NEW DATA ON THERMAL FLOW IN THE CENTRAL PART OF THE KOLA PENINSULA

dc.contributor.author	Glaznev V.N.
dc.contributor.author	Raevskii A.B.
dc.contributor.author	Kukkonen I.T.
dc.contributor.author	Jokinen J.
dc.date.accessioned	2022-08-03T05:21:00Z
dc.date.available	2022-08-03T05:21:00Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13466151
dc.identifier.citation	Doklady Earth Sciences, 2004, 396, 4, 512-514
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38467
dc.description.abstract	Geothermal studies in the central Kola Peninsula revealed the existence of anomalously low heat flows in the depth range of 0-1 km. The nature of such anomalous temperature behavior in the Earth's upper crust is related to paleoclimatic influence of the Valdaian glaciation, presumably characterized by the absence of thick ice cover during long intervals.
dc.title	NEW DATA ON THERMAL FLOW IN THE CENTRAL PART OF THE KOLA PENINSULA
dc.type	Статья

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