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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">geology</journal-id><journal-title-group><journal-title xml:lang="ru">Известия высших учебных заведений. Геология и разведка</journal-title><trans-title-group xml:lang="en"><trans-title>Proceedings of higher educational establishments. Geology and Exploration</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0016-7762</issn><issn pub-type="epub">2618-8708</issn><publisher><publisher-name>Sergo Ordzhonikidze Russian State University for Geological Prospecting</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.32454/0016-7762-2015-2-5-8</article-id><article-id custom-type="elpub" pub-id-type="custom">geology-22</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</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOLOGY</subject></subj-group></article-categories><title-group><article-title>Стратиграфические и седиментологические аспекты палеоихнологического анализа</article-title><trans-title-group xml:lang="en"><trans-title>Stratigraphic and sedimentological aspects of ichnofabric analysis</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>Марусин</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Marusin</surname><given-names>V. V.</given-names></name></name-alternatives><email xlink:type="simple">marussin.vas@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>ФГБУН Институт нефтегазовой геологии и геофизики СО РАН им. А.А. Трофимука</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2015</year></pub-date><pub-date pub-type="epub"><day>28</day><month>04</month><year>2015</year></pub-date><volume>0</volume><issue>2</issue><fpage>5</fpage><lpage>8</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Марусин В.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Марусин В.В.</copyright-holder><copyright-holder xml:lang="en">Marusin V.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.geology-mgri.ru/jour/article/view/22">https://www.geology-mgri.ru/jour/article/view/22</self-uri><abstract><p>Одной из групп палеонтологических остатков, предоставляющих возможность решения комплексных геологических задач, являются ископаемые следы жизнедеятельности. Они представляют собой осадочные текстуры, образованные в результате жизнедеятельности (питания, перемещения и т. д.) организмов в осадке. Особое, «пограничное», положение ихнофоссилий между палеонтологическими остатками и осадочными текстурами приводит к тому, что использование ихнофоссилий для установления возраста, расчленения и корреляции отложений сопровождается серьезными ограничениями. Автором показаны основные особенности группы ископаемых следов жизнедеятельности, а также возможности применения данных палеоихнологического анализа для решения седиментологических и стратиграфических задач.</p></abstract><trans-abstract xml:lang="en"><p>Trace fossils are one of the paleontological groups that could be used for solving complex geological problems. Trace fossils represent the sedimentological structures, produced by living organisms in the mass of sediment. This complex, both paleontological and sedimentological, nature of ichnofossils results in serious limiiations for sedimentary sequences stratigraphic dissection, correlation and age determination. This paper demonstrates the main aspects of trace fossils and appliance of ichnofabric analysis for solving sedimentological and stratigraphic probl ems.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>ископаемые следы жизнедеятельности</kwd><kwd>ихнофации</kwd><kwd>ихнотекстурный анализ</kwd><kwd>ихностратиграфия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>trace fossils</kwd><kwd>ichnofacies</kwd><kwd>ichnofabric analysis</kwd><kwd>ichnostratigraphy</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">Микулаш Р., Дронов А. Палеоихнология - введение в изучение ископаемых следов жизнедеятельности. 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