HIGH-TEMPERATURE CARBONATITE MELT AND ITS INTERRELATIONS WITH ALKALINE MAGMAS OF THE DUNKEL'DYK COMPLEX, SOUTHEASTERN PAMIRS

Solovova I.P.; Girnis A.V.; Ryabchikov I.D.; Simakin S.G.

dc.contributor.author	Solovova I.P.
dc.contributor.author	Girnis A.V.
dc.contributor.author	Ryabchikov I.D.
dc.contributor.author	Simakin S.G.
dc.date.accessioned	2024-11-02T11:07:58Z
dc.date.available	2024-11-02T11:07:58Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524330
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1148-1151
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46385
dc.description.abstract	This paper is aimed at studying the inclusions (microportions of mineral-forming media in minerals) in clinopyroxenes from a leucite fergusite sample taken from a diatreme of the Dunkel’dyk alkaline complex in the southeastern Pamirs. The Dunkel’dyk Complex is bounded in the north and the west by the Rushan–Pshart and Gunt-Alichur deep-seated faults, respectively, which were formed in the Paleozoic and partly rejuvenated in the Neogene.
dc.subject	Dunkel’dyk complex
dc.subject	Pamirs
dc.title	HIGH-TEMPERATURE CARBONATITE MELT AND ITS INTERRELATIONS WITH ALKALINE MAGMAS OF THE DUNKEL'DYK COMPLEX, SOUTHEASTERN PAMIRS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070336