ВЛИЯНИЕ ГИПЕРГЕННЫХ УСЛОВИЙ НА КАЧЕСТВО ИСКОПАЕМОЙ МАМОНТОВОЙ КОСТИ

dc.contributor.author	Смирнов A.H.
dc.date.accessioned	2024-03-16T02:51:53Z
dc.date.available	2024-03-16T02:51:53Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9222558
dc.identifier.citation	Записки Российского минералогического общества, 2006, 135, 1, 130-139
dc.identifier.issn	0869-6055
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42994
dc.description.abstract	Fossil ivory (FI) - tusks of Siberian mammoth (Mammuthus primigenius) - is a complicated organic-mineral aggregate of orthobiogenic origin. As a natural composite, it consists of collogene, water and hydroxylapatite (up to 50 %). The paper briefly considers features of composition and structure of the mammoth tusk; its elementary composition was studied by microprobe analysis: CaO 18.30-25.94%, P2O5 14.93-21.55%, MgO 0.23-1.82 % (CamScan MV 2300, OXVORT, LINK ISIS-300). There is also shown influence of taphonomic settings on the qualitative characteristics of FI, i. e. its commercial value.
dc.title	ВЛИЯНИЕ ГИПЕРГЕННЫХ УСЛОВИЙ НА КАЧЕСТВО ИСКОПАЕМОЙ МАМОНТОВОЙ КОСТИ
dc.type	Статья
dc.subject.udc	551.311.22:569.61

Files in this item

Files	Size	Format	View
There are no files associated with this item.