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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">reggeomet</journal-id><journal-title-group><journal-title xml:lang="ru">Региональная геология и металлогения</journal-title><trans-title-group xml:lang="en"><trans-title>Regional Geology and Metallogeny</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0869-7892</issn><publisher><publisher-name>(ФГБУ "Институт Карпинского")</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.52349/0869-7892_2025_101_134-152</article-id><article-id custom-type="elpub" pub-id-type="custom">reggeomet-129</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>ВЕТЕРАНЫ ГЕОЛОГИИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>VETERANS OF GEOLOGY</subject></subj-group></article-categories><title-group><article-title>Околорудные гидротермокарстовые полости</article-title><trans-title-group xml:lang="en"><trans-title>Wallrock hydrothermokarst cavities</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>Ляхницкий</surname><given-names>Ю. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Lyakhnitskiy</surname><given-names>Yu. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кандидат геолого-минералогических наук, ведущий специалист, отдел по связям с общественностью, Центр научно-методического и организационного обеспечения государственного геологического картографирования</p><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>PhD (Geology and Mineralogy), Leading Specialist, Public Relations Department Centre of Scientific-Methodological and Organizational Support of State Geological Mapping</p><p>Saint Petersburg</p></bio><email xlink:type="simple">yuri_lyahnitsky@karpinskyinstitute.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Всероссийский научно-исследовательский геологический институт им. А. П. Карпинского<country>Россия</country></aff><aff xml:lang="en">All-Russian Geological Research Institute of A. P. Karpinsky<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>12</day><month>04</month><year>2025</year></pub-date><volume>32</volume><issue>1 (101)</issue><fpage>134</fpage><lpage>152</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ляхницкий Ю.С., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Ляхницкий Ю.С.</copyright-holder><copyright-holder xml:lang="en">Lyakhnitskiy Y.S.</copyright-holder><license 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://reggeomet.elpub.ru/jour/article/view/129">https://reggeomet.elpub.ru/jour/article/view/129</self-uri><abstract><p>Статья посвящена описанию гидротермокарстовых полостей рудных месторождений. Они различаются по морфологии, генезису и положению в рудных полях. Наличие гидротермальных полостей является дополнительным поисковым признаком оруденения. Полости часто содержат уникальные минералогические агрегаты и могут служить ценными экскурсионно-туристическими объектами.</p></abstract><trans-abstract xml:lang="en"><p>The paper focuses on hydrothermokarst cavities of ore deposits. They differ in morphology, genesis, and location in ore fields. Hydrothermal cavities relate to an additional search sign of mineralization. Cavities often contain unique mineralogical aggregates and can serve as valuable sightseeing and tourist sites.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>гидротермокарст</kwd><kwd>карстовые месторождения</kwd><kwd>уникальная минерализация</kwd><kwd>музеи в природе</kwd></kwd-group><kwd-group xml:lang="en"><kwd>hydrothermokarst</kwd><kwd>karst deposits</kwd><kwd>unique mineralization</kwd><kwd>open-air museums</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Ферсман А. Е. К морфологии и геохимии Тюя-Муюна // Труды по изучению радия. Т. 3. Л. : АН СССР, 1927. 93 с.</mixed-citation><mixed-citation xml:lang="en">Fersman A. E. Morphology and geochemistry of Tyuya-Muyun. Publications on Radium. Vol. 3. Leningrad: AS USSR; 1927. 93 p. 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