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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">10.15356/0435-4281-2014-1-29-35</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-24</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>Общетеоретические статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>БЕРЕГОВАЯ ЗОНА КРУПНЫХ ВОДОХРАНИЛИЩ (СТ. 1. ОСНОВНЫЕ ЧЕРТЫ РЕЛЬЕФА)</article-title><trans-title-group xml:lang="en"><trans-title>COASTAL ZONE OF LARGE MAN-MADE LAKES (PAPER 1. COASTAL MORPHOLOGY PECULIARITIES)</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>Хабидов</surname><given-names>А. Ш.</given-names></name><name name-style="western" xml:lang="en"><surname>Khabidov</surname><given-names>А. Sh.</given-names></name></name-alternatives><email xlink:type="simple">geomorfologiya@mail.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>Жиндарев</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Zhindarev</surname><given-names>L. А.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Географический факультет</p></bio><bio xml:lang="en"><p>Geographical Department</p></bio><email xlink:type="simple">lzhindarev@yandex.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Федорова</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Fedorova</surname><given-names>Е. А.</given-names></name></name-alternatives><email xlink:type="simple">fedorova@iwep.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>Марусин</surname><given-names>К. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Marusin</surname><given-names>К. V.</given-names></name></name-alternatives><email xlink:type="simple">kat@iwep.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт водных и экологических проблем СО РАН, Барнаул</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for Water and Environmental Problems SB RAS, Barnaul</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2014</year></pub-date><pub-date pub-type="epub"><day>21</day><month>02</month><year>2015</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>29</fpage><lpage>35</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хабидов А.Ш., Жиндарев Л.А., Федорова Е.А., Марусин К.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Хабидов А.Ш., Жиндарев Л.А., Федорова Е.А., Марусин К.В.</copyright-holder><copyright-holder xml:lang="en">Khabidov А.S., Zhindarev L.А., Fedorova Е.А., Marusin К.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://geomorphology.igras.ru/jour/article/view/24">https://geomorphology.igras.ru/jour/article/view/24</self-uri><abstract><p>Особенности морфолитогенеза береговой зоны крупных водохранилищ отличны друг от друга в волновой, флювиальной и переходной зоне. При этом условия флювиального морфогенеза схожи с теми, которые наблюдаются в природе в дельтах рек. Переходная зона представляет собой постепенное замещение дельтовой обстановки на обстановку мелководных водоемов. Условия волнового морфолитогенеза водохранилищ схожи с теми, которые наблюдаются в береговой зоне моря.</p><p><ext-link xlink:href="https://www.elibrary.ru/item.asp?id=21353741" ext-link-type="uri">статья в библиотеке elibrary.ru</ext-link></p></abstract><trans-abstract xml:lang="en"><p>The peculiarities of a coastal morphology of large man-made lakes under the wave-dominated, fluvial dominated and transitional environments were discussed. It was shown that the fluvial-dominated environment is similar to the one in a river delta. In the transitional environments, the gradual replacement of delta sub-environments by shallow areas is observed. In the wave-dominated environments the relief is similar to the characteristic relief of the sea coastal zone.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>водохранилище</kwd><kwd>рельеф береговой зоны</kwd><kwd>осадконакопление</kwd><kwd>флювиальный морфолитогенез</kwd><kwd>морфолитогенез переходной зоны водоемов</kwd><kwd>волновой морфолитогенез</kwd></kwd-group><kwd-group xml:lang="en"><kwd>man-made lake</kwd><kwd>relief of coastal zone</kwd><kwd>sedimentation</kwd><kwd>fluvial morphogenesis</kwd><kwd>morphogenesis of transitional zone</kwd><kwd>wave morphogenesis</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">Авакян А.Б., Салтанкин В.П., Шарапов В.А. и др. Водохранилища мира. М.: Наука, 1979. 287 c.</mixed-citation><mixed-citation xml:lang="en">Avakyan A.B., Saltankin V.P., Sharapov V.A., etc. Vodohranilishcha mira (World man-made lakes). 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