“…Introduction VAPNIKITE, Ca 3 UO 6 (IMA2013-082), was discovered in pyrometamorphic larnite rocks of the Jabel (Mountain in Arabian) Harmun locality belonging to the Hatrurim Formation ('Mottled Zone'; Picard, 1931;Bentor, 1960;Gross, 1977;Vapnik et al, 2007), situated in the Judean Desert, West Bank, Palestinian Autonomy, Israel (31º46'N 35º26'E). Vapnikite (P2 1 /n, Z = 2, a = 5.739(1), b = 5.951(1), c = 8.312(1) Å , b = 90.4(1)º, V = 283.9(1) Å 3 ) is the first naturally occurring ordered double perovskite of the A 2 BB'O 6 type (A, B = Ca; B' = U 6+ ) with the synthetic analogue named b-Ca 3 UO 6 (P2 1 /n, Z = 2, a = 5.728(1), b = 5.956(1), c = 8.298(2) Å , b = 90.55(3)º, V = 283.1(1) Å 3 ; Loopstra and Rietveld, 1969;van Duivenboden and IJdo, 1986;Mitchell, 2002;Read et al, 2013). The synthetic low-temperature polymorph a-Ca 3 UO 6 is trigonal (R3 , a = 9.624(1), c = 11.388(1) Å , g = 120º, V = 913.3(1) Å 3 ; Holc and Goli, 1983).…”