gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2019-10-3-0443gtcrust-901Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSИСПОЛЬЗОВАНИЕ СРАВНИТЕЛЬНОГО АНАЛИЗА РАСПРОСТРАНЕНИЯ И ПРОИСХОЖДЕНИЯ КАЛЬДЕР С БАЗАЛЬТ-АНДЕЗИТОВЫМ СОСТАВОМ МАГМ ДЛЯ ИЗУЧЕНИЯ ГЕНЕЗИСА МИОЦЕНОВЫХ ИГНИМБРИТОВ ВОСТОЧНОГО ВУЛКАНИЧЕСКОГО ПОЯСА КАМЧАТКИTHE ANALYSIS OF SPATIAL DISTRIBUTIONS, ORIGINS OF CALDERA-FORMING ERUPTIONS WITH BASALTIC-ANDESITIC MAGMA COMPOSITIONS, AND GENESIS OF MIOCENE IGNIMBRITES OF THE EASTERN VOLCANIC BELT, KAMCHATKAhttps://orcid.org/0000-0003-0079-507XБергаль-КувикасО. В.Bergal-KuvikasO. V.

Бергаль-Кувикас Ольга Валерьевна - PhD, старший научный сотрудник.

683006, Петропавловск-Камчатский, бульвар Пийпа, 9; 119017, Москва, Старомонетный пер., 35, строение 2.

Olga V. Bergal-Kuvikas - PhD, Senior Researcher.

9 Piip Boulevard, Petropavlovsk-Kamchatsky 683006; 35 Staromonetnyi per., building 2, Moscow 109017.

kuvikas@mail.ruhttps://orcid.org/0000-0001-5736-1489РогозинА. Н.RogozinA. N.

Рогозин Алексей Николаевич - научный сотрудник.

683006, Петропавловск-Камчатский, бульвар Пийпа, 9.

Aleksei N. Rogozin – Researcher.

9 Piip Boulevard, Petropavlovsk-Kamchatsky 683006.

alekseiras@yandex.ruhttps://orcid.org/0000-0003-1727-5695КляпицкийЕ. С.KlyapitskyE. S.

Кляпицкий Евгений Сергеевич - младший научный сотрудник.

683006, Петропавловск-Камчатский, бульвар Пийпа, 9.

Evgenii S. Klyapitsky - Junior Researcher.

9 Piip Boulevard, Petropavlovsk-Kamchatsky 683006.

Kliapich@gmail.comИнститут вулканологии и сейсмологии ДВО РАН; Институт геологии рудных месторождений, петрографии, минералогии и геохимии РАНРоссияInstitute of Volcanology and Seismology, Far East Branch of RAS; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry of RASRussian FederationИнститут вулканологии и сейсмологии ДВО РАНРоссияInstitute of Volcanology and Seismology, Far East Branch of RASRussian Federation201915092019103815828Copyright © Бергаль-Кувикас О.В., Рогозин А.Н., Кляпицкий Е.С., 20192019Бергаль-Кувикас О.В., Рогозин А.Н., Кляпицкий Е.С.Bergal-Kuvikas O.V., Rogozin A.N., Klyapitsky E.S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/901

На основе статистической обработки базы данных Глобальной программы вулканизма (ГПВ) Смитсоновского института и опубликованных материалов представлен сравнительный анализ кальдерообразующих извержений вулканов Земли. Показаны геодинамические позиции и условия формирования кальдер с базальт-андезитовым составом магм. В основном искомые кальдеры – это щитовые вулканы. Большинство из них имеют массивные лавовые потоки, только в нескольких случаях были описаны игнимбриты с базальт-андезитовым составом магм. Объединяющими признаками происхождения базальт-андезитовых игнимбритов являются контакты горячего пирокластического потока с «внешней» водой. Палеогеодинамические реконструкции Камчатки миоценового времени и анализ материалов геологического картирования базальт-андезитовых игнимбритов Восточного вулканического пояса Камчатки подтверждают их образование в прибрежно-морской обстановке, что согласуется с приведенными результатами изучения происхождения базальт-андезитовых игнимбритов вулканов в других регионах Земли. Полученные данные показывают значимость реконструкций палеогеодинамических обстановок в изучении типов палеовулканов и рельефообразующих пирокластических пород.

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The authors declare that there are no conflicts of interest present.