>576</fpage><lpage>576</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Станевич А.М., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Станевич А.М.</copyright-holder><copyright-holder xml:lang="en">Stanevich A.M.</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/1429">https://www.gt-crust.ru/jour/article/view/1429</self-uri><abstract><p>Описан разрез (12 км) мощной толщи осадочных пород левого берега р. Витим, напротив рек Нижний Орлов и Данная. Участок относится к Каралон-Мамаканскому блоку Байкало-Муйского внутреннего пояса Байкальской складчатой области [Rytsk et al., 2011]. Изменены формально выделенные ранее названия стратиграфических подразделений: сюльбанская серия на чаянгрскую толщу, келянская подсерия на каралонскую толщу. Выявлена сложная складчато-разрывная структура и литолого-фациальные характеристики разреза. Подтверждено более молодое положение каралонской толщи по отношению к чаянгрской. При сопоставлении с хорошо изученными подразделениями северных зон региона показано, что каралонская толща, вероятнее всего, соотносится с дальнетайгинским горизонтом нижнего венда, чаянгрская толща сопоставляется с баллаганахской серией верхнего рифея, а ее нижние слои, судя по составу, могут соответствовать медвежевскому горизонту.</p></abstract><trans-abstract xml:lang="en"><p>The descripton has been provided for the cross-section (12 km) of a thick sediment unit on the left bank of the Vitim River, opposite the Nizhny Orlov and Dannaya rivers. This place is related to the Karalon-Mamakan area of the Baikal-Muya belt of the Baikal folded area. The changes have been made to the names formally assigned to the following stratigraphic subdivisions: Sulban series was renamed Chayangra formation, and Kelyan subseries was renamed Karalon formation. Evidence has been found for the complex folded and faulted structure and litological-facial characteristics of the cross-section. Some evidence has been provided to confirm that the Karalon formation is younger than the Chayangra formation. When this result is comapared to the well-studied subdivisions of the northern areas of the region, it is apparent that the Karalon formation may well correlate with the Dalnetaiga horizon of the Lower Vendian, the Chayangra formation – with the Ballaganakh series of the Late Riphean, and its layers at the bottom are similar in composition to the the Medvezhevsk horizon.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Байкальская складчатая область</kwd><kwd>р. Витим</kwd><kwd>неопротерозой</kwd><kwd>корреляция</kwd><kwd>обстановки осадконакопления</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Baikal folded area</kwd><kwd>Vitim River</kwd><kwd>Neoproterozoic</kwd><kwd>correlation</kwd><kwd>depositional environment</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">В работе задействовалось оборудование ЦКП «Геодинамика и гехронология» Института земной коры СО РАН в рамках гранта № 075-15-2021-682.</funding-statement><funding-statement xml:lang="en">This work involved equipment from the Shared Research Facilities "Geodynamics and Geochronology" of the Institute of the Earth’s Crust SB RAS (grant 075-15-2021-682).</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">Решения Всесоюзного стратиграфического совещания по докембрию, палеозою и четвертичной системе Средней Сибири. 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