TEMPERATURE RANGE FOR THE FORMATION OF SODALITE-BEARING ASSEMBLAGES

Ustinov V.I.; Grinenko V.A.; Kotel'nikov A.R.

dc.contributor.author	Ustinov V.I.
dc.contributor.author	Grinenko V.A.
dc.contributor.author	Kotel'nikov A.R.
dc.date.accessioned	2024-11-09T08:38:25Z
dc.date.available	2024-11-09T08:38:25Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13530452
dc.identifier.citation	Geochemistry International, 2006, 44, 2, 199-201
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46459
dc.description.abstract	Sodalites are framework aluminosilicates with the general formula Na8Al6Si6O24 · (X)(1–2), where X represents Cl –, Br–, I–, S , C , OH –, and other anions. Sodalites usually crystallize in a cubic structure with space group P43n for chlorine-sodalite and P43 m for sulfate-sodalite (nosean). Sodalite occurs in alkaline igneous rocks and, occasionally, in pegmatites. The greatest diversity of sodalite-group minerals was observed in the Lovozero alkaline massif, where hydroxyl-, chlorine-, and sulfate-bearing sodalites were found.
dc.subject	sodalites
dc.title	TEMPERATURE RANGE FOR THE FORMATION OF SODALITE-BEARING ASSEMBLAGES
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906020091