SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE
Model to explain the crater formation at the Yamal Peninsula and methane release on the Bennett Island is proposed. The reason causing these phenomena consists in the shock wave impact on permafrost gas hydrates deposits. Gas hydrates break up as the shock wave of an earthquake on an icequake common...
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ftdoajarticles:oai:doaj.org/article:a556c98c580c463cb80377f7f13cbdf0 2023-05-15T15:42:01+02:00 SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE V.V. Kuznetsov 2018-04-01T00:00:00Z https://doi.org/10.18454/2079-6641-2018-21-1-117-130 https://doaj.org/article/a556c98c580c463cb80377f7f13cbdf0 EN RU eng rus KamGU by Vitus Bering http://krasec.ru/wp-content/uploads/2018/04/Kuznetsov.pdf https://doaj.org/toc/2079-6641 https://doaj.org/toc/2079-665X doi:10.18454/2079-6641-2018-21-1-117-130 2079-6641 2079-665X https://doaj.org/article/a556c98c580c463cb80377f7f13cbdf0 Vestnik KRAUNC: Fiziko-Matematičeskie Nauki, Iss 1(21), Pp 117-130 (2018) gas hydrates methane release earthquake Science Q article 2018 ftdoajarticles https://doi.org/10.18454/2079-6641-2018-21-1-117-130 2022-12-30T22:01:30Z Model to explain the crater formation at the Yamal Peninsula and methane release on the Bennett Island is proposed. The reason causing these phenomena consists in the shock wave impact on permafrost gas hydrates deposits. Gas hydrates break up as the shock wave of an earthquake on an icequake common in their deposits area passes through them. Origin of crater or volcano formation on the Bennett Island appears to need a series of earthquakes (shock waves). Article in Journal/Newspaper Bennett Island permafrost Yamal Peninsula Directory of Open Access Journals: DOAJ Articles Yamal Peninsula ENVELOPE(69.873,69.873,70.816,70.816) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
gas hydrates methane release earthquake Science Q |
spellingShingle |
gas hydrates methane release earthquake Science Q V.V. Kuznetsov SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
topic_facet |
gas hydrates methane release earthquake Science Q |
description |
Model to explain the crater formation at the Yamal Peninsula and methane release on the Bennett Island is proposed. The reason causing these phenomena consists in the shock wave impact on permafrost gas hydrates deposits. Gas hydrates break up as the shock wave of an earthquake on an icequake common in their deposits area passes through them. Origin of crater or volcano formation on the Bennett Island appears to need a series of earthquakes (shock waves). |
format |
Article in Journal/Newspaper |
author |
V.V. Kuznetsov |
author_facet |
V.V. Kuznetsov |
author_sort |
V.V. Kuznetsov |
title |
SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
title_short |
SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
title_full |
SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
title_fullStr |
SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
title_full_unstemmed |
SHOCK WAVE MODEL OF THE CRATER FORMATION AND OTHER CAUSES OF EXPLOSIVE METHANE RELEASE |
title_sort |
shock wave model of the crater formation and other causes of explosive methane release |
publisher |
KamGU by Vitus Bering |
publishDate |
2018 |
url |
https://doi.org/10.18454/2079-6641-2018-21-1-117-130 https://doaj.org/article/a556c98c580c463cb80377f7f13cbdf0 |
long_lat |
ENVELOPE(69.873,69.873,70.816,70.816) |
geographic |
Yamal Peninsula |
geographic_facet |
Yamal Peninsula |
genre |
Bennett Island permafrost Yamal Peninsula |
genre_facet |
Bennett Island permafrost Yamal Peninsula |
op_source |
Vestnik KRAUNC: Fiziko-Matematičeskie Nauki, Iss 1(21), Pp 117-130 (2018) |
op_relation |
http://krasec.ru/wp-content/uploads/2018/04/Kuznetsov.pdf https://doaj.org/toc/2079-6641 https://doaj.org/toc/2079-665X doi:10.18454/2079-6641-2018-21-1-117-130 2079-6641 2079-665X https://doaj.org/article/a556c98c580c463cb80377f7f13cbdf0 |
op_doi |
https://doi.org/10.18454/2079-6641-2018-21-1-117-130 |
_version_ |
1766374891396792320 |