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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-2020-11-2-0478</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1036</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>СОВРЕМЕННАЯ ГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RECENT GEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>ГЕОДИНАМИЧЕСКИЕ РЕЖИМЫ ЦЕНТРАЛЬНОЙ АЗИИ ЗАПАДНЕЕ И ВОСТОЧНЕЕ ГЕОРАЗДЕЛА 102–104°</article-title><trans-title-group xml:lang="en"><trans-title>CENTRAL ASIAN GEODYNAMIC REGIMES WEST AND EAST 102–104° GEODIVIDER</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7225-7073</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Гатинский</surname><given-names>Ю. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Gatinsky</surname><given-names>Yu. G.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"/><email xlink:type="simple">gatinsky@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8829-2081</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Прохорова</surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Prokhorova</surname><given-names>T. V.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"/><email xlink:type="simple">tatprokh@mitp.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/0000-0001-8428-5936</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рундквист</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Rundquist</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"/><email xlink:type="simple">dvr@sgm.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт теории прогноза землетрясений и математической геофизики РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Earthquake Prediction Theory and Mathematical Geophysics of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Государственный геологический музей им. В.И. Вернадского РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.I. Vernadsky State Geological Museum 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>20</day><month>06</month><year>2020</year></pub-date><volume>11</volume><issue>2</issue><fpage>334</fpage><lpage>351</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гатинский Ю.Г., Прохорова Т.В., Рундквист Д.В., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Гатинский Ю.Г., Прохорова Т.В., Рундквист Д.В.</copyright-holder><copyright-holder xml:lang="en">Gatinsky Y.G., Prokhorova T.V., Rundquist D.V.</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/1036">https://www.gt-crust.ru/jour/article/view/1036</self-uri><abstract><p>Геораздел 102–104° в.д. выделяется по многочисленным геологическим и геофизическим при­знакам в Северной, Центральной и Южной Азии, подтверждаемым в его центральной части данными по сейсмичности, сейсмоактивным разломам и современному блоковому строению земной коры. На основании этих данных и по распространению эпицентров инструментально зафиксированных и исторических землетрясе­ний откорректированы границы блоков и межблоковых зон в центральной части геораздела и на его крыльях. Значительное возрастание объемов высвобождающейся сейсмической энергии до 1011–1016 Дж происходит в восточной части западного крыла геораздела, реже – непосредственно в нем, а к востоку от него – только на западной границе блока Юго-Восточного Китая вблизи геораздела. Проведенный авторами анализ глубинных сейсмических разрезов и графиков диссипации энергии вдоль трансектов, пересекающих геораздел и его западное крыло, показывает преобладание левосторонних сдвигов с северо-западным простиранием на севере, надвигов к востоку и юго-востоку в центре и правосторонних сдвигов с северо-восточным простиранием на юге. Общий уровень объема энергии постоянно возрастает к западу. Перемещения по горизонтали блоков в центральном и северном сегментах центральной части геораздела 102–104° в.д. и к западу от него по данным GPS оказывают непосредственное влияние на увеличение уровня сейсмичности и изменение геодинамических режимов в пределах изучаемых районов Центральной Азии. Смена направления векторов горизонтального перемещения сопровождается изменением режима тектонических напряжений. Установлено возрастание значений теплового потока к востоку от геораздела в Восточно-Азиатской транзитной зоне, предположительно связанное со сменой геодинамического режима в том же направлении под влиянием погруженного тихоокеанского слэба. Данные по сейсмической анизотропии и томографии литосферы, полученные китайскими и российскими исследователями, подтверждают процессы деламинации коры Юго-Восточного Тибета при ее взаимодействии с более холодной и мощной литосферой Юго-Восточного Китая и перемещение ее верхних слоев к юго-востоку и к югу, предполагавшееся в более ранних работах авторов.</p></abstract><trans-abstract xml:lang="en"><p>Ample geologic and geophysical data provide the basis for distinguishing the 102–104° E geodivider in the North, Central and South Asia. The geodivider’s central part is confirmed by the data on seismicity, seismically active faults and the modern crust block structure. These data and historical and instrumentally identified earthquake epicenters were used for a more correct definition of the block boundaries and interblock zones in the central part of the geodivider and in its wings. Seismic energy is considerably increased (to 1011–1016 J) in the eastern part of the geodivider’s western wing, and rarely increased directly in the geodivider itself. Near the geodivider, a seismic energy increase is detected east of it only at the western border of the South-Eastern China Block. The authors analyzed deep seismic sections and constructed energy dissipation graphs along transects crossing the geodivider and its western wing. The analysis and the graphs show the predomination of left-lateral NW-striking slips in the north, thrusts to the east and southeast in the center, and right-lateral NE-striking slips in the south. The total seismic energy increases constantly to the west. In the central and northern segments of the geodivider’s central part and west of it, horizontal blocks displacements cause a direct influence on seismicity level increasing and changes in geodynamic regimes within the investigated territory of Central Asia. Changes in the horizontal displacement vector are accompanied by the change of tectonic strain regimes. Increased heat flow values to the east from the geodivider within the East Asian transit zone are probably related to the change of the geodynamic regimes in the same direction under the influence of the submerged Pacific slab. The data obtained by the Chinese and Russian researchers confirm delamination (stratification) processes in the Southeast Tibet crust during its interaction with the colder and thicker lithosphere of Southeast China, and displacement of its upper layers to the southeast and south, as we supposed in our earlier publications.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>геодинамический режим</kwd><kwd>геораздел</kwd><kwd>транзитная зона</kwd><kwd>блок</kwd><kwd>межблоковая зона</kwd><kwd>сейсмичность</kwd><kwd>сейсмическая энергия</kwd><kwd>тепловой поток</kwd><kwd>геофизическое по ле</kwd><kwd>томография литосферы</kwd></kwd-group><kwd-group xml:lang="en"><kwd>geodynamic regime</kwd><kwd>geodivider</kwd><kwd>transitional zone</kwd><kwd>block</kwd><kwd>interblock zone</kwd><kwd>seismicity</kwd><kwd>seismic energy</kwd><kwd>heat flow</kwd><kwd>geophysical field</kwd><kwd>lithosphere tomography</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Проведенное исследование выполнено в рамках темы государственного задания АААА-А19-119011490127-6 и при поддержке РФФИ (проект № 18-05-00160).</funding-statement><funding-statement xml:lang="en">The study was carried out under the state assignment АААА-А19-119011490127-6 and supported by RFBR (Project 18-05-00160).</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">Bonvalot S., Balmino G., Briais A., Kuhn M., Peyrefitte A., Vales N., Biancale R., Gabalda G., Moreaux G., Reinquin F., Sarrailh M., 2012. 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