FLUORIDES DEPOSITED DURING POSTERUPTIVE ACTIVITIES ON KAMCHATKAN VOLCANOES

dc.contributor.author	Serafimova E.K.
dc.date.accessioned	2020-12-24T08:52:36Z
dc.date.available	2020-12-24T08:52:36Z
dc.date.issued	1997
dc.identifier	https://elibrary.ru/item.asp?id=20949853
dc.identifier.citation	Volcanology & Seismology, 1997, , 5, 571-613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21335
dc.description.abstract	According to their formation conditions, the fluorides are classified in two types - pneumatolytic and metasomatic. They are spatially confined to rootless fumaroles of basalt volcanoes. The main mineral among the fluorides is α-ralstonite. The less common minerals are fluorite, sellaite, malladrite, and elpasolite. The chemical compositions of fluoride-bearing sublimation deposits are presented along with the results of X-ray diffraction and optical analyses. Fluorine mineral assemblages are described.
dc.title	FLUORIDES DEPOSITED DURING POSTERUPTIVE ACTIVITIES ON KAMCHATKAN VOLCANOES
dc.type	Статья

Files in this item

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