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Kharisun, Taylor, M. R., Bevan, D. J. M., Rae, A. D., Pring, A. (1997) The crystal structure of mawbyite, PbFe2(AsO4)2(OH)2. Mineralogical Magazine, 61 (408). 685-691 doi:10.1180/minmag.1997.061.408.07

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Reference TypeJournal (article/letter/editorial)
TitleThe crystal structure of mawbyite, PbFe2(AsO4)2(OH)2
JournalMineralogical MagazineISSN0026-461X
AuthorsKharisunAuthor
Taylor, M. R.Author
Bevan, D. J. M.Author
Rae, A. D.Author
Pring, A.Author
Year1997 (October)Volume61
Page(s)685-691Issue408
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_61/61-408-685.pdf+
DOIdoi:10.1180/minmag.1997.061.408.07Search in ResearchGate
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Mindat Ref. ID207Long-form Identifiermindat:1:5:207:5
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Full ReferenceKharisun, Taylor, M. R., Bevan, D. J. M., Rae, A. D., Pring, A. (1997) The crystal structure of mawbyite, PbFe2(AsO4)2(OH)2. Mineralogical Magazine, 61 (408). 685-691 doi:10.1180/minmag.1997.061.408.07
Plain TextKharisun, Taylor, M. R., Bevan, D. J. M., Rae, A. D., Pring, A. (1997) The crystal structure of mawbyite, PbFe2(AsO4)2(OH)2. Mineralogical Magazine, 61 (408). 685-691 doi:10.1180/minmag.1997.061.408.07
In(1997, October) Mineralogical Magazine Vol. 61 (408) Mineralogical Society
Abstract/NotesAbstractThe crystal structure of mawbyite, PbFe2(AsO4)2(OH)2 has been refined. The mineral is monoclinic, C2/m with a = 9.066(4), b = 6.286(3) c = 7.564(3) Å, β = 114.857(5)°, Z = 2; the structure has been refined to a conventional R = 4.3% using 361 observed reflections [I> 3σ(I)]. The structure contains chains of edgesharing Fe(O,OH)6 octahedra which are linked by AsO4 tetrahedra and Pb atoms in distorted square antiprismatic co-ordination. The hydrogen bonding network in the structure has been modelled using bond valence calculations. Mawbyite is confirmed to be isostructural with tsumcorite and dimorphous with carminite and the relationship between these two structures is discussed.

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Mawbyite


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