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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">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2023-14-5-0724</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1747</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>СОВРЕМЕННАЯ ГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RECENT GEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>АКТУАЛЬНОСТЬ ИССЛЕДОВАНИЯ ПРИБРЕЖНОГО ВУЛКАНИЧЕСКОГО КОМПЛЕКСА В КОНТЕКСТЕ ИСТОРИИ ИЗУЧЕНИЯ ЮЖНОЙ КАМЧАТКИ</article-title><trans-title-group xml:lang="en"><trans-title>THE RELEVANCE OF THE STUDY OF THE PRIBREZHNY VOLCANIC COMPLEX   IN THE CONTEXT OF THE HISTORY INVESTIGATIONS OF SOUTH KAMCHATKA</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>Бергаль-Кувикас</surname><given-names>О. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Bergal-Kuvikas</surname><given-names>O. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>683006, Петропавловск-Камчатский, б-р Пийпа, 9</p></bio><bio xml:lang="en"><p>9 Piip Blvd, Petropavlovsk-Kamchatsky 683006</p></bio><email xlink:type="simple">kuvikas@mail.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>Рогозин</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Rogozin</surname><given-names>A. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>683006, Петропавловск-Камчатский, б-р Пийпа, 9</p></bio><bio xml:lang="en"><p>9 Piip Blvd, Petropavlovsk-Kamchatsky 683006</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт вулканологии и сейсмологии ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Volcanology and Seismology, Far Eastern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>17</day><month>10</month><year>2023</year></pub-date><volume>14</volume><issue>5</issue><fpage>724</fpage><lpage>724</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Бергаль-Кувикас О.В., Рогозин А.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Бергаль-Кувикас О.В., Рогозин А.Н.</copyright-holder><copyright-holder xml:lang="en">Bergal-Kuvikas O.V., Rogozin A.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://www.gt-crust.ru/jour/article/view/1747">https://www.gt-crust.ru/jour/article/view/1747</self-uri><abstract><p>Представленная работа содержит обзор опубликованных источников информации, геологических карт и отчетов об изучении прибрежного вулканического комплекса Южной Камчатки. Прибрежный вулканический комплекс сформирован рядом сближенных вулканических массивов, протягивающихся дуговой цепью в узкой прибрежной полосе Берегового хребта от Авачинской губы до бухты Вестник. Актуальность работы связана с необходимостью пересмотра геодинамической истории формирования изучаемого региона ввиду появления обрывочных, противоречивых сведений о магматических комплексах Южной Камчатки. В публикации приводятся данные о магматических породах, вскрытых в береговых обрывах Тихоокеанского побережья Южной Камчатки. Рассмотрены представления об условиях их формирования со стороны господствовавшей в свое время теории геосинклиналей, а затем – тектоники плит. На основе проведенного обзора формулируются проблемы будущих исследований, связанные с неопределенностью границ распространения прибрежного вулканического комплекса, с неясностью временных интервалов образования комплекса, с отсутствием минералогических и изотопно-геохимических исследований магматических пород. Отдельной проблемой исследования является формирование перехода от континентальной окраины Камчатки к островной дуге Курильских островов. В работе показана актуальность изучения прибрежного вулканического комплекса Южной Камчатки и предложены возможные пути решения научных проблем. Детальное картирование зоны сочленения прибрежного вулканического комплекса Южной Камчатки и Кроноцкого террейна в районе Малко-Петропавловской зоны поперечных дислокаций позволит уточнить возраст и кинематику их взаимоотношений. Определение редких элементов и изотопов стронция, неодима, свинца поможет установить природу магматизма в сравнении с разновозрастными сериями вулканитов Южной Камчатки. Полученные данные будут востребованы для изучения условий магмогенерации кислого вулканизма Южной Камчатки и моногенного вулканизма МалкоПетропавловской зоны поперечных дислокаций. Палеомагнитные исследования, наряду с определениями абсолютного возраста пород, помогут реконструировать палеошироту формирования прибрежного вулканического комплекса и восстановить геодинамическую эволюцию формирования Южной Камчатки.</p></abstract><trans-abstract xml:lang="en"><p>The present paper contains a review of publications, geological maps and reports on the study of the Pribrezhny volcanic complex of South Kamchatka. The Pribrezhny volcanic complex is comprised of a number of closeset volcanic massifs stretching chain-like along the narrow coastline of the Beregovoy ridge from the Avacha Bay to the Vestnik Bay. The relevance of the work is related to the necessity of revising the geodynamic history of formation of the study area which stems from emergence of some fragmentary, contradictory information about magmatic complexes of South Kamchatka. The paper presents the data on magmatic rocks penetrated in the coastal cliffs of South Kamchatka. Consideration is being given to their formation conditions in the context of a once-popular theory of geosynclines and in that of plate tectonics. Based on the review, several open research problems are formulated concerning the undetermined propagation limits of the Pribrezhny volcanic complex and unknown time intervals of its formation, and the lack of mineralogical and isotopic-geochemical studies of magmatic rocks. A separate research problem is the formation of transitional zone between the continental margin of Kamchatka and the Kuril Island Arc. The paper shows the relevance of the study of the Pribrezhny volcanic complex of South Kamchatka and proposes possible solutions to the research problems. A detailed mapping of the junction zone of Pribrezhny volcanic complex of South Kamchatka and the Kronotsky terrain near the Malko-Petropavlovsk zone of transverse dislocations will make it possible to refine the age and kinematics of their relationship. Determination of rare elements and strontium, neodymium and lead isotopes will provide a possibility to clarify the nature of magmatism as compared to heterochronous volcanic series of South Kamchatka. The data obtained will be needed to study magmogeneration conditions for acid volcanism of South Kamchatka and monogenic volcanism of the Malko-Petropavlovsk zone of transverse dislocations. The paleomagnetic studies, along with dating of rock absolute age, will help to reconstruct the paleolatitude of formation of the Pribrezhny volcanic complex and to restore the geodynamic evolution of formation of South Kamchatka.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>миоцен</kwd><kwd>Южная Камчатка</kwd><kwd>обзор</kwd><kwd>магматические породы</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Miocene</kwd><kwd>Southern Kamchatka</kwd><kwd>review</kwd><kwd>magmatic rocks</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при поддержке Российского научного фонда, грант № 22-77-10019 (https://rscf.ru/project/22-77-10019/).</funding-statement><funding-statement xml:lang="en">The research was supported by the Russian Science Foundation, grant 22-77-10019 (https://rscf.ru/ project/22-77-10019/).</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">Апрелков С.Е. 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