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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-1835</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>Дискуссии</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Discussions</subject></subj-group></article-categories><title-group><article-title>Принципы и некоторые вопросы методики составления геоморфологических карт, специализированных для поисков бокситов</article-title><trans-title-group xml:lang="en"><trans-title>Principles and some methodical problems of compilation of special geomorphic maps for bauxite search</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>Селиверстов</surname><given-names>Ю. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Seliverstov</surname><given-names>Yu. 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>ВСЕГЕИ</institution><country>Россия</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>1</issue><issue-title>Геоморфология</issue-title><fpage>95</fpage><lpage>99</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Селиверстов Ю.П., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Селиверстов Ю.П.</copyright-holder><copyright-holder xml:lang="en">Seliverstov Y.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/1835">https://geomorphology.igras.ru/jour/article/view/1835</self-uri><abstract><p>Principles of special geomorphic mapping for bauxite search as introduced by V. F. Filatov, Yu. K. Loskutov and G. F. Kuznetsova need more precise definition, particularly of age and genesis of the mapped categories. Besides generate stages of planation and mantle development, it is necessary to determine precise age of denudational topography which is covered with orebearing formations. Therefore it is most important to follow the relations between the denudation relief and its hypergenic mantle formation as well as to specify their genesis.</p></abstract><trans-abstract xml:lang="en"><p>Principles of special geomorphic mapping for bauxite search as introduced by V. F. Filatov, Yu. K. Loskutov and G. F. Kuznetsova need more precise definition, particularly of age and genesis of the mapped categories. Besides generate stages of planation and mantle development, it is necessary to determine precise age of denudational topography which is covered with orebearing formations. Therefore it is most important to follow the relations between the denudation relief and its hypergenic mantle formation as well as to specify their genesis.</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>
