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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-2012-3-4-0078</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-169</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>ФЛЮИДОДИНАМИЧЕСКИЕ ПРОЦЕССЫ В ЗОНЕ ЦЕНТРАЛЬНОСАХАЛИНСКОГО РАЗЛОМА (ПО РЕЗУЛЬТАТАМ НАБЛЮДЕНИЙ НА ЮЖНО-САХАЛИНСКОМ ГРЯЗЕВОМ ВУЛКАНЕ)</article-title><trans-title-group xml:lang="en"><trans-title>FLUID DYNAMICS PROCESSES AT THE CENTRAL SAKHALIN FAULT (BASED ON OBSERVATIONS OF THE YUZHNO-SAKHALINSK MUD VOLCANO)</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>Ершов</surname><given-names>Валерий Валерьевич</given-names></name><name name-style="western" xml:lang="en"><surname>Ershov</surname><given-names>Valery V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>научный сотрудник,</p><p>693022, Южно-Сахалинск, ул. Науки, 1Б</p></bio><bio xml:lang="en"><p>Researcher,</p><p>1B Nauki street, Yuzhno-Sakhalinsk 693022</p></bio><email xlink:type="simple">ershov@imgg.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт морской геологии и геофизики ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Marine Geology and Geophysics, Far East Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2012</year></pub-date><pub-date pub-type="epub"><day>01</day><month>10</month><year>2015</year></pub-date><volume>3</volume><issue>4</issue><fpage>345</fpage><lpage>360</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ершов В.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Ершов В.В.</copyright-holder><copyright-holder xml:lang="en">Ershov V.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/169">https://www.gt-crust.ru/jour/article/view/169</self-uri><abstract><p>Проанализированы результаты мониторинга дебита, химического и изотопного состава свободных газов, температуры и элементного состава водогрязевой смеси в грифонах на Южно-Сахалинском грязевом вулкане. Данный вулкан приурочен к Центрально-Сахалинскому взбросо-надвигу – одной из самых крупных дизъюнктивных дислокаций о. Сахалин. Наблюдения выполнены в полевые сезоны 2005–2007 гг., которые  характеризовались различной сейсмической активностью южной части о. Сахалин. В результате нами установлены проявления Горнозаводского землетрясения 17 (18) августа 2006 г. и Невельского землетрясения 2 августа 2007 г. в грифонной деятельности Южно-Сахалинского грязевого вулкана. Данные натурных наблюдений, а также математического моделирования свидетельствуют о том, что дополнительный подток глубинных геофлюидов не мог быть основной причиной активизации вулкана после землетрясений. По нашему мнению, весь комплекс наблюдаемых аномалий объясняется взаимодействием «вода–порода–газ» в верхней части подводящего канала грязевого вулкана. Потоки воды и газа в канале вулкана, а также вмещающие алюмосиликатные породы образуют специфическую геохимическую систему, которая является чувствительной к внешним (сейсмическим) воздействиям. Следовательно, для корректной интерпретации эмпирических данных следует более полно учитывать физико-химические процессы, которые протекают внутри флюидодинамических систем.</p></abstract><trans-abstract xml:lang="en"><p>The Yuzhno-Sakhalinsk mud volcano is located in the southern part of the Sakhalin Island within the area of the Central Sakhalin fault, one of the largest disjunctive dislocations of the island. The volcano was monitored during field seasons in the period from 2005 to 2007, and data on flow rates, chemical and isotope compositions of gases, temperature and chemical composition of watermud mixture in the volcano’s blowouts were collected and analysed. During the observation period, seismic activity in the region under study was significantly variable in time and space. The monitoring results revealed «traces» of two earthquakes in the blowout activity of the Yuzhno-Sakhalinsk mud volcano – the Gornazavodsk earthquake, that took place on 17 (18) August 2006, and the Nevelsk earthquake of 2 August 2007. Based on results of our analyses of the field data and mathematical simulation data, it is possible to conclude that an additional inflow of «deep geofluids» could not have been a major trigger of the activity of the volcano after the earthquakes. In our opinion, all the observed anomalies may result from «water – rock – gas» interactions in the top part of the mud volcano’s feeder channel. A combination of water and gas flows in the volcano’s channel and silica-alumina rocks comprises a specific geochemical system that is sensitive to external (seismic) impacts. Therefore, comprehensive consideration of physical and chemical processes within fluid-dynamic systems is required for assurance of correct interpretation of empirical data.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>грязевые вулканы</kwd><kwd>геофлюиды</kwd><kwd>вещественный состав</kwd><kwd>динамика</kwd><kwd>о. Сахалин</kwd><kwd>сейсмичность</kwd><kwd>мониторинг</kwd><kwd>математическое моделирование</kwd></kwd-group><kwd-group xml:lang="en"><kwd>mud volcanoes</kwd><kwd>geofluids</kwd><kwd>material composition</kwd><kwd>dynamics</kwd><kwd>Sakhalin Island</kwd><kwd>seismicity</kwd><kwd>monitoring</kwd><kwd>mathematical modelling</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">Aliev Ad.A., 2006. Mud volcanism of the South Caspian basin. Geologiya i poleznye iskopaemye Mirovogo okeana 3, 35–51 (in Russian) [Алиев Ад.А. 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