The phenomenon of gas trails in Bennett Island

Eruptions of strong gas plumes near the Bennett Island (Arctic, Russia, De Long Archipelago) observed during 1973-1986 were studied on the base of complex field and laboratory works. The site of probable sources has been found as presented by submarine cones of presumably basaltic outflows dated as...

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Дата:2013
Автори: Masurenkov, Yu. P., Sobiesevich, A. L., Petrova, V. V., Slezin, Yu. B., Shuvalov, R. A.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116327
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1163272020-10-07T12:01:09Z The phenomenon of gas trails in Bennett Island Masurenkov, Yu. P. Sobiesevich, A. L. Petrova, V. V. Slezin, Yu. B. Shuvalov, R. A. Eruptions of strong gas plumes near the Bennett Island (Arctic, Russia, De Long Archipelago) observed during 1973-1986 were studied on the base of complex field and laboratory works. The site of probable sources has been found as presented by submarine cones of presumably basaltic outflows dated as a period from 1974 to 1983. Iron-manganese nodules picked up near the cones are hydrothermal products. Rhythmic character of gas explosions is comparable with the change of the Earth rotation velocity and similar to rhythm of volcanic process and the strength of eruptions is adequate to average strength of basalt cones production. The volcanic hypothesis of the Bennett gas plumes origin, expressed before, is confirmed. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116327 10.24028/gzh.0203-3100.v35i1.2013.116327 Geofizicheskiy Zhurnal; Vol. 35 No. 1 (2013); 27-45 Геофизический журнал; Том 35 № 1 (2013); 27-45 Геофізичний журнал; Том 35 № 1 (2013); 27-45 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116327/110388 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Masurenkov, Yu. P.
Sobiesevich, A. L.
Petrova, V. V.
Slezin, Yu. B.
Shuvalov, R. A.
spellingShingle Masurenkov, Yu. P.
Sobiesevich, A. L.
Petrova, V. V.
Slezin, Yu. B.
Shuvalov, R. A.
The phenomenon of gas trails in Bennett Island
author_facet Masurenkov, Yu. P.
Sobiesevich, A. L.
Petrova, V. V.
Slezin, Yu. B.
Shuvalov, R. A.
author_sort Masurenkov, Yu. P.
title The phenomenon of gas trails in Bennett Island
title_short The phenomenon of gas trails in Bennett Island
title_full The phenomenon of gas trails in Bennett Island
title_fullStr The phenomenon of gas trails in Bennett Island
title_full_unstemmed The phenomenon of gas trails in Bennett Island
title_sort phenomenon of gas trails in bennett island
description Eruptions of strong gas plumes near the Bennett Island (Arctic, Russia, De Long Archipelago) observed during 1973-1986 were studied on the base of complex field and laboratory works. The site of probable sources has been found as presented by submarine cones of presumably basaltic outflows dated as a period from 1974 to 1983. Iron-manganese nodules picked up near the cones are hydrothermal products. Rhythmic character of gas explosions is comparable with the change of the Earth rotation velocity and similar to rhythm of volcanic process and the strength of eruptions is adequate to average strength of basalt cones production. The volcanic hypothesis of the Bennett gas plumes origin, expressed before, is confirmed.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2013
url https://journals.uran.ua/geofizicheskiy/article/view/116327
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first_indexed 2024-04-21T19:40:41Z
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