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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-3366</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>Влияние русловых процессов на механизм формирования аллювиальных россыпей в долинах средних порядков</article-title><trans-title-group xml:lang="en"><trans-title>Hydrodynamic control over the mechanism of alluvial placers formation in the medium order valleys</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>Хмелева</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Khmeleva</surname><given-names>N. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Виноградова</surname><given-names>О. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Vinogradova</surname><given-names>O. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Маорс</surname><given-names>Л. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Maors</surname><given-names>L. V.</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>Московский государственный университет имени М.В. Ломоносова, географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1996</year></pub-date><pub-date pub-type="epub"><day>26</day><month>10</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>102</fpage><lpage>107</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хмелева Н.В., Виноградова О.В., Маорс Л.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Хмелева Н.В., Виноградова О.В., Маорс Л.В.</copyright-holder><copyright-holder xml:lang="en">Khmeleva N.V., Vinogradova O.V., Maors L.V.</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/3366">https://geomorphology.igras.ru/jour/article/view/3366</self-uri><abstract><p>Hydrodynamic conditions, type of river channel and erosional sculpture of bedrock control the mechanism of formation of genetic metal concentrations. Laboratory studies indicated different distance of transportation for metal particles different in size. The latter depends on the stream order and its hydrodynamic indices. The regularities revealed permit to increase the efficiency of prospecting.</p></abstract><trans-abstract xml:lang="en"><p>Hydrodynamic conditions, type of river channel and erosional sculpture of bedrock control the mechanism of formation of genetic metal concentrations. Laboratory studies indicated different distance of transportation for metal particles different in size. The latter depends on the stream order and its hydrodynamic indices. The regularities revealed permit to increase the efficiency of prospecting.</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>
