Publication Date:
2011-08-01
Description:
Fluorocronite ([FE][t][o][p][o][kcy][p][o][ncy][icy][t]), ideally PbF2, is a new mineral (IMA2010-023), from the Kupol'noe deposit, Sarychev range, Sakha Republic, Russian Federation. It occurs intimately mixed with cassiterite and a potentially new Sn oxy-hydroxide with the composition Sn4O(OH,F)6, and is found in direct association with quartz, anglesite, cerussite, galena, hocartite, bindheimite and chlorargyrite. Fluorocronite forms flattened, leaf-like microcrystals up to about 20 {micro}m across. The main form observed is {100}, while {111} may also be present. The crystals are translucent and white with a pearly lustre. The streak is also white and Mohs hardness is between 3 and 4 (estimated). No parting or twinning was observed. Fluorocronite has prefect cleavage on {111} by analogy with other minerals with the fluorite structure type. Crystals are optically isotropic; however, the refractive index could not be measured due to the small size of the crystals. The empirical formula (based on 3 apfu) is Pb0.98F2.02. The simplified formula is PbF2. Fluorocronite is cubic, space group Fm[IMG]f1.gif" ALT="Formula" BORDER="0"〉m, with a = 5.9306(5) A, V = 208.59(5) A3 and Z = 4. Fluorocronite is isostructural with fluorite. The five strongest lines in the powder X-ray diffraction pattern are [dobs in A (I) (hkl)]: 3.437 (100) (111); 2.976 (46) (002); 2.103 (44) (022); 1.794 (42) (311); 1.717 (21) (222). The name is in relation to the composition; fluoro (for fluorine) and cron ({kappa}{rho}[ó]{nu}o{varsigma}, the alchemical name for lead).
Print ISSN:
0935-1221
Electronic ISSN:
1617-4011
Topics:
Geosciences
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