GENETIC TYPES OF METHANE FROM LAKE BAIKAL

dc.contributor.author	Kalmychkov G.V.
dc.contributor.author	Kuz'min M.I.
dc.contributor.author	Egorov A.V.
dc.contributor.author	Khlystov O.M.
dc.date.accessioned	2024-10-27T02:28:48Z
dc.date.available	2024-10-27T02:28:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518438
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1462-1465
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46267
dc.description.abstract	In the coastal (shallow-water) part of Lake Baikal, we studied gas from several ice holes, which represent polynyas (ice-free water areas) typically formed at the end of March–beginning of April due to intense gas release from the lake floor. The water depth here is no more than 30–40 m. Gas seeps in the deep-water part of Baikal have been studied since the 1990s after the detection of seismoacoustic traces of gas seeps from the lake floor. Complex geophysical works in the Southern depression of the lake at a depth of ~1400 m revealed several morphologically distinct uplifts up to 40 m high and 800 m across with gas conduits and high heat flow.
dc.subject	Baikal
dc.subject	methane
dc.title	GENETIC TYPES OF METHANE FROM LAKE BAIKAL
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090285

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