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Publication details
Concurrent treatment of metamict and crystalline fergusonite by U, Th and Pb-rich fluids:an EMPA and TEM study
Authors | |
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Year of publication | 2011 |
Type | Article in Periodical |
Magazine / Source | Asociation Geologica Argentina, Series D. |
MU Faculty or unit | |
Citation | |
Field | Geology and mineralogy |
Keywords | fergusonite; metamict state; experimental alteration; EMPA; TEM; FIB |
Description | Metamict and well crystalline fergusonite-(Y) were treated by U,Th,Pb-rich fluids at temperature 200oC for 60 days. The well crystalline fergusonite did not show any apparent features of alteration. The metamict fergusonite was intensivelly replaced by newly-formed U and Th-rich phases. The TEM study of the FIB prepared foils revealed, that Th-rich phase is amorphous, whereas the U-rich phase corresponds to UNb3O10. On the border of unchanged metamict fergusonite and newly-formed phases the numerous of nanopores were found. The alteration corresponds to dissolution-reaction-precipitation process. |
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