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Baldwin, Joy R. (1989) Replacement phenomena in tantalum minerals from rare-metal pegmatites in South Africa and Namibia. Mineralogical Magazine, 53 (373) 571-581 doi:10.1180/minmag.1989.053.373.08

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Reference TypeJournal (article/letter/editorial)
TitleReplacement phenomena in tantalum minerals from rare-metal pegmatites in South Africa and Namibia
JournalMineralogical MagazineISSN0026-461X
AuthorsBaldwin, Joy R.Author
Year1989 (December)Volume53
Issue373
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-373-571.pdf+
DOIdoi:10.1180/minmag.1989.053.373.08Search in ResearchGate
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Mindat Ref. ID1552Long-form Identifiermindat:1:5:1552:7
GUID0
Full ReferenceBaldwin, Joy R. (1989) Replacement phenomena in tantalum minerals from rare-metal pegmatites in South Africa and Namibia. Mineralogical Magazine, 53 (373) 571-581 doi:10.1180/minmag.1989.053.373.08
Plain TextBaldwin, Joy R. (1989) Replacement phenomena in tantalum minerals from rare-metal pegmatites in South Africa and Namibia. Mineralogical Magazine, 53 (373) 571-581 doi:10.1180/minmag.1989.053.373.08
In(1989, December) Mineralogical Magazine Vol. 53 (373) Mineralogical Society
Abstract/NotesAbstractManganotantalite replacement by (1) microlite and (2) ferrotantalite, and changes in composition of uranoan microlite from rare-metal pegmatites in South Africa and Namibia have been investigated with the electron microprobe. A uranmicrolite from Karibib, Namibia contained 14.35% UO2, 1.03% PbO, 56.12% Ta2O5, 13.18% Nb2O5, 0.58% Fe2O3, 6.87% CaO, 0.54% SrO, 0.59% MnO, 0.86% Na2O and 0.47% F. Analyses along traverses across a 1.3 mm uranoan microlite, Tantalite Valley, Namibia, revealed two essentially distinct compositions: a more hydrated rim area of 200 µm radius containing 7% higher Ta2O5, 10% lower CaO and 1.3% lower F than a main central area of slightly variable composition. Back-scattered electron images reveal zoning and distinctive subspheroidal structures. New data and structural features are given for radioactive uranoan microlite from Namaqualand, South Africa. These crystals contain remnants of a bismuth phase and are in various stages of replacement. In the microlites replacing manganotantalite, the microlite reflects the composition of the replaced mineral. At Rubicon Mine, Karibib, a narrow marginal zone of mangantantalite is replaced by ferrotantalite along cleavages; a zone of intermediate composition is apparent. Detailed traverses have been completed across all of these crystals.

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Locality Pages

LocalityCitation Details
Homestead pegmatite, Tantalite Valley, Karasburg East, ǁKaras Region, Namibia
Lepidolite pegmatite, Tantalite Valley, Karasburg East, ǁKaras Region, Namibia

Mineral Pages

MineralCitation Details
Uranmicrolite (of Hogarth 1977)[as uranoan microlite]

Mineral Occurrences

LocalityMineral(s)
Homestead pegmatite, Tantalite Valley, Karasburg East, ǁKaras Region, Namibia Microlite Group, Tantalite-(Mn)
Lepidolite pegmatite, Tantalite Valley, Karasburg East, ǁKaras Region, Namibia Lepidolite, Microlite Group
Jakkalswater (Jackal's Water; Noumas I pegmatite; Blesberg mine), Steinkopf, Nama Khoi Local Municipality, Namakwa District Municipality, Northern Cape, South Africa Tantalite-(Mn)


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