THE KHIBINY-LOVOZERO BINUCLEUS VORTEX STRUCTURE

dc.contributor.authorKulakovsky A.L.
dc.date.accessioned2022-08-14T03:31:12Z
dc.date.available2022-08-14T03:31:12Z
dc.date.issued2004
dc.description.abstractIt 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.identifierhttps://www.elibrary.ru/item.asp?id=13472698
dc.identifier.citationDoklady Earth Sciences, 2004, 395, 2, 149-152
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38551
dc.titleTHE KHIBINY-LOVOZERO BINUCLEUS VORTEX STRUCTURE
dc.typeСтатья

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