BELKOVITE BA2(NB, TI)6(SI2O7)2O12. A NEW MINERAL FROM CARBONATITE OF THE VUORIYARVI PLUTON (KOLA PENINSULA)

dc.contributor.authorVoloshin A.V.
dc.contributor.authorSubbotin V.V.
dc.contributor.authorPakhomovskiy Y.A.
dc.contributor.authorBakhchisaraytsev A.Y.
dc.contributor.authorYamnova N.A.
dc.contributor.authorPushcharovskiy D.Y.
dc.date.accessioned2020-10-31T02:50:06Z
dc.date.available2020-10-31T02:50:06Z
dc.date.issued1990
dc.description.abstractThe mineral described here was found in a drill core, where it occurred in veins of dolomite- and calcite-containing carbonate cutting pyroxenite of the alkalic-ultramafic Vuoriyarvi pluton on the Kola Peninsula. The belkovite segregations occur in solution cavities that are produced by the dolomitization of pyrochlore-containing calcite carbonatite. The mineral is associated with magnetite, pyrochlore, pyrite, pyrrhotite, minerals of the apatite group, barite, alstonite, chlorite, and nenadkewitschite. It is formed by hydrothermal alteration of pyrochlore.
dc.identifierhttps://elibrary.ru/item.asp?id=31076781
dc.identifier.citationTransactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 6, 229-232
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/18257
dc.titleBELKOVITE BA2(NB, TI)6(SI2O7)2O12. A NEW MINERAL FROM CARBONATITE OF THE VUORIYARVI PLUTON (KOLA PENINSULA)
dc.typeСтатья

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