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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">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.15356/0435-4281-2012-1-81-91</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-569</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>ОРОГРАФИЯ КОРЕННОГО РЕЛЬЕФА РАЙОНА ПОДЛЕДНИКОВОГО ОЗЕРА ВОСТОК (ВОСТОЧНАЯ АНТАРКТИДА)</article-title><trans-title-group xml:lang="en"><trans-title>OROGRAPHY OF THE BEDROCK RELIEF OF SUBGLACIAL LAKE VOSTOK AND ITS VICINITY (EAST ANTARCTIC)</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>Попов</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Popov</surname><given-names>S. V.</given-names></name></name-alternatives><email xlink:type="simple">root@polarex.spb.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>Лунев</surname><given-names>П. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Lunev</surname><given-names>P. I.</given-names></name></name-alternatives><email xlink:type="simple">root@polarex.spb.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Полярная Морская Геологоразведочная Экспедиция, Санкт-Петербург</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Polar Marine Geosurvey Expedition, Saint Petersburg</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2012</year></pub-date><pub-date pub-type="epub"><day>22</day><month>07</month><year>2015</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>81</fpage><lpage>91</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Попов С.В., Лунев П.И., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Попов С.В., Лунев П.И.</copyright-holder><copyright-holder xml:lang="en">Popov S.V., Lunev P.I.</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://geomorphology.igras.ru/jour/article/view/569">https://geomorphology.igras.ru/jour/article/view/569</self-uri><abstract><p>На основе обобщенных отечественных и зарубежных материалов по коренному рельефу района подледникового озера Восток рассмотрены особенности орографии этой территории. Выполненное районирование работы, опирающееся на комплект кондиционных карт масштаба 1: 500 000. Выявлено три региональных геоморфологических комплекса, границы которых могут простираться далеко за пределы района исследований: желоб Восток, равнина Шмидта, горы Комсомольские. Они, в свою очередь, подразделяются, на ряд комплексов экзогенных форм мезорельефа, отличающиеся высотным положением, степенью вертикальной расчлененности, а также общим типом формы.</p></abstract><trans-abstract xml:lang="en"><p>On the base of topographic maps of 1 : 500 000 scale the regionalization of the territory was fulfilled. Three geomorphic regions were distinguished: 1 – the Vostok trench – submarine hilly plain –900 m below sea level, with several depressions and elevations; 2 – the Komsomolski mountains up to 1580 m a.s.l.; 3 – the Shmidt plain about 300 m a.s.l. and relief about 100 m. These regions are complicated with exogenic meso-landforms different in height, depth of dissection and general morphology. </p></trans-abstract><kwd-group xml:lang="ru"><kwd>озеро Восток</kwd><kwd>Антарктида</kwd><kwd>коренной рельеф</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Antarctic</kwd><kwd>geomorphic subdivision</kwd><kwd>topographic maps</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">Ridley J.K., Cudlip W., Laxon W. Identifi cation of subglacial lakes using ERS–1 radar altimeter // Journ. Glaciol. 1993. V. 73. № 133. P. 625–634.</mixed-citation><mixed-citation xml:lang="en">Ridley J.K., Cudlip W., Laxon W. Identification of subglacial lakes using ERS–1 radar altimeter.  Journ. 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