NA-RICH CARBONATE INCLUSIONS IN PEROVSKITE AND CALZIRTITE FROM THE GULI INTRUSIVE CA-CARBONATITE, POLAR SIBERIA

dc.contributor.author	Kogarko L.N.
dc.contributor.author	Plant D.A.
dc.contributor.author	Henderson C.M.B.
dc.contributor.author	Kjarsgaard B.A.
dc.date.accessioned	2020-11-06T05:35:45Z
dc.date.available	2020-11-06T05:35:45Z
dc.date.issued	1991
dc.identifier	https://elibrary.ru/item.asp?id=30819745
dc.identifier.citation	Contributions to Mineralogy and Petrology, 1991, , 1, 124-129
dc.identifier.issn	0010-7999
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18542
dc.description.abstract	Carbonate phases, some rich in Na2O and comparatively rich in SrO and BaO, occur as inclusions in perovskite and calzirtite (Ca2Zr5Ti2O16) in the carbonatite of the Guli complex, Siberia. This is the first record of alkali carbonates, akin to nyerereite [Na2Ca(CO3)2], in plutonic igneous rocks. The inclusion populations suggest that the parental magma of the complex was Ca-rich but developed Na-rich differentiates during the latest stages. This points to the dominant calcic carbonatites of the complex not being derivatives of alkali-rich parental carbonatites. These alkali-rich carbonate inclusions (and rare inclusions of djerfisherite) have been preserved due to the resistance of perovskite and calzirtite to processes of leaching, hydrothermal alteration and weathering.
dc.title	NA-RICH CARBONATE INCLUSIONS IN PEROVSKITE AND CALZIRTITE FROM THE GULI INTRUSIVE CA-CARBONATITE, POLAR SIBERIA
dc.type	Статья

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