Mineral extinction

Remobilization of U and REE and the formation of secondary minerals in oxidized U deposits

Uranyl phosphate sheet reconstruction during dehydration of metatorbernite [Cu(UO 2 ) 2 (PO 4 ) 2 ·8H 2 O]

THE ORIGIN AND ZONING OF HYPOGENE AND SUPERGENE Fe–Mn–Mg–Sc–U–REE PHOSPHATE MINERALIZATION FROM THE NEWLY DISCOVERED TRUTZHOFMÜHLE APLITE, HAGENDORF PEGMATITE PROVINCE, GERMANY

Discussion on Dill et al . (2007) ‘Cu-Fe-U phosphate mineralization of the Hagendorf-Pleystein pegmatite province, Germany: with special reference to laser-ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS) of limonite-cored torbernite’, Mineralogical Magazine , 71, 371–387.

Reply to Discussion by Romer (2008) Mineralogical Magazine , 72, 827–831.

Cu-Fe-U phosphate mineralization of the Hagendorf-Pleystein pegmatite province, Germany: with special reference to laser-ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS) of limonite-cored torbernite

Dehydration processes in the meta-autunite group minerals meta-autunite, metasaléeite, and metatorbernite

CRYSTAL STRUCTURES AND SYNTHESIS OF THE COPPER-DOMINANT MEMBERS OF THE AUTUNITE AND META-AUTUNITE GROUPS: TORBERNITE, ZEUNERITE, METATORBERNITE AND METAZEUNERITE

Studies of Uranium Minerals (XXIII): Torbernite, Zeunerite and Uranospherite.

Anomalous fluorescence in torbernite from rum jungle, N.T. Australia

Torbernite in missouri fire clay