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The Canadian Mineralogist GSW 2008 Users' Group Meeting
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The Canadian Mineralogist; June 2007; v. 45; no. 3; p. 451-456; DOI: 10.2113/gscanmin.45.3.451
© 2007 Mineralogical Association of Canada
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KRIVOVICHEVITE, Pb3[Al(OH)6](SO4)(OH), A NEW MINERAL SPECIES FROM THE LOVOZERO ALKALINE MASSIF, KOLA PENINSULA, RUSSIA

Victor N. Yakovenchuk1,§, Yakov A. Pakhomovsky1, Yuri P. Men’shikov1, Julia A. Mikhailova1, Gregory Yu. Ivanyuk1 and Oleg A. Zalkind2

1 Geological Institute, Kola Science Center, Russian Academy of Sciences, 14 Fersman Street, Apatity 184209, Russia
2 Institute of Chemistry, Technology of Rare Elements and Mineral Resources, Kola Science Center, Russian Academy of Sciences, 14 Fersman Street, Apatity 184209, Russia


Figure 1
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  		FIG. 1. Simplified geology of the Lovozero massif according to Bussen & Sakharov (1972), with additions.

 

Figure 2
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  		FIG. 2. Natrolite – aegirine – orthoclase vein in lujavrite, Mt. Lepkhe–Nelm.

 

Figure 3
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  		FIG. 3. Krivovichevite grain, which look like ice, with another sulfate of lead, covering a galena crystal, from a natrolite – aegirine – orthoclase vein in lujavrite, Mt. Lepkhe –Nelm. Field of view: 25 x 14 mm.

 

Figure 4
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  		FIG. 4. Infrared-absorption spectrum of powdered krivovichevite.

 




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