Ixiolite-(Sc), (Ta <sub>0.5</sub> Sc <sub>0.5</sub> )O <sub>2</sub> , a new columbite-supergroup mineral from the Heftetjern pegmatite, Tørdal, Telemark, Norway

Scandium-rich members of the ixiolite group have been reported for decades from the Sveconorwegian Heftetjern pegmatite (Trdal, Telemark, Norway), but their mineralogical taxonomic status remained unresolved.Here we characterize and describe ixiolite-(Sc), a new ixiolite-group member (IMA 2025-054), with the ideal formula (Ta 0.5 Sc 0.5 )O 2 .The mineral occurs as dull black, submetallic, opaque aggregates up to 2-3 mm (locally reported as prismatic crystals to 5 mm), partly altered to a secondary Sc-rich microlite-group phase.It is associated with albite, quartz, fluorite, spessartine and microlite-group minerals, and is interpreted as a primary accessory phase crystallized from Sc-enriched late-stage pegmatitic

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Publication Details

Journal
Mineralogical Magazine
Published
2026-02-26
DOI
https://doi.org/10.1180/mgm.2026.10208
Primary Topic
Crystal Structures and Properties
Type
article
Field-Weighted Citation Impact
0.00

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article

Ixiolite-(Sc), (Ta 0.5 Sc 0.5 )O 2 , a new columbite-supergroup mineral from the Heftetjern pegmatite, Tørdal, Telemark, Norway

Roy Kristiansen, Dan Holtstam, Alice Taddei, Luca Bindi
Mineralogical Magazine
Crystal Structures and Properties
article

Ixiolite-(Sc), (Ta 0.5 Sc 0.5 )O 2 , a new columbite-supergroup mineral from the Heftetjern pegmatite, Tørdal, Telemark, Norway

Roy Kristiansen, Dan Holtstam, Alice Taddei, Luca Bindi
article en

Abstract

Scandium-rich members of the ixiolite group have been reported for decades from the Sveconorwegian Heftetjern pegmatite (Trdal, Telemark, Norway), but their mineralogical taxonomic status remained unresolved.Here we characterize and describe ixiolite-(Sc), a new ixiolite-group member (IMA 2025-054), with the ideal formula (Ta 0.5 Sc 0.5 )O 2 .The mineral occurs as dull black, submetallic, opaque aggregates up to 2-3 mm (locally reported as prismatic crystals to 5 mm), partly altered to a secondary Sc-rich microlite-group phase.It is associated with albite, quartz, fluorite, spessartine and microlite-group minerals, and is interpreted as a primary accessory phase crystallized from Sc-enriched late-stage pegmatitic

Mineralogical Magazine
Swedish Museum of Natural History (SE), Institute of Geosciences and Earth Resources (IT), ViGØR Rehabiliteringssykehus (NO), Museo Galileo (IT), University of Florence (IT)
Università degli Studi di Firenze
Openalex Percentile: Top 45%
Crystal Structures and Properties
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