ORE-BEARING GABBROID ROCKS OF THE SMELYY ANORTHOSITE PLUTON

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dc.contributor.author Borisenko L.F.
dc.contributor.author Tarasenko V.S.
dc.contributor.author Kolomiyets G.D.
dc.contributor.author Lukinykh A.D.
dc.date.accessioned 2020-10-09T08:58:15Z
dc.date.available 2020-10-09T08:58:15Z
dc.date.issued 1989
dc.identifier https://elibrary.ru/item.asp?id=31126126
dc.identifier.citation Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 1, 145-148
dc.identifier.issn 0891-5571
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/17881
dc.description.abstract Ore-bearing gabbroid rocks were recently detected in various places on the Ukrainian shield as segregations relatively high in ilmenite and locally in apatite. The ore body in gabbro-norite of the Smelyy anorthosite pluton studied by us in relatively high in TiO2. Because this pluton is part of the Korsun'-Novomirgorod batholith, the latter can be regarded as a potential source of titanium mineralization. Thus, the detection of ilmenite ore in the Smelyy pluton confirms the accuracy of conclusions that the Ukrainian shield is one of the main titanium provinces in the USSR.
dc.title ORE-BEARING GABBROID ROCKS OF THE SMELYY ANORTHOSITE PLUTON
dc.type Статья


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