<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-1971</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Типизация карстового рельефа</article-title><trans-title-group xml:lang="en"><trans-title>Typisation of karst topography</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>Цыкин</surname><given-names>Р. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Tsykin</surname><given-names>R. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Красноярский институт цветных металлов</institution><country>USSR</country></aff><pub-date pub-type="collection"><year>1979</year></pub-date><pub-date pub-type="epub"><day>19</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>22</fpage><lpage>27</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Цыкин Р.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Цыкин Р.А.</copyright-holder><copyright-holder xml:lang="en">Tsykin R.A.</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/1971">https://geomorphology.igras.ru/jour/article/view/1971</self-uri><abstract><p>Выделяются голый, задернованный, покрытый, погребенный и бронированный карст, указывается на наличие переходных типов. Рассмотрены морфологические и генетические особенности каждого из типов карета и некоторые вопросы терминологии.</p></abstract><trans-abstract xml:lang="en"><p>The karst with naked surface of limestones is proved to result from degradation of the karst covered with vegetation. Within the limits of the latter besides sod cover loose deposits often can be found filling individual narrow wedge-like depressions. Covered karst is a type of karst topography which develops under loose mantle, the latter compensate for chemical erosion and determine formation of «karstogenous» aggradations surfaces. Buried karst is covered with thick series of younger deposits. «Armoured» karst develops under solid volcanic or unsalable sedimentary rocks within zone of erosional cuts influence. There are also some transitional types between those discussed above, as well as fluvial-karstic forms.</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>
