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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 custom-type="elpub" pub-id-type="custom">geomorf-1848</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>Развитие новейшей структуры Западной Камчатки</article-title><trans-title-group xml:lang="en"><trans-title>Development of neotectonic structures of Western Kamchatka</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>Кривулин</surname><given-names>К. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Krivulin</surname><given-names>K. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Свиточ</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Svitoch</surname><given-names>A. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>СССР</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1977</year></pub-date><pub-date pub-type="epub"><day>06</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>79</fpage><lpage>84</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кривулин К.П., Свиточ А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Кривулин К.П., Свиточ А.А.</copyright-holder><copyright-holder xml:lang="en">Krivulin K.P., Svitoch A.A.</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/1848">https://geomorphology.igras.ru/jour/article/view/1848</self-uri><abstract><p>Neotectonic development of Western Kamchatka does not show direct inheritance from the Bolsheretskaya depression structure. Neotectonic structure of the region is characterized with differentiated movements within separate zones. Internal and northern parts of Western Kamchatka underwent to a slow uplift controlled by uplift of Central Kamchatka mountain ridges. Maritime zone adjacent to the descending regions of the Sea of Okhotsk was relatively stable or slightly moved downward and upward. Ancient sea terraces have not been established at Western Kamchatka with the exception of low marine surfaces (up to 20 meters) within the coastal zone.</p></abstract><trans-abstract xml:lang="en"><p>Neotectonic development of Western Kamchatka does not show direct inheritance from the Bolsheretskaya depression structure. Neotectonic structure of the region is characterized with differentiated movements within separate zones. Internal and northern parts of Western Kamchatka underwent to a slow uplift controlled by uplift of Central Kamchatka mountain ridges. Maritime zone adjacent to the descending regions of the Sea of Okhotsk was relatively stable or slightly moved downward and upward. Ancient sea terraces have not been established at Western Kamchatka with the exception of low marine surfaces (up to 20 meters) within the coastal zone.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
