THE KHIBINY-LOVOZERO BINUCLEUS VORTEX STRUCTURE

dc.contributor.author	Kulakovsky A.L.
dc.date.accessioned	2022-08-14T03:31:12Z
dc.date.available	2022-08-14T03:31:12Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13472698
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 149-152
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38551
dc.description.abstract	It is concluded that structural position of Khibiny and Lovozero massifs was predetermined already in Precambrian Period, with formation of binucleus vortex structure upon shear deformation. Paleozoic activation of this structure (in arcogenic rifting mode?) is responsible for formation in the place of nuclei of the conical spallation zones, which controlled the alkaline massif development.
dc.title	THE KHIBINY-LOVOZERO BINUCLEUS VORTEX STRUCTURE
dc.type	Статья

Files in this item

Name: Kula_04.pdf

Size: 2.701Mb

Format: PDF