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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_2026_106_6-22</article-id><article-id custom-type="elpub" pub-id-type="custom">reggeomet-482</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>РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>REGIONAL GEOLOGY</subject></subj-group></article-categories><title-group><article-title>Особенности эволюции магматических систем Карельской провинции Фенноскандинавского щита при переходе от архея к протерозою</article-title><trans-title-group xml:lang="en"><trans-title>Magmatic system evolution in the Karelian province of the Fennoscandian Shield during the Archean–Proterozoic transition</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7488-7394</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Чекулаев</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Chekulaev</surname><given-names>V. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Валерий Петрович Чекулаев, Доктор геолого-минералогических наук, главный научный сотрудник</p><p>Scopus Author ID 6701662357</p><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Valeriy P. Chekulaev, DSc (Geology and Mineralogy), Chief Researcher</p><p>Scopus Author ID 6701662357</p><p>Saint Petersburg</p></bio><email xlink:type="simple">vpchekulaev@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/0000-0001-5008-6867</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Егорова</surname><given-names>Ю. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Egorova</surname><given-names>Yu. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Юлия Сергеевна Егорова, Кандидат геолого-минералогических наук, научный сотрудник</p><p>Scopus Author ID 56017161300</p><p>WoS ResearcherID AAR-2265-2021</p><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Yuliya S. Egorova, PhD (Geology and Mineralogy), Researcher</p><p>Scopus Author ID 56017161300</p><p>WoS ResearcherID AAR-2265-2021</p><p>Saint Petersburg</p></bio><email xlink:type="simple">egorova@ipggras.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/0000-0003-0627-1293</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Арестова</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Arestova</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Наталия Александровна Арестова, Доктор геолого-минералогических наук, ведущий научный сотрудник</p><p>Scopus Author ID 6701725034</p><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Nataliya A. Arestova, DSc (Geology and Mineralogy), Leading Researcher</p><p>Scopus Author ID 6701725034</p><p>Saint Petersburg</p></bio><email xlink:type="simple">narestova2009@rambler.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии и геохронологии докембрия Российской академии наук</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>12</day><month>07</month><year>2026</year></pub-date><volume>33</volume><issue>2 (106)</issue><fpage>6</fpage><lpage>22</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чекулаев В.П., Егорова Ю.С., Арестова Н.А., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Чекулаев В.П., Егорова Ю.С., Арестова Н.А.</copyright-holder><copyright-holder xml:lang="en">Chekulaev V.P., Egorova Y.S., Arestova N.A.</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/482">https://reggeomet.elpub.ru/jour/article/view/482</self-uri><abstract><p>Проведено сравнение составов магматических пород неоархея и раннего палеопротерозоя (сумия) Карельской провинции Фенноскандинавского щита. В неоархее базит-ультрабазитовый магматизм имел ограниченное распространение, а главную роль в формировании коры играл гранитоидный магматизм. В это время появились первые в истории щита породы субщелочного и щелочного состава: санукитоиды (2,75–2,71 млрд лет), граниты и пегматиты (2,7–2,65 млрд лет) и карбонатиты (2,61 млрд лет). После перерыва в магматической активности продолжительностью около 100 млн лет протерозой начался с масштабного ультрабазит-базитового магматизма, проявленного в виде расслоенных интрузий, друзитов и вулканических комплексов (2,5–2,45 млрд лет). Сумийские базиты обогащены легкими редкоземельными элементами и характеризуются отрицательными значениями εNd(t) от −3,4 до −0,5. Среди неоархейских метакоматиитов и метабазальтов присутствуют как примитивные разности, так и обогащенные легкими редкоземельными элементами; те и другие имеют положительные значения εNd(t) от +0,5 до +2,6. Неоархейские породы средне-кислого состава представлены метавулканитами и различными гранитоидами — от тоналит-трондьемит-гранодиоритовых (ТТГ) разностей до санукитоидов и плагиомикроклиновых гранитов. ТТГ, санукитоиды и метавулканиты (2,76–2,70 млрд лет) обогащены K, Ba, Sr и легкими редкоземельными элементами и характеризуются значениями εNd(t) от −1 до +2,5. Плагиомикроклиновые граниты (2,72–2,65 млрд лет) варьируют по содержанию редких и редкоземельных элементов, а также по значениям εNd(t) от −5 до +2,2. Сумийские средне-кислые породы представлены двумя группами. Метавулканиты с SiO2 &lt;65 %, не имеющие интрузивных аналогов, вероятнее всего, являются дифференциатами сумийских вулканитов основного состава. Породы с SiO2 &gt;65 % представлены калиевыми метариолитами и гранитами (2,45–2,40 млрд лет) с высокими содержаниями Ti, Zr, Y, а также Ba и Rb, и характеризуются преимущественно отрицательными значениями εNd(t) от +0,5 до −3.</p></abstract><trans-abstract xml:lang="en"><p>The authors compared the Neoarchean and Early Paleoproterozoic (Sumian) igneous rock compositions in the Karelian province of the Fennoscandian Shield. The Neoarchean basite-ultrabasite magmatism was not widely spread, but granitoid magmatism was critical for crust formation. At that time, the first subalkaline and alkaline rocks appeared in the Shield: sanukitoids (2.75–2.71 Ga), granites and pegmatites (2.7–2.65 Ga), and carbonatites (2.61 Ga). After a magmatic activity hiatus of about 100 Ma, the Proterozoic began with large-scale ultrabasite-basite magmatism manifested as layered intrusions, drusites, and volcanic complexes (2.5–2.45 Ga). Sumian basites are enriched in light rare earth elements and have negative εNd(t) values ranging from −3.4 to −0.5. The Neoarchean metakomatiites and metabasalts include primitive varieties as well as those enriched in light rare earth elements; they both have positive εNd(t) values ranging from +0.5 to +2.6. The Neoarchean rocks of intermediate-felsic composition present metavolcanites and various granitoids — from tonalite-trondhjemite-granodiorite (TTG) to sanukitoids and plagiomicrocline granites. TTG, sanukitoids, and metavolcanics (2.76– 2.70 Ga) are enriched in K, Ba, Sr, and light rare earth elements, and are characterized by εNd(t) values from –1 to +2.5. Plagiomicrocline granites (2.72–2.65 Ga) vary in rare and rare earth element contents, as well as εNd(t) values from –5 to +2.2. The Sumian intermediate-felsic rocks have two groups. Metavolcanites with SiO2 &lt;65 %, which have no intrusive analogs, are more likely to be derivatives of the Sumian mafic volcanites. The rocks with SiO2 &gt;65 % are represented by potassic metarhyolites and granites (2.45–2.40 Ga) with high contents of Ti, Zr, Y, as well as Ba and Rb; they predominantly have negative εNd(t) values from +0.5 to –3.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>неоархей</kwd><kwd>палеопротерозой</kwd><kwd>геохимия магматических пород</kwd><kwd>метавулканиты</kwd><kwd>граниты</kwd><kwd>ТТГ</kwd><kwd>Sm–Nd</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Neoarchean</kwd><kwd>Paleoproterozoic</kwd><kwd>igneous rock geochemistry</kwd><kwd>metavolcanite</kwd><kwd>granite</kwd><kwd>TTG</kwd><kwd>Sm–Nd</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">работа выполнена в рамках государственного задания Института геологии и геохронологии докембрия Российской академии наук (тема FMUW- 2025-0003).</funding-statement><funding-statement xml:lang="en">the Institute of Precambrian Geology and Geochronology supported the work (state geological study, project FMUW-2025-0003).</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">Арестова Н. 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