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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-2024-15-6-0797</article-id><article-id custom-type="edn" pub-id-type="custom">UPDKTV</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1945</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>ГЛУБИННОЕ СТРОЕНИЕ НИЖНЕАМУРСКОЙ ПРОВИНЦИИ И ЭПИТЕРМАЛЬНАЯ ЗОЛОТАЯ МИНЕРАЛИЗАЦИЯ В ЕЕ ПРЕДЕЛАХ</article-title><trans-title-group xml:lang="en"><trans-title>DEEP-SEATED STRUCTURE OF THE LOWER AMUR PROVINCE AND EPITHERMAL GOLD MINERALIZATION THEREIN</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>Носырев</surname><given-names>М. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Nosyrev</surname><given-names>M. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>680000, Хабаровск, ул. Ким Ю. Чена, 65</p></bio><bio xml:lang="en"><p>65 Kim Yu Chen St, Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Юрчук</surname><given-names>А. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Yurchuk</surname><given-names>A. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>680000, Хабаровск, ул. Ким Ю. Чена, 65</p></bio><bio xml:lang="en"><p>65 Kim Yu Chen St, Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Диденко</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Didenko</surname><given-names>A. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>680000, Хабаровск, ул. Ким Ю. Чена, 65, </p><p>119017, Москва, Пыжевский пер., 7, стр. 1</p></bio><bio xml:lang="en"><p>65 Kim Yu Chen St, Khabarovsk 680000,</p><p>7-1 Pyzhevsky Ln, Moscow 119017</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт тектоники и геофизики им. Ю.А. Косыгина ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kosygin Institute of Tectonics and Geophysics, Far Eastern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт тектоники и геофизики им. Ю.А. Косыгина ДВО РАН;&#13;
Геологический институт РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kosygin Institute of Tectonics and Geophysics, Far Eastern Branch of the Russian Academy of Sciences;&#13;
Geological Institute, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>13</day><month>12</month><year>2024</year></pub-date><volume>15</volume><issue>6</issue><fpage>797</fpage><lpage>797</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Носырев М.Ю., Юрчук А.Ю., Диденко А.Н., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Носырев М.Ю., Юрчук А.Ю., Диденко А.Н.</copyright-holder><copyright-holder xml:lang="en">Nosyrev M.Y., Yurchuk A.Y., Didenko A.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://www.gt-crust.ru/jour/article/view/1945">https://www.gt-crust.ru/jour/article/view/1945</self-uri><abstract><p>Построены плотностная и магнитная модели земной коры и литосферной мантии Нижнеамурской золотоносной площади. Выполнена геологическая и геодинамическая интерпретация полученных глубинных неоднородностей. Показано, что основная дифференциация региональных геофизических полей территории связана с неоднородностями подкоровой мантии и магматическими телами в средней и верхней части земной коры. Эти неоднородности являются результатом магматических процессов, происходивших на данном участке палеоазиатской окраины в позднемеловое – кайнозойское время в условиях субдукции, в режиме трансформной окраины и континентального рифтогенеза.</p><p>Показана пространственная связь эпитермальных золоторудных месторождений с рядом особенностей глубинного строения территории. Отмечена роль мантийных плотностных границ и плотностных неоднородностей на глубине до 20 км в распределении золотой минерализации. Выделены зоны развития глубинных магнитных тел, которые могут интерпретироваться как базитовые интрузии, трассирующие возможные глубинные магмоконтролирующие разломы, с которыми, в свою очередь, может быть связана золотая минерализация.</p></abstract><trans-abstract xml:lang="en"><p>The density and magnetic models of the Earth’s crust and lithospheric mantle were developed for the Lower Amur River gold-bearing area. Geological and geodynamical interpretations were made of the deep-seated inhomogeneities found there. It has been shown that the main differentiation of regional geophysical fields in the area is related to the subcrustal mantle inhomogeneities and magmatic bodies in the middle and upper crusts. These inhomogeneities resulted from the Late Cretaceous – Cenozoic magmatic processes occurring in this segment of the Paleoasian margin under subduction conditions, in the mode of strike-slip margin or continental rifting.</p><p>The spatial relationship was shown between the epithermal gold deposits and some of the deep-seated structural features of the area. Consideration was given to the role of the mantle density boundaries and up to 20 km deep density inhomogeneities in the gold mineralization distribution. There were identified zones of development of deep-seated magmatic bodies which can be interpreted as basaltic intrusions tracing the inferred deep-seated magma-controlling faults, to which, in its turn, gold mineralization can be related.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Сихотэ-Алинь</kwd><kwd>гравитационное поле</kwd><kwd>магнитное поле</kwd><kwd>глубинное строение</kwd><kwd>земная кора</kwd><kwd>литосфера</kwd><kwd>золоторудное месторождение</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Sikhote-Alin</kwd><kwd>gravity field</kwd><kwd>magnetic field</kwd><kwd>deep-seated structure</kwd><kwd>Earth’s crust</kwd><kwd>lithosphere</kwd><kwd>gold deposit</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках проекта Российского научного фонда (№ 22-17-00023). Базовое финансирование за счет субсидий на выполнение госзаданий ИТиГ ДВО РАН (темы НИР № 121021000095-1, № 121021000094-4) и ГИН РАН (тема № FMMG-2023-0010)</funding-statement><funding-statement xml:lang="en">The study was supported by the Russian Science Foundation (project No. 22-17-00023). Base funding is provided at the expense of subsidies for the implementation of state assignments of the ITIG FEB RAS (No. 121021000095-1, No. 121021000094-4) and GIN RAS (No. FMMG-2023-0010)</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">Алексеев А.С., Старостин В.И. Новое месторождение золота в Нижнем Приамурье – Чульбаткан (Хабаровский край) // Вестник МГУ. Серия 4. Геология. 2017. № 1. С. 33–38.</mixed-citation><mixed-citation xml:lang="en">Alekseev A.S., Starostin V.I., 2017. New Gold Deposit in Lower Amur – Chulbatkan (Khabarovsk Region). 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