FRANCOLITE-GROUTITE ASSOCIATION. A NEW ORE MINERAL TYPE IN THE CARBONATITE ROCK ASSOCIATION

dc.contributor.authorEntin A.R.
dc.contributor.authorYeremenko G.K.
dc.contributor.authorTyan O.K.
dc.contributor.authorOrlov A.N.
dc.date.accessioned2020-10-02T08:47:04Z
dc.date.available2020-10-02T08:47:04Z
dc.date.issued1989
dc.description.abstractOre consisting primarily of francolite and groutite was found in Siberia in an ultramafic pluton consisting of alkalic rock and carbonatites. Groutite has not previously been reported in carbonatite complexes; the hand-books describe it as a rare mineral. The find of significant concentrations of manganese as groutite suggests that a new mineral type of carbonatite and apparently a new type of commercial manganese deposit is involved. The data indicate that ore zones that contain not only in the usual assortment of elements (Fe, Ti, P, Nb, Ta and RE) but also manganese, occur in ultramafic alkalic plutons in association with carbonatites produced in the volcanic and subvolcanic depth facies.
dc.identifierhttps://elibrary.ru/item.asp?id=31074606
dc.identifier.citationTRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1989, 307, 4, 162-164
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/17641
dc.titleFRANCOLITE-GROUTITE ASSOCIATION. A NEW ORE MINERAL TYPE IN THE CARBONATITE ROCK ASSOCIATION
dc.typeСтатья

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