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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-2256</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>Опыт геоморфологической интерпретации космических многозональных изображений равнин (на примере Среднерусской возвышенности)</article-title><trans-title-group xml:lang="en"><trans-title>An attempt of geomorphological interpretation of space multi-zonal images of plain areas (a case study of Middle Russian Plain)</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>Асоян</surname><given-names>Д. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Asoyan</surname><given-names>D. S.</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 АН СССР</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1981</year></pub-date><pub-date pub-type="epub"><day>08</day><month>09</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>50</fpage><lpage>56</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Асоян Д.С., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Асоян Д.С.</copyright-holder><copyright-holder xml:lang="en">Asoyan D.S.</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/2256">https://geomorphology.igras.ru/jour/article/view/2256</self-uri><abstract><p>To study plain topography of the forest-steppe zone the space are most efficient which have been taken in spring in near field of the infra-red spectral band. The images analysis as well as the routine structural-geomorphological surface studies revealed new data on river valley features, supposed fault lines, local structures like swells, domes, depressions, isometric block morphostructures, and allows to forecast neotectonic movements of the morphostructures.</p></abstract><trans-abstract xml:lang="en"><p>To study plain topography of the forest-steppe zone the space are most efficient which have been taken in spring in near field of the infra-red spectral band. The images analysis as well as the routine structural-geomorphological surface studies revealed new data on river valley features, supposed fault lines, local structures like swells, domes, depressions, isometric block morphostructures, and allows to forecast neotectonic movements of the morphostructures.</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>
