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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-2017-8-2-0245</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-366</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>УСЛОВИЯ ПЛАВЛЕНИЯ ГРАНИТОИДНЫХ КСЕНОЛИТОВ В КОНТАКТЕ СО ЩЕЛОЧНО‐БАЗИТОВОЙ МАГМОЙ (ГУСИНООЗЕРСКАЯ ДАЙКА, ЗАПАДНОЕ ЗАБАЙКАЛЬЕ): К ПРОБЛЕМЕ ПРОИСХОЖДЕНИЯ УЛЬТРАКАЛИЕВЫХ КИСЛЫХ РАСПЛАВОВ</article-title><trans-title-group xml:lang="en"><trans-title>MELTING CONDITIONS OF GRANITOID XENOLITHS IN CONTACT WITH ALKALINE MAFIC MAGMA (GUSINOOZERSKAYA DYKE, WESTERN TRANSBAIKALIA): TO THE PROBLEM OF THE ORIGIN OF ULTRAPOTASSIC ACID MELTS</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>Хубанов</surname><given-names>В. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Khubanov</surname><given-names>V. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, с.н.с.,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а;</p><p>670000, Улан-Удэ, ул. Смолина, 24а</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior Researcher,</p><p>6a Sakhyanova street, Ulan-Ude 670047;</p><p>24a Smolin street, Ulan-Ude 670000</p></bio><email xlink:type="simple">khubanov@mail.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>Врублевская</surname><given-names>Т. Т.</given-names></name><name name-style="western" xml:lang="en"><surname>Vrublevskaya</surname><given-names>T. T.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, c.н.с.,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а;</p><p>670000, Улан-Удэ, ул. Смолина, 24а</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior Researcher,</p><p>6a Sakhyanova street, Ulan-Ude 670047;</p><p>24a Smolin street, Ulan-Ude 670000</p></bio><email xlink:type="simple">vrublevskayatt@rambler.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>Цыганков</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Tsygankov</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, директор,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а;</p><p>670000, Улан-Удэ, ул. Смолина, 24а</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Director,</p><p>6a Sakhyanova street, Ulan-Ude 670047;</p><p>24a Smolin street, Ulan-Ude 670000</p></bio><email xlink:type="simple">tsygan@gin.bscnet.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>Владимиров</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Vladimirov</surname><given-names>A. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, г.н.с., профессор,</p><p>630090, Новосибирск, просп. Академика Коптюга, 3;</p><p>630090, Новосибирск, ул. Пирогова, 2;</p><p>634050, Томск, просп. Ленина, 50</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Chief Researcher, Professor,</p><p>3 Academician Koptyug ave, Novosibirsk 630090;</p><p>2 Pirogov street, Novosibirsk 630090;</p><p>50 Lenin ave, Tomsk 634050</p></bio><email xlink:type="simple">vladimir@igm.nsc.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Буянтуев</surname><given-names>М. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Buyantuev</surname><given-names>M. D.</given-names></name></name-alternatives><bio xml:lang="ru"><p>м.н.с.,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а</p></bio><bio xml:lang="en"><p>Junior Researcher,</p><p>6a Sakhyanova street, Ulan-Ude 670047</p></bio><email xlink:type="simple">molon2@rambler.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Соколова</surname><given-names>Е. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Sokolova</surname><given-names>E. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, н.с.,</p><p>630090, Новосибирск, просп. Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Researcher,</p><p>3 Academician Koptyug ave, Novosibirsk 630090</p></bio><email xlink:type="simple">ekaterina@igm.nsc.ru</email><xref ref-type="aff" rid="aff-4"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Посохов</surname><given-names>В. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Posokhov</surname><given-names>V. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>с.н.с.,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а</p></bio><bio xml:lang="en"><p>Senior Researcher,</p><p>6a Sakhyanova street, Ulan-Ude 670047</p></bio><email xlink:type="simple">vitaf1@yandex.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хромова</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Khromova</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>м.н.с.,</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а</p></bio><bio xml:lang="en"><p>Junior Researcher,</p><p>6a Sakhyanova street, Ulan-Ude 670047</p></bio><email xlink:type="simple">lena.khromova.00@mail.ru</email><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геологический институт СО РАН;&#13;
Бурятский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute, Siberian Branch of RAS;&#13;
Buryat State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт геологии и минералогии им. В.С. Соболева СО РАН;&#13;
Новосибирский государственный университет;&#13;
Томский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS;&#13;
Novosibirsk State University;&#13;
Tomsk State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Геологический институт СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Институт геологии и минералогии им. В.С. Соболева СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2017</year></pub-date><pub-date pub-type="epub"><day>23</day><month>06</month><year>2017</year></pub-date><volume>8</volume><issue>2</issue><fpage>347</fpage><lpage>368</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хубанов В.Б., Врублевская Т.Т., Цыганков А.А., Владимиров А.Г., Буянтуев М.Д., Соколова Е.Н., Посохов В.Ф., Хромова Е.А., 2017</copyright-statement><copyright-year>2017</copyright-year><copyright-holder xml:lang="ru">Хубанов В.Б., Врублевская Т.Т., Цыганков А.А., Владимиров А.Г., Буянтуев М.Д., Соколова Е.Н., Посохов В.Ф., Хромова Е.А.</copyright-holder><copyright-holder xml:lang="en">Khubanov V.B., Vrublevskaya T.T., Tsygankov A.A., Vladimirov A.G., Buyantuev M.D., Sokolova E.N., Posokhov V.F., Khromova E.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://www.gt-crust.ru/jour/article/view/366">https://www.gt-crust.ru/jour/article/view/366</self-uri><abstract><p>Щелочно‐мафическая (лампрофировая) Гусиноозерская дайка (Западное Забайкалье) содержит гранитные ксенолиты, испытавшие частичное плавление. Среди ксенолитов выявлено два субстрата, претерпевших плавление: 1) плагиоклаз и кварц и 2) щелочной полевой шпат и кварц. Продукты плавления представляют собой микрофельзитовые и микрогранофировые оторочки вокруг гранитных ксенолитов мощностью в первые миллиметры. Во внутренних частях ксенолитов на границе кварца и полевых шпатов наблюдается ультракислое стекло. Отличительной особенностью новообразованных расплавов, независимо от состава протолитового субстрата, является их повышенная калиевость с отношением K2O/Na2O≥2. На основе сопоставления составов производных контактового плавления с экспериментальными данными показано, что плавление происходило в присутствии щелочно‐хлоридного и/или щелочно‐углекислого флюида, выделявшегося из кристаллизующейся вмещающей щелочно‐основной магмы. Оценены вероятные геотектонические условия возникновения ультракалиевых кислых магм.</p></abstract><trans-abstract xml:lang="en"><p>The alkaline mafic (lamprophyric) Gusinoozerskaya dyke in West Transbaikalia is composed of partially melted granite xenoliths. Among the xenoliths, two melted substrates are observed: (1) plagioclase and quartz, and (2) alkaline feldspar and quartz. Few millimeters thick microfelsite and microgranophiric rims are the products of melting around the granite xenoliths. Ultra‐acid glass is observed in the inner parts of the xenoliths at the boundary of quartz and feldspars. A distinctive feature of the fresh melts (regardless of the composition of the protolithic sub‐ strate) is an increased content of potassium with K2O/Na2O≥2. Having compared the compositions of the products of contact melting with the experimental data, we conclude that melting took place in the presence of alkaline‐chloride and/or alkaline‐carbonic fluid released from the crystallizing host alkaline‐basic magma. The probable geotectonic conditions for the occurrence of ultrapotassic acid magmas are estimated.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>щелочно‐базитовая магма</kwd><kwd>известково‐щелочной лампрофир</kwd><kwd>гранитоидные ксенолиты</kwd><kwd>контактовое плавление</kwd><kwd>ультракалиевый кислый расплав</kwd><kwd>петрогенетические и тектонические условия</kwd><kwd>Гусиноозерская дайка</kwd><kwd>Забайкалье</kwd></kwd-group><kwd-group xml:lang="en"><kwd>alkaline mafic magma</kwd><kwd>calc‐alkaline lamprophyre</kwd><kwd>granitoid xenoliths</kwd><kwd>contact melting</kwd><kwd>ultrapotassic acidic melt</kwd><kwd>petrogenetic and tectonic conditions</kwd><kwd>Gusinoozerskaya dyke</kwd><kwd>Transbaikalia</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Российский фонд фундаментальных исследований</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">Andryushchenko S.V., Vorontsov A.A., Yarmolyuk V.V., Sandimirov I.V., 2010. 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