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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-2018-9-2-0358</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-588</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>ДЕФОРМАЦИИ	ЗЕМНОЙ ПОВЕРХНОСТИ ОСТРОВА САХАЛИН ПО ДАННЫМ GPS‐НАБЛЮДЕНИЙ</article-title><trans-title-group xml:lang="en"><trans-title>EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA</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>Прытков</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Prytkov</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. физ.-мат. наук, в.н.с.,</p><p>693022, Южно-Сахалинск, ул. Науки, 1Б</p></bio><bio xml:lang="en"><p>Candidate of Physics and Mathematics, Lead Researcher,</p><p>1B Nauka street, Yuzhno-Sakhalinsk 693022</p></bio><email xlink:type="simple">a.prytkov@imgg.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>Василенко</surname><given-names>Н. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Vasilenko</surname><given-names>N. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. техн. наук, в.н.с.,</p><p>693022, Южно-Сахалинск, ул. Науки, 1Б</p></bio><bio xml:lang="en"><p>Candidate of Technical Sciences, Lead Researcher,</p><p>1B Nauka street, Yuzhno-Sakhalinsk 693022</p></bio><email xlink:type="simple">n.vasilenko@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>2018</year></pub-date><pub-date pub-type="epub"><day>03</day><month>07</month><year>2018</year></pub-date><volume>9</volume><issue>2</issue><fpage>503</fpage><lpage>514</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Прытков А.С., Василенко Н.Ф., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Прытков А.С., Василенко Н.Ф.</copyright-holder><copyright-holder xml:lang="en">Prytkov A.S., Vasilenko N.F.</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/588">https://www.gt-crust.ru/jour/article/view/588</self-uri><abstract><p>На основе GPS‐скоростей пунктов Сахалинской геодинамической сети выполнено моделирование деформированного состояния земной поверхности северной, центральной и южной части о. Сахалин. Полученные данные показывают сложную картину современных горизонтальных деформаций в окрестностях главных субмеридиональных разломов острова. Преобладающим деформационным режимом является сжатие островной суши, однако пространственное распределение деформаций неоднородно. Сокращение земной коры происходит в основном в субширотном и ЮЗ‐СВ направлениях. Наряду со сжатием на севере и в центре острова выделяются области достаточно интенсивных деформаций правостороннего сдвига, в юго‐восточной части острова преобладают деформации растяжения. Региональная геодинамическая обстановка находит отражение в сейсмичности острова. В районах интенсивного деформирования земной поверхности проявляется повышенная сейсмическая активность последних лет, тогда как области низких скоростей деформаций коррелируют с зонами слабой и разреженной сейсмичности.</p></abstract><trans-abstract xml:lang="en"><p>The earth surface deformation was modeled for the North, Central and South Sakhalin on the basis of de‐ formation velocities recorded by the GPS stations of the Sakhalin Geodynamical Network. A pattern of contemporary horizontal deformation is intricate in the vicinity of the main submeridional faults of the island. On the island surface, the dominant deformation regime is compression; however, the spatial distribution of deformation is heterogeneous. The horizontal compression is mainly sublatitudinal and SW‐NE‐trending. In addition to compression, there are zones of rather intense right‐lateral strike‐slip in the northern and central parts of the island, while stretching dominates in the south‐eastern parts. The regional geodynamic setting is reflected in the seismicity of the island. Recently, the seismic activity has been increased in the areas characterized by intensive surface deformation, while the areas of low deformation rates correlate with the zones of weak and sparse seismicity.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>современные движения земной коры</kwd><kwd>GPS‐наблюдения</kwd><kwd>деформация</kwd><kwd>остров Сахалин</kwd></kwd-group><kwd-group xml:lang="en"><kwd>contemporary crustal movement</kwd><kwd>GPS observations</kwd><kwd>deformation</kwd><kwd>Sakhalin Island</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">Altamimi Z., Collilieux X., Métivier L., 2011. ITRF2008: an improved solution of the international terrestrial reference frame. 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