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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">sergeogr</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Российской академии наук. Серия географическая</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2587-5566</issn><issn pub-type="epub">2658-6975</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31857/S2587556620050076</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-1152</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>Природные процессы и динамика геосистем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Natural Processes and Dynamics of Geosystems</subject></subj-group></article-categories><title-group><article-title>Оценка темпов палеоденудации в горах: основные подходы и результаты</article-title><trans-title-group xml:lang="en"><trans-title>Evaluation of the Paleodenudation Rates in the Mountains: Main Approaches and Results</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>Грачев</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Grachev</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Москва</p></bio><bio xml:lang="en"><p>Moscow</p></bio><email xlink:type="simple">agrachev@igras.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Голосов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Golosov</surname><given-names>V. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Географический факультет</p><p>Москва</p></bio><bio xml:lang="en"><p>Faculty of Geography</p><p>Moscow</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Geography, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт географии РАН; Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Geography, Russian Academy of Sciences; Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>06</day><month>11</month><year>2020</year></pub-date><volume>84</volume><issue>5</issue><elocation-id>704–714</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Грачев А.М., Голосов В.Н., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Грачев А.М., Голосов В.Н.</copyright-holder><copyright-holder xml:lang="en">Grachev A.M., Golosov 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://izvestia.igras.ru/jour/article/view/1152">https://izvestia.igras.ru/jour/article/view/1152</self-uri><abstract><p>В статье систематизированы методы изучения темпов современной и палеоденудации и обобщены опубликованные данные об интенсивности палеоденудации, полученные на основе использования 10Be и комплекса методов изучения озерных отложений для горных стран различных регионов мира. Показано, что в настоящее время наиболее изученными территориями в плане оценки темпов палеоденудации являются Альпы, Тибет, Скалистые горы и Анды. Скорости палеоденудации, определенные для речных и озерных водосборов в различных частях мира, изменяются в широких пределах в интервале 2–3240 м/млн лет. Аналогично закономерности, выявленной для современной денудации, прослеживается высокая корреляция между темпами палеоденудации и уклонами водосборов. Тем не менее локальные ландшафтные особенности конкретных речных бассейнов и их изменения в течение голоцена определяют пространственную вариабельность и динамику изменений темпов денудации во времени. Роль деятельности человека усиливается и приводит к 10–100-кратному усилению денудации горных стран, в первую очередь в пределах предгорно-низкогорного пояса.</p></abstract><trans-abstract xml:lang="en"><p>The article systematizes methods for studying modern and paleodenudation rates and summarizes the published data on the paleodenudation intensity obtained using 10Be and a set of methods for studying lake sediments for mountainous areas of different regions of the world. It has been shown that currently the most studied territories in terms of assessing paleodenudation rates are the European Alps, Tibet, the Rocky Mountains, and the Andes. Paleodenudation rates determined for river and lake catchments in various parts of the world vary over a wide range in the interval 2–3240 m/106 years. Similarly to the regularities revealed for modern denudation, there is a high correlation between the paleodenudation rates and the catchments slopes. Nevertheless, the local landscape features of specific river basins and their changes during the Holocene determine the spatial variability and dynamics of changes in the denudation rate over time. The role of human activity intensifies and leads to a 10 to 100-fold increase in the denudation of mountainous areas, primarily within the foothills and low mountains.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>голоцен</kwd><kwd>горы</kwd><kwd>денудация</kwd><kwd>количественные методы</kwd><kwd>озерные осадки</kwd><kwd>10Be</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Holocene</kwd><kwd>mountains</kwd><kwd>denudation</kwd><kwd>quantitative methods</kwd><kwd>lake sediments</kwd><kwd>10Be</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Раздел данной работы по &lt;sup&gt;10&lt;/sup&gt;Be подготовлен в рамках госзадания Института географии РАН 0148-2019-0005 (АААА-А19-119021990091-4). Работа над остальными разделами велась в рамках проекта РНФ №19-17-00181 “Количественная оценка бассейновой составляющей стока наносов и ее изменений в голоцене на реках Кавказа”.</funding-statement><funding-statement xml:lang="en">The section on &lt;sup&gt;10&lt;/sup&gt;Be was prepared within the framework of the state-ordered research theme of the Institute of Geography RAS, no. 0148-2019-0005. The work on remaining sections was financially supported by the Russian Science Foundation, project no. 19-17-00181 (“Quantitative Assessment of the Slope Sediment Flux and Its Changes in the Holocene for the Caucasus Mountain Rivers”).</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Мозжерин В.В. Расчленение стока взвешенных наносов рек Северной Евразии на русловую и бассейновую составляющие и его геоморфологическая интерпретация. 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