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- W2001077478 abstract "The mineral fluorannite, a new member in trioctahedral micas, has been approved by the Commission on New Minerals and Mineral Names (CNMMN) in 1999. Here a room-temperature Mossbauer data of this new mineral from Suzhou, China was reported and interpreted in terms of quadrupole splitting distributions (QSDs). Based on QSD analysis, the overall of QSDs at 298 K can be interpreted in terms of four QSD contributions centered at QS = 2.571 mm/s for Fe 2+ -O 4 (OH) 2 octahedra (cis and trans not resolved), QS = 2.255 mm/s for Fe 2+ -O 4 (OH)F octahedra (cis and trans not resolved), QS = 2.166 mm/s for cis-Fe 2+ -O 4 F 2 octahedra, and QS = 1.278 mm/s for trans-Fe 2+ -O 4 F 2 octahedra. The ferric iron spectral component with CS = 0.378 mm/s and QS = 0.645 mm/s was also characterized." @default.
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- W2001077478 date "2002-12-01" @default.
- W2001077478 modified "2023-09-26" @default.
- W2001077478 title "The Mössbauer spectrum of the new mineral fluorannite" @default.
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- W2001077478 doi "https://doi.org/10.1127/0935-1221/2002/0014-1049" @default.
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