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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 pub-id-type="doi">10.24930/1681-9004-2020-20-6-851-862</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1371</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>О плотности теплового потока, структуре мантии и нефтегазоносности полуострова Ямал (Арктика)</article-title><trans-title-group xml:lang="en"><trans-title>Heat flux density, mantle structure and oil and gas potential of the Yamal Peninsula (Arctic)</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>Иванов</surname><given-names>К. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>К. S.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"/><email xlink:type="simple">ivanovks55@ya.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Костров</surname><given-names>Н. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Kostrov</surname><given-names>N. Р.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"/><email xlink:type="simple">kostrov65@yandex.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 геохимии УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A.N. Zavaritsky Institute of Geology and Geochemistry, UB of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>29</day><month>12</month><year>2020</year></pub-date><volume>20</volume><issue>6</issue><fpage>851</fpage><lpage>862</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Иванов К.С., Костров Н.П., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Иванов К.С., Костров Н.П.</copyright-holder><copyright-holder xml:lang="en">Ivanov К.S., Kostrov N.Р.</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.lithosphere.ru/jour/article/view/1371">https://www.lithosphere.ru/jour/article/view/1371</self-uri><abstract><sec><title>Объект исследований</title><p>Объект исследований. П-ов Ямал представляет интерес в связи с тем, что концентрация месторождений углеводородов на единицу площади здесь более чем в 100 раз превышает “среднемировую”, что подтверждают запасы уже открытых крупнейших нефтегазовых месторождений. В то же время изученность глубинных горизонтов земной коры и мантии в пределах Ямала и смежных площадей по сравнению с более южными районами явно недостаточна.</p></sec><sec><title>Методы</title><p>Методы. В работе использовался метод сейсмической томографии, позволяющий выделять аномалии скоростей сейсмических волн напрямую связанных с плотностью теплового потока и геодинамической активностью недр.</p></sec><sec><title>Выводы</title><p>Выводы. По-видимому, Западно-Ямальская положительная тепловая аномалия маркирует область повышенной геодинамической активности, проницаемую для глубинных флюидно-газовых потоков. Расположение Ямала на приподнятом восточном плече этой аномальной области и обусловило высокую нефтегазоносность этого полуострова. Интерес для поисков могут представлять и другие районы, прилегающие к этой тепловой аномалии.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Research subject</title><p>Research subject. The Yamal Peninsula is of interest due to the fact that the concentration of hydrocarbon deposits per unit area is more than 100 times higher than the “world average”, which is confirmed by the reserves of the largest oil and gas fields already discovered. At the same time, the knowledge of the deep horizons of the earth’s crust and mantle within the Yamal and adjacent areas is clearly insufficient in comparison with more southern regions.</p></sec><sec><title>Methods</title><p>Methods. In this work, the method of seismic tomography was used, which makes it possible to identify anomalies in the velocities of seismic waves directly related to the heat flow density and geodynamic activity of the subsurface.</p></sec><sec><title>Conclusons</title><p>Conclusons. Apparently, the Western Yamal positive thermal anomaly indicates a region of a high geodynamic activity permeable for deep fluid-gas streams. The location of Yamal on a slightly raised shoulder of this anomalous region has determined the high oil and gas potential of this peninsula. Other regions situated in the vicinity of the discovered thermal anomaly may present significant research interest.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>месторождения нефти и газа</kwd><kwd>Ямал</kwd><kwd>плотность теплового потока</kwd><kwd>глубинное строение</kwd><kwd>триасовые рифты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>oil and gas deposits</kwd><kwd>Yamal</kwd><kwd>heat flux density</kwd><kwd>deep structure</kwd><kwd>Triassic rifts</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">Астафьев Д.А. 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