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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">reggeomet</journal-id><journal-title-group><journal-title xml:lang="ru">Региональная геология и металлогения</journal-title><trans-title-group xml:lang="en"><trans-title>Regional Geology and Metallogeny</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0869-7892</issn><publisher><publisher-name>(ФГБУ "Институт Карпинского")</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.52349/0869-7892_2024_99_15-33</article-id><article-id custom-type="elpub" pub-id-type="custom">reggeomet-6</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>Терригенные коллекторы и россыпи алмазов древних платформ</article-title><trans-title-group xml:lang="en"><trans-title>Terrigenous diamond-bearing rocks and diamond placers of ancient platforms</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>Устинов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Ustinov</surname><given-names>V. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Устинов Виктор Николаевич – доктор геол.-минерал. наук, Советник ген. директора по минеральным ресурсам</p><p>Троицкий пр., 168, Архангельск, 163001</p></bio><bio xml:lang="en"><p>Ustinov Viktor Nikolaevich – DSc (Geology and Mineralogy), Advisor of General Director on Mineral Resources</p><p>168 Troitskiy Pr., Arkhangelsk, 163001</p></bio><email xlink:type="simple">UstinovVN@agddiamonds.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Акционерное общество «АГД Даймондс» (АО «АГД Даймондс»)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Joint Stock Company «AGD Diamonds» (JSC «AGD Diamonds»)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>21</day><month>09</month><year>2024</year></pub-date><volume>0</volume><issue>99</issue><fpage>15</fpage><lpage>33</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Устинов В.Н., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Устинов В.Н.</copyright-holder><copyright-holder xml:lang="en">Ustinov V.N.</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://reggeomet.elpub.ru/jour/article/view/6">https://reggeomet.elpub.ru/jour/article/view/6</self-uri><abstract><p>Выявлены особенности строения и условий формирования терригенных коллекторов алмазов на территориях древних платформ в течение доплатформенного, протоплатформенного и платформенного мегаэтапов эволюции. Сделаны выводы о потенциале россыпной и коренной алмазоносности. Выделены этапы формирования коллекторов алмазов в фанерозое. Показано, что образование ореолов рассеяния индикаторных минералов кимберлитов и россыпей различалось во времени в пределах платформ Гондвана и Лавразия. Исключение представляет неоген-четвертичный этап, который проявился во всех алмазоносных провинциях мира. Перечислены факторы формирования промышленных россыпей алмазов в процессе накопления терригенных коллекторов.</p></abstract><trans-abstract xml:lang="en"><p>There is specified structure and conditions of forming terrigenous diamond-bearing rocks within the territories of ancient platforms during the Preplatform, Protoplatform and Platform mega-stages of evolution. There are made conclusions about diamond placers and primary deposits potential. Stages of forming diamond-bearing rocks in the Phanerozoic are distinguished. The formation of dispersion halos of kimberlite indicator minerals varied in time on the Gondwana and Laurasia platforms. The exception is the Neogene-Quarternary stage, which manifested itself within all diamond provinces of the world. There are listed factors of forming commercial diamond placers during sedimentation of terrigenous diamond-bearing rocks.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>коллекторы алмазов</kwd><kwd>россыпь</kwd><kwd>коренной источник</kwd><kwd>алмаз</kwd><kwd>ореол рассеяния</kwd><kwd>кимберлит</kwd></kwd-group><kwd-group xml:lang="en"><kwd>terrigenous diamond-bearing rocks</kwd><kwd>placer</kwd><kwd>primary deposit</kwd><kwd>dispersion halo</kwd><kwd>diamond</kwd><kwd>kimberlite</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">Владимиров Б. М. Месторождения алмазов СССР. Методика поисков и разведки / Б. М. Владимиров, Ю. М. Дауев, Б. 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