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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">nznistu</journal-id><journal-title-group><journal-title xml:lang="ru">Науки о Земле и недропользование</journal-title><trans-title-group xml:lang="en"><trans-title>Earth sciences and subsoil use</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2686-9993</issn><issn pub-type="epub">2686-7931</issn><publisher><publisher-name>Federal State Budget Educational Institution of Higher Education "Irkutsk National Research Technical University"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.21285/2686-9993-2024-47-1-100-128</article-id><article-id custom-type="edn" pub-id-type="custom">AVKQNU</article-id><article-id custom-type="elpub" pub-id-type="custom">nznistu-335</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>Горнопромышленная и нефтегазопромысловая геология, геофизика, маркшейдерское дело и геометрия недр</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Applied mining and petroleum field geology, geophysics, mine surveying and subsoil geometry</subject></subj-group></article-categories><title-group><article-title>Петромагнетизм и палеомагнетизм кимберлитовых трубок Верхне-Мунского месторождения (Якутская алмазоносная провинция)</article-title><trans-title-group xml:lang="en"><trans-title>Petromagnetism and paleomagnetism of kimberlite pipesof the Verkhnemunskoe deposit (Yakutsk diamondiferous province)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-0688-2249</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хороших</surname><given-names>М. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Khoroshikh</surname><given-names>M. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Максим Сергеевич Хороших, cтарший горный инженер</p><p>Бодайбо</p></bio><bio xml:lang="en"><p>Maksim S. Khoroshikh, Senior Mining Engineer</p><p>Bodaibo</p></bio><email xlink:type="simple">xoroshix1991@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/0000-0002-1196-8776</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Константинов</surname><given-names>К. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Konstantinov</surname><given-names>K. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Константин Михайлович Константинов, доктор геолого-минералогических наук, руководитель департамента</p><p>институт «Сибирская школа геонаук»; департамент геофизики</p><p>Иркутск</p></bio><bio xml:lang="en"><p>Konstantin M. Konstantinov, Dr. Sci. (Geol. &amp; Mineral.),Head of the Department</p><p>Siberian School of Geosciences; Geophysics Department</p><p>Irkutsk</p></bio><email xlink:type="simple">konstantinovkm@ex.istu.edu</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2722-4958</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шарыгин</surname><given-names>И. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Sharygin</surname><given-names>I. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Игорь Сергеевич Шарыгин, кандидат геолого-минералогических наук, заведующий лабораторией</p><p>лаборатория петрологии, геохимии и рудогенеза</p><p>Иркутск</p></bio><bio xml:lang="en"><p>Igor S. Sharygin, Cand. Sci. (Geol. &amp; Mineral.), Head of the Laboratory</p><p>Laboratory of Petrology, Geochemistry and Ore Genesis</p><p>Irkutsk</p></bio><email xlink:type="simple">isharygin@crust.irk.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-1626-4636</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кузина</surname><given-names>Д. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Kuzina</surname><given-names>D. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Диляра Мтыгулловна Кузина, кандидат геолого-минералогических наук, старший научный сотрудник</p><p>Институт геологии и нефтегазовых технологий</p><p>Казань</p></bio><bio xml:lang="en"><p>Dilyara M. Kuzina, Cand. Sci. (Geol. &amp; Mineral.), Senior Researcher</p><p>Institute of Geology and Oil and Gas Technologies</p><p>Kazan</p></bio><email xlink:type="simple">di.kuzina@gmail.com</email><xref ref-type="aff" rid="aff-4"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-8745-3376</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Потапов</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Potapov</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Сергей Владимирович Потапов, младший научный сотрудник</p><p>лаборатория петрологии, геохимии и рудогенеза</p><p>Иркутск</p></bio><bio xml:lang="en"><p>Sergei V. Potapov, Junior Researcher of the Laboratory</p><p>Laboratory of Petrology, Geochemistry and Ore Genesis</p><p>Irkutsk</p></bio><email xlink:type="simple">potapovsv@crust.irk.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0009-6481-9633</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кокодей</surname><given-names>Д. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Kokodey</surname><given-names>D. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Диана Юрьевна Кокодей, студент</p><p>институт «Сибирская школа геонаук»</p><p>Иркутск</p></bio><bio xml:lang="en"><p>Diana Yu. Kokodey, Student</p><p>Siberian School of Geosciences</p><p>Irkutsk</p></bio><email xlink:type="simple">di_kokodey@geo.istu.edu</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ПАО «Лензолото»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>JSC Gold Mining Company “Lenzoloto”</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Иркутский национальный исследовательский технический университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Irkutsk National Research Technical University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><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 SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Казанский федеральный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kazan Federal University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>28</day><month>04</month><year>2024</year></pub-date><volume>47</volume><issue>1</issue><fpage>100</fpage><lpage>128</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хороших М.С., Константинов К.М., Шарыгин И.С., Кузина Д.М., Потапов С.В., Кокодей Д.Ю., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Хороших М.С., Константинов К.М., Шарыгин И.С., Кузина Д.М., Потапов С.В., Кокодей Д.Ю.</copyright-holder><copyright-holder xml:lang="en">Khoroshikh M.S., Konstantinov K.M., Sharygin I.S., Kuzina D.M., Potapov S.V., Kokodey D.Y.</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.nznj.ru/jour/article/view/335">https://www.nznj.ru/jour/article/view/335</self-uri><abstract><p>   Цель проведенных исследований кимберлитовых трубок Верхне-Мунского месторождения алмазов заключалась в расчете среднепалеозойского палеомагнитного полюса для уточнения траектории кажущейся миграции полюса и реконструкций палеогеографического положения Сибирской платформы на время проявления активныхтектоно-магматических процессов.</p><p>   Верхне-Мунское месторождение расположено в пределах Верхне-Мунского кимберлитового поля Якутской алмазоносной провинции и включает пять кимберлитовых трубок («Деймос», «Заполярная», «Комсомольская-Магнитная», «Новинка» и «Поисковая»), возраст которых по геологическим и изотопным данным оценивается как поздний девон – ранний карбон (372–347 млн лет). Впервые получены скалярные и векторные физические параметры кимберлитов и захваченных ими ксенолитов из разных структурно-вещественных комплексов земной коры, а также вмещающих террегенно-осадочные породы раннего палеозоя, необходимые для разработки физико-геологических моделей месторождений Верхне-Мунского поля. По данным анизотропии магнитной восприимчивости установлен относительно глубокий уровень эрозионного среза месторождения. Согласно палеомагнитным данным, в связующей массе кимберлитов сохранилась первичная (синхронная становлению месторождения) естественная остаточная намагниченность. Основными минералами-носителями векторов естественной остаточной намагниченности кимберлитов являются неизмененные магнезиоферрит и магнетит, что свидетельствует об их термоостаточной природе. Векторы естественной остаточной намагниченности захваченных ксенолитов указывают на то, что влияние гипергенных процессов не сильно отразилось на векторах естественной остаточной намагниченности кимберлитов. Тест «обжига» вмещающих пород положительный, что указывает на первичную природу характеристической естественной остаточной намагниченности кимберлитов. По полученным кластерам N = 10 векторов первичной естественной остаточной намагниченности кимберлитовых трубок рассчитан палеомагнитный полюс с координатами Φ = 26,5° с. ш., Λ = 142,2° в. д., dp/dm = 6,2/7,8°. Палеомагнитное датирование векторов естественной остаточной намагниченности кимберлитов Верхне-Мунского месторождения соответствует среднему палеозою. На основе рассчитанного палеомагнитного полюса реконструировано палеогеографическое положение Сибирской платформы, которая на момент внедрения кимберлитов находилась на средних широтах северного полушария и была обращена к северу своим южным краем.</p></abstract><trans-abstract xml:lang="en"><p>   The purpose of the studies of kimberlite pipes of the Verkhnemunskoe diamond field is to calculate the Middle Paleozoic paleomagnetic pole to clarify the trajectory of the apparent migration of the pole and reconstructions of the paleogeographic position of the Siberian platform at the time of the manifestation of active tectono-magmatic processes.</p><p>   The Verkhnemunskoye deposit is located within the Verkhnemunskoye kimberlite field of the Yakutsk diamondiferous province and includes five kimberlite pipes (Deimos, Zapolyarnaya, Komsomolskaya-Magnitnaya, Novinka and Poiskovaya), the age of which according to geological and isotopic data is estimated as Late Devonian-Early Carboniferous (372–347 Ma). For the first time scalar and vector physical parameters of kimberlites and captured xenoliths from different structural-material complexes of the Earth’s crust, as well as the host terrigenous sedimentary rocks of the Early Paleozoic were obtained, which are necessary for the development of physical-geological models of the Verkhnemunskoe field deposits. A relatively deep level of erosional shearing of the field has been established. The primary (synchronous with the formation of the field) natural residual magnetization was preserved in the kimberlite cohesive mass. The main carrier minerals of natural remanent magnetization vectors of kimberlites are unaltered magnesioferrite and magnetite, which indicates their thermo-sufficient nature. The natural remanent magnetization vectors of captured xenoliths indicate that the influence of hypergenic processes did not strongly affect the NRM vectors of kimberlites. Firing test is positive. The paleomagnetic pole with coordinates Φ = 26.5°N, Λ = 142.2°E, dp/dm = 6.2/7.8° was calculated from the obtained clusters of N = 10 vectors of the primary natural remanent magnetization of kimberlite pipes. On its basis, we reconstructed the paleogeographic position of the Siberian Platform, which at the time of the kimberlite intrusion was located in the middle latitudes of the northern hemisphere and was facing north with its southern edge.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Якутская алмазоносная провинция</kwd><kwd>Верхне-Мунское месторождение</kwd><kwd>кимберлитовые трубки</kwd><kwd>Заполярная</kwd><kwd>Деймос</kwd><kwd>Комсомольская-Магнитная</kwd><kwd>Новинка</kwd><kwd>Поисковая</kwd><kwd>кимберлиты</kwd><kwd>средний палеозой</kwd><kwd>палеомагнетизм</kwd><kwd>магнетиты</kwd><kwd>магнезиоферриты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Yakutsk diamondiferous province</kwd><kwd>Verkhnemunskoe deposit</kwd><kwd>kimberlite pipes</kwd><kwd>Zapolyarnaya</kwd><kwd>Deimos</kwd><kwd>Komsomolkaya-Magnitnaya</kwd><kwd>Novinka</kwd><kwd>Poiskovaya</kwd><kwd>kimberlites</kwd><kwd>Middle Paleozoic</kwd><kwd>paleomagnetism</kwd><kwd>magnetites</kwd><kwd>magnesioferrites</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">Храмов А.Н., Гончаров Г.И., Комиссарова Р.А., Писаревский С.А., Погарская И.А., Ржевский Ю.С. 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