摘要
<正>Objective Galuskin et al.(2011)firstly discovered that vorlanite(CaU~(6+/4+))O_4 is a rare Ca-rich mineral with a fluorite-type structure,which is isostructural with uraninite(U~(4+)O_2).Previous studies of the Xianshi granite-related uranium deposit reported that uraninite and pyrite are the major ore minerals whereas galena,clausthalite(PbSe),and pyrite are minor phases in the ores.A more detailed petrographic
引文
Galuskin,E.V.,Armbruster,T.,Galuskina,I.O.,Lazic,B.,Winiarski,A.,Gazeev,V.M.,Dzierzanowski,P.,Zadov,A.E.,Pertsev,N.N.,Wrzalik,R.,Gurbanov,A.G.,Janeczek,J.,2011.Vorlanite(Ca U6+)O4—A new mineral from the Upper Chegem caldera,Kabardino-Balkaria,Northern Caucasus,Russia.American Mineralogist 96:188–196.
Luo,J.C.,Hu,R.Z.,Fayek,M.,Li,C.S.,Bi,X.W.,Abdu,Y.,Chen,Y.W.,2015.In-situ SIMS uraninite U–Pb dating and genesis of the Xianshi granite-hosted uranium deposit,South China.Ore Geology Reviews 65:968–978.
Mercadier,J.,Cuney,M.,Lach,P.,Boiron,M.C.,Bonhoure,J.,Richard,A.,Leisen,M.,Kister,P.,2011,Origin of uranium deposits revealed by their rare earth element signature.Terra Nova 23:264–269.