Add to ORKGAbstract: Raman spectra of the mineral uranopilite at 298 and 77 K have been obtained and used to elucidate the structure of the mineral. A single intense band at 1010 cm-1 is assigned to the ν1 (SO4)2- symmetric stretching mode. Three low intensity bands in the 298 K Raman spectrum ar
Uranyl silicates are understood as common constituents of the oxidized parts of uranium deposits. Th...
Raman spectroscopy complimented with infrared spectroscopy has been used to study the uranyl carbona...
Raman spectroscopy at 298 and 77K has been used to study the mineral kamotoite-(Y), a uranyl rare ea...
Raman spectra of jáchymovite, (UO2)8(SO4)(OH)14•13H2O, were studied, complemented with infrared spec...
The mineral parsonsite with samples from The Ranger Uranium Mine, Australia and La Faye Mine, Grury,...
Uranyl micas are based upon (UO2 PO4)- units in layered structures with hydrated counter cations bet...
The mineral parsonsite with samples from The Ranger Uranium Mine, Australia and La Faye Mine, Grury,...
Raman and infrared spectra of secondary uranyl phosphate vanmeersscheite and Raman spectrum of secon...
Raman spectra of the uranyl containing mineral coconinoite, Fe2Al2(UO2)2(PO4)4(SO4)(OH)2•20H2O, are ...
Raman spectra of dumontite were measured at 298 and 77 K. Observed bands were attributed to the stre...
Raman spectroscopic study of the uranyl phosphate minerals phosphuranylite and yingjiangit
Raman spectra of two uranyl mineral dewindtite samples are presented and interpreted. Observed bands...
Raman spectra of two uranyl mineral dewindtite samples are presented and interpreted. Observed bands...
Raman spectra of phosphuranylite and yingjiangite were measured, interpreted and compared with publi...
Raman spectra of phosphuranylite and yingjiangite were measured, interpreted and compared with publi...
Uranyl silicates are understood as common constituents of the oxidized parts of uranium deposits. Th...
Raman spectroscopy complimented with infrared spectroscopy has been used to study the uranyl carbona...
Raman spectroscopy at 298 and 77K has been used to study the mineral kamotoite-(Y), a uranyl rare ea...
Raman spectra of jáchymovite, (UO2)8(SO4)(OH)14•13H2O, were studied, complemented with infrared spec...
The mineral parsonsite with samples from The Ranger Uranium Mine, Australia and La Faye Mine, Grury,...
Uranyl micas are based upon (UO2 PO4)- units in layered structures with hydrated counter cations bet...
The mineral parsonsite with samples from The Ranger Uranium Mine, Australia and La Faye Mine, Grury,...
Raman and infrared spectra of secondary uranyl phosphate vanmeersscheite and Raman spectrum of secon...
Raman spectra of the uranyl containing mineral coconinoite, Fe2Al2(UO2)2(PO4)4(SO4)(OH)2•20H2O, are ...
Raman spectra of dumontite were measured at 298 and 77 K. Observed bands were attributed to the stre...
Raman spectroscopic study of the uranyl phosphate minerals phosphuranylite and yingjiangit
Raman spectra of two uranyl mineral dewindtite samples are presented and interpreted. Observed bands...
Raman spectra of two uranyl mineral dewindtite samples are presented and interpreted. Observed bands...
Raman spectra of phosphuranylite and yingjiangite were measured, interpreted and compared with publi...
Raman spectra of phosphuranylite and yingjiangite were measured, interpreted and compared with publi...
Uranyl silicates are understood as common constituents of the oxidized parts of uranium deposits. Th...
Raman spectroscopy complimented with infrared spectroscopy has been used to study the uranyl carbona...
Raman spectroscopy at 298 and 77K has been used to study the mineral kamotoite-(Y), a uranyl rare ea...