MELT INCLUSIONS IN MINERALS OF SCAPOLITE-BEARING GRANULITE (LOWER CRUSTAL XENOLITHS FROM DIATREMES OF THE PAMIRS)

Chupin V.P.; Kuz'min D.V.; Madyukov I.A.

dc.contributor.author	Chupin V.P.
dc.contributor.author	Kuz'min D.V.
dc.contributor.author	Madyukov I.A.
dc.date.accessioned	2024-11-09T08:38:26Z
dc.date.available	2024-11-09T08:38:26Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13530886
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 507-511
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46463
dc.description.abstract	The study of scapolite-bearing eclogite-like rocks and granulites, experimental data, and finds of scapolite in igneous rocks showed that high-Ca scapolite can be of both metamorphic and magmatic origin under the high partial pressure of CO2 and/or SO3 in the fluid or melt. This communication presents the first direct data on scapolite crystallization in the lower crust with participation of CO2-saturated melts.
dc.subject	scapolite
dc.subject	Pamirs
dc.title	MELT INCLUSIONS IN MINERALS OF SCAPOLITE-BEARING GRANULITE (LOWER CRUSTAL XENOLITHS FROM DIATREMES OF THE PAMIRS)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030366