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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">litosphere-355</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>ЗАКОНОМЕРНОСТИ ДИНАМИКИ ОКРАИННОМОРСКОГО МАГМАТИЗМА (КОРЕЙСКО-ЯПОНСКИЙ РЕГИОН)</article-title><trans-title-group xml:lang="en"><trans-title></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>Филатова</surname><given-names>Н. И.</given-names></name></name-alternatives><email xlink:type="simple">filatova@ilran.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт литосферы окраинных и внутренних морей РАН<country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2004</year></pub-date><pub-date pub-type="epub"><day>07</day><month>02</month><year>2019</year></pub-date><volume>0</volume><issue>3</issue><fpage>33</fpage><lpage>56</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Филатова
                 Н.И., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Филатова
                 Н.И.</copyright-holder><copyright-holder xml:lang="en">Филатова
                 Н.И.</copyright-holder><license 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.lithosphere.ru/jour/article/view/355">https://www.lithosphere.ru/jour/article/view/355</self-uri><abstract><p>Синтез информации по магматическим породам Корейско-Япономорского региона и вулканитам некоторых задуговых бассейнов запада Тихого океана позволил выявить специфику динамики магматизма Японского бассейна. Среди вулканитов, связанных с формированием Японского моря, на основе изотопно-геохимических критериев выделены: толеиты типа N-MORB; обогащенные известково-щелочной компонентой толеиты типа E-MORB2; толеиты E-MORB,, обогащенные компонентой WPB; щелочные базальты, аналогичные составам WPB (OIB). Источники магматизма сменялись в течение эволюции окраинного бассейна. Общая тенденция динамики магматизма бассейнов запада Тихого океана (включая Японское море) заключается в переходе от обогащенных известково-щелочной компонентой лав (плавление ранее модифицированной субдукционными флюидами верхней мантии) к N-MORB подобным толеитам зон спрединга (астеносферный источник типа Pacific). Специфика динамики Япономорского магматизма заключается в вовлечении в качестве источника неистощенного нижнемантийного вещества составов WPB (OIB). Судя по сейсмотомографическим данным, нижнемантийный материал распространялся от Тихоокеанского суперплюма на приповерхностные уровни мантии, создавая там аномалию DUPAL типа и участвуя в эволюции магматизма Японского бассейна.
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