karelianiten.

/kəˈriːlɪənʌɪt/

Etymology: < Karelian n. + -ite suffix¹.

Mineralogy.

An oxide of vanadium, V₂O₃.

ΘΚΠ

the world > the earth > minerals > types of mineral > oxides and hydroxides > [noun] > other oxides > other simple oxides

red lead1295

martial ethiops1773

ilsemannite1871

brookite1879

karelianite1963

1963 J. V. P. Long et al. in Amer. Mineralogist 48 40 Electron microprobe analyses and the crystallographic data obtained suggest the existence of a new vanadium mineral, V₂O₃, isostructural with hematite, eskolaite and corundum. The name karelianite, after the region of Finland in which the Outokumpu mine is situated, is proposed for this mineral, the name to be applied to the pure end member.

1967 Mineral. Abstr. 18 282/2 Three principal minerals compose the dominantly vanadiferous ores [at Mounana, Gabon]—karelianite, montroseite, and roscoelite. Karelianite, rarely more than 0·5 mm in size, occurs as grains in the grit cement or as blades forming 60° stars in quartz.

This entry has not yet been fully updated (first published 1976; most recently modified version published online June 2018).

单词	karelianite
释义	karelianiten. /kəˈriːlɪənʌɪt/ Etymology: < Karelian n. + -ite suffix¹. Mineralogy. An oxide of vanadium, V₂O₃. ΘΚΠ the world > the earth > minerals > types of mineral > oxides and hydroxides > [noun] > other oxides > other simple oxides red lead1295 martial ethiops1773 ilsemannite1871 brookite1879 karelianite1963 1963 J. V. P. Long et al. in Amer. Mineralogist 48 40 Electron microprobe analyses and the crystallographic data obtained suggest the existence of a new vanadium mineral, V₂O₃, isostructural with hematite, eskolaite and corundum. The name karelianite, after the region of Finland in which the Outokumpu mine is situated, is proposed for this mineral, the name to be applied to the pure end member. 1967 Mineral. Abstr. 18 282/2 Three principal minerals compose the dominantly vanadiferous ores [at Mounana, Gabon]—karelianite, montroseite, and roscoelite. Karelianite, rarely more than 0·5 mm in size, occurs as grains in the grit cement or as blades forming 60° stars in quartz. This entry has not yet been fully updated (first published 1976; most recently modified version published online June 2018). < n.1963
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