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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-2019-10-1-0404</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-769</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>ГЛОБАЛЬНАЯ ЭНДОДРЕНАЖНАЯ СИСТЕМА: НЕКОТОРЫЕ ФЛЮИДОФИЗИЧЕСКИЕ МЕХАНИЗМЫ ГЕОДИНАМИЧЕСКИХ ПРОЦЕССОВ</article-title><trans-title-group xml:lang="en"><trans-title>THE GLOBAL ENDODRAINAGE SYSTEM: SOME FLUID-PHYSICAL MECHANISMS OF GEODYNAMIC PROCESSES</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>Вартанян</surname><given-names>Г. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Vartanyan</surname><given-names>G. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Генрих Сенекеримович Вартанян - доктор геолого-минералогических наук, профессор</p><p>2-217 Valhalla Inn Rd. Toronto, Ontario M9B 6C3</p></bio><bio xml:lang="en"><p>Genrikh S. Vartanyan - Doctor of Geology and Mineralogy, Professor</p><p>2-217 Valhalla Inn Rd. Toronto, Ontario M9B 6C3</p></bio><email xlink:type="simple">gayanav@hotmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Lithosphere Strain Kinetics Inc.</institution><country>Канада</country></aff><aff xml:lang="en"><institution>Lithosphere Strain Kinetics Inc.</institution><country>Canada</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>21</day><month>03</month><year>2019</year></pub-date><volume>10</volume><issue>1</issue><fpage>53</fpage><lpage>78</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Вартанян Г.С., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Вартанян Г.С.</copyright-holder><copyright-holder xml:lang="en">Vartanyan G.S.</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/769">https://www.gt-crust.ru/jour/article/view/769</self-uri><abstract><p>В статье рассматриваются основные результаты более чем сорокалетних исследований гидрогеодеформационного поля, которые позволили установить некоторые новые свойства литосферных толщ, особенно четко проявленные в периоды скоротечной геодинамической активизации. Эти процессы контрастно прослеживаются в пределах планетарной мегаструктуры – глобальной эндодренажной системы (ГЭДС) Земли. Предлагаются к обсуждению представления об условиях формирования, специфических особенностях функционирования и роли астеносферы как важнейшего элемента ГЭДС.Показана доминантная роль флюидных процессов, которые в пределах ГЭДС обеспечивают условия «созревания» геодинамических катастроф. Рассматриваются особенности формирования деформационных возмущений и господствующие направления планетарной миграции деформационных импульсов от мест будущей сейсмической катастрофы вдоль ГЭДС. Излагаются результаты регионального гидрогеодеформационного (ГГД) мониторинга, свидетельствующие о тесной связи литосферных массивов в удаленных друг от друга регионах Земли: сигналы-реплики вдоль протяженности ГЭДС повторяют первоначальный импульс, зародившийся в регионе будущего сейсмического события. Рассматриваются триггерные эффекты, вызывающие срыв сейсмической энергии на большом удалении и в некоторых случаях способные вызвать каскад землетрясений. Предлагается создание системы ГГД-мониторинга крупных сейсмоопасных регионов Земли.</p></abstract><trans-abstract xml:lang="en"><p>The article presents the main results of more than forty-year studies of the hydrogeodeformation field. We have establish some new properties of lithospheric massifs, which are clearly detectable during the periods of fast geodynamic activation (FGeDA). These processes are contrastingly manifested within the planetary megastructure – the Global Endodrainage System (GEDS) of the Earth. The article discusses ideas about the conditions of formation, the specific features of functioning and the role of the asthenosphere as an essential element of the GEDS. It shows the dominant role of fluid processes that take place in the GEDS and provide the conditions for the ‘maturation’ of geodynamic catastrophes. The features of the formation of deformation disturbances and the dominant directions of the planetary migration of deformation impulses from the places of future catastrophic seismic events along the GEDS are considered. The regional hydrogeodeformation monitoring (HDGM) results give evidence of a close relationship between the lithospheric massifs in distant regions of the Earth: replica signals along the GDES length repeat an initial impulse originating from the area of a future seismic event. Attention is given to trigger effects that cause a seismic energy discharge at a large distance and, in some cases, can cause a cascade of earthquakes. It is proposed to create a HDGM system for monitoring of large seismic regions of the Earth.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>глобальная эндодренажная система</kwd><kwd>флюидосфера Земли</kwd><kwd>региональная гидрогеодеформатика</kwd><kwd>ГГД-поле Земли</kwd><kwd>гидрогеодеформационный мониторинг</kwd><kwd>землетрясение</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Global Endodrainage System (GEDS)</kwd><kwd>Earth fluidosphere</kwd><kwd>regional hydrogeodeformatics</kwd><kwd>HGD field of the Earth</kwd><kwd>hydrogeodeformation monitoring</kwd><kwd>earthquake</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">Авдалович В.С. Канандинская вулкано-тектоническая структура в юго-восточной части Тунгусской синеклизы // Вестник Московского университета. Серия 4: Геология. 1972. № 5. С. 95–99.</mixed-citation><mixed-citation xml:lang="en">Avdalovich V.S., 1972. 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