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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-3008</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>К проблеме аэрокосмической индикации геодинамики рельефа областей древнематерикового оледенеиия</article-title><trans-title-group xml:lang="en"><trans-title>On the problem of the relief's geodynamics indication within areas of ancient ice sheets using aerial and space methods</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>Губин</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Gubin</surname><given-names>V. N.</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>Белорусский научно-исследовательский геологоразведочный институт</institution><country>Беларусь</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1992</year></pub-date><pub-date pub-type="epub"><day>25</day><month>01</month><year>2023</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>72</fpage><lpage>77</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Губин В.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Губин В.Н.</copyright-holder><copyright-holder xml:lang="en">Gubin V.N.</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/3008">https://geomorphology.igras.ru/jour/article/view/3008</self-uri><abstract><p>Geoindicational features are considered which have been used in the study of relief endogenous dynamic in a formerly glaciated region using aerial and space technique. It has been inferred that the nature of geodynamic manifestations on the remote sensing materials is controlled by the neotectonic movements (endogenous and rotational) of the Earth's crust, heterogeneities of the geophysical field, activation of geochemical processes as well as by the glaciodynamic events.</p></abstract><trans-abstract xml:lang="en"><p>Geoindicational features are considered which have been used in the study of relief endogenous dynamic in a formerly glaciated region using aerial and space technique. It has been inferred that the nature of geodynamic manifestations on the remote sensing materials is controlled by the neotectonic movements (endogenous and rotational) of the Earth's crust, heterogeneities of the geophysical field, activation of geochemical processes as well as by the glaciodynamic events.</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>
