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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 pub-id-type="doi">10.15356/0435-4281-1970-2-65-70</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-848</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>ПАЛЕОКАРСТ РАННЕПЕРМСКОЙ СУШИ НА ТЕРРИТОРИИ ТАТАРСКОЙ АССР</article-title><trans-title-group xml:lang="en"><trans-title>PALEOKARST OF THE EARLY PERMIAN PERIOD ON THE TERRITORY OF THE TATAR ASSR</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>Каштанов</surname><given-names>С. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Kashtanov</surname><given-names>S. G.</given-names></name></name-alternatives><email xlink:type="simple">geomorfologiya@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Казанский государственный университет им. В.И. Ульянова-Ленина</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V. I. Ulyanov-Lenin Kazan State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1970</year></pub-date><pub-date pub-type="epub"><day>18</day><month>08</month><year>2016</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>65</fpage><lpage>70</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Каштанов С.Г., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Каштанов С.Г.</copyright-holder><copyright-holder xml:lang="en">Kashtanov S.G.</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/848">https://geomorphology.igras.ru/jour/article/view/848</self-uri><abstract><p>Со времени своего появления поверхность Раннего пермского времени подвергалась интенсивным процессам денудации. Карст лучше всего проявлен в областях развития коры выветривания.</p></abstract><trans-abstract xml:lang="en"><p>Since the time of its emergence the Early Permian land has been exposed to the processes of intensive denudation. Karst is best manifested in the areas of development of the weathering crust.</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>
