<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-3227</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>Генетические и динамические особенности рельефа островных гор Восточной Монголии</article-title><trans-title-group xml:lang="en"><trans-title>Genetic and dynamic features of the relief of inselbergs in Eastern Mongolia</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>Чичагов</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Chichagov</surname><given-names>V. P.</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>Институт географии РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1995</year></pub-date><pub-date pub-type="epub"><day>13</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>4</issue><fpage>92</fpage><lpage>106</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чичагов В.П., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Чичагов В.П.</copyright-holder><copyright-holder xml:lang="en">Chichagov V.P.</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/3227">https://geomorphology.igras.ru/jour/article/view/3227</self-uri><abstract><p>Two types of inselbergs are recognized in Eastern Mongolia: structural, that is created by block uplifts, and erosional ones (resulted from erosional dissection of plains). Inselbergs of the first type continue to rise and involve adjacent areas of plains. The second type is erosional remnants of mountains lowered and dissected by erosion. Landforms typical of each type of inselbergs are considered, including specific debris flows and sand flows. The flows were formed in the process of irregular uplifts, probably accompanied by seismic shocks and shaking.</p></abstract><trans-abstract xml:lang="en"><p>Two types of inselbergs are recognized in Eastern Mongolia: structural, that is created by block uplifts, and erosional ones (resulted from erosional dissection of plains). Inselbergs of the first type continue to rise and involve adjacent areas of plains. The second type is erosional remnants of mountains lowered and dissected by erosion. Landforms typical of each type of inselbergs are considered, including specific debris flows and sand flows. The flows were formed in the process of irregular uplifts, probably accompanied by seismic shocks and shaking.</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>
