THE EURASIAN LATITUDINAL LINEAMENT 52°N: GEOPHYSICAL AND MINERAGENIC CHARACTERISTICS

dc.contributor.author	Bulin N.K.
dc.contributor.author	Vlasov N.G.
dc.contributor.author	Erinchek Y.M.
dc.contributor.author	Gal'perov G.V.
dc.contributor.author	Solodilov L.N.
dc.date.accessioned	2022-08-03T05:20:56Z
dc.date.available	2022-08-03T05:20:56Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13464354
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 3, 347-351
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38441
dc.description.abstract	This article provides evidence for the existence of a Eurasian transregional latitudinal lineament. This lineament, 40-100 km wide, extends along 52° N from the Warsaw area to Sakhalin Island between 24° and 146° E over approximately 14 000 km. The recognition of this lineament is conditional to a certain extent, because it is based on geophysical data pertaining to three (Belorussian, Russian-Kazakh, and Far Eastern) segments that are separated by rather long intervals and in which the lineament is inferred from images taken from space and other data.
dc.title	THE EURASIAN LATITUDINAL LINEAMENT 52°N: GEOPHYSICAL AND MINERAGENIC CHARACTERISTICS
dc.type	Статья

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