Ages of active volcanoes in the Kuril-Kamchatka region
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dc.contributor.author | Braitseva O.A. | |
dc.contributor.author | Melekestsev I.V. | |
dc.contributor.author | Ponomareva V.V. | |
dc.contributor.author | Sulerzhitskiy L.D. | |
dc.contributor.author | Litasova S.N. | |
dc.date.accessioned | 2019-08-29T10:27:31Z | |
dc.date.available | 2019-08-29T10:27:31Z | |
dc.date.issued | 1995 | |
dc.identifier | http://repo.kscnet.ru/1111/ | |
dc.identifier.citation | Braitseva O.A., Melekestsev I.V., Ponomareva V.V., Sulerzhitskiy L.D., Litasova S.N. (1995) Ages of active volcanoes in the Kuril-Kamchatka region // Volcanology and Seismology. Vol. 16, No. 4-5. pp. 341-369. | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/4355 | |
dc.description.abstract | The births (ages) of most of the active volcanoes, calderas, and large craters produced by caldera-resembling eruptions (subcaldera craters) were dated as a result of geological, geomorphological, tephrochronological, and isotopic studies. The dated active volcanoes were found to be fairly young formations, the age of the oldest being 40-50 thousand years. Most of the presently highly active volcanoes had been born at the very end of the late Pleistocene or during the Holocene. Carbon-14 ages were determined for the majority of the Holocene volcanoes. The periods of time when Holocene volcanoes had been synchronously active were 7500-7800 and 1300-1800 years ago. -from Journal summary | |
dc.language.iso | en | |
dc.subject | 38.37.25 Вулканология | |
dc.title | Ages of active volcanoes in the Kuril-Kamchatka region | |
dc.type | Статья |
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