“…These rare minerals are from the oxidizied zone of a U deposit at Shinkolobwe, Democratic Republic of Congo, and the oxidized zone of a hydrothermal Au/Te deposit at the Moctezuma mine in Mexico [4]. More recently, 11 hydrothermally synthesized uranyl tellurites have been synthesized and structurally characterized: Pb 2 UO 2 (TeO 3 ) 3 [5] [6], Na 8 [(UO 2 ) 6 (TeO 3 ) 10 ] [7], A 2 [(UO 2 ) 3 (TeO 3 ) 2 O 2 ] (A¼K, Rb, Cs) [8], and K 4 [(UO 2 ) 5 (TeO 3 ) 2 O 5 ] [9]. Considerable structural diversity is exhibited by these compounds, which contain structural units consisting of uranyl tellurite chains, sheets, and frameworks.…”