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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-3537</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Складчатые горы Евразии (Статья 2. Структурные и геодинамические черты складчатого горообразования)</article-title><trans-title-group xml:lang="en"><trans-title>Fold mountains of Eurasia (Paper 2. Structural and geodynamic features of fold mountain making)</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>Уфимцев</surname><given-names>Г. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Ufimtsev</surname><given-names>G. F.</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 земной коры СО РАН, Иркутск</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1999</year></pub-date><pub-date pub-type="epub"><day>03</day><month>01</month><year>2024</year></pub-date><volume>0</volume><issue>1</issue><fpage>16</fpage><lpage>24</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Уфимцев Г.Ф., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Уфимцев Г.Ф.</copyright-holder><copyright-holder xml:lang="en">Ufimtsev G.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://geomorphology.igras.ru/jour/article/view/3537">https://geomorphology.igras.ru/jour/article/view/3537</self-uri><abstract><p>Tectonic relief of fold mountains is characterized as wells their structural ensembles, organization levels, geologic structure. Exogenous factors of fold mountain making are discussed, its general model is suggested and some considerations are proposed concerning possible combination of near-surface folding and deep tectonic. The consequent reformations of mountains and folds of Jura type are shown.</p></abstract><trans-abstract xml:lang="en"><p>Tectonic relief of fold mountains is characterized as wells their structural ensembles, organization levels, geologic structure. Exogenous factors of fold mountain making are discussed, its general model is suggested and some considerations are proposed concerning possible combination of near-surface folding and deep tectonic. The consequent reformations of mountains and folds of Jura type are shown.</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>
