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Hill, R. J., Canterford, J. H., Moyle, F. J. (1982) New data for lansfordite. Mineralogical Magazine, 46 (341) 453-457 doi:10.1180/minmag.1982.046.341.08

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Reference TypeJournal (article/letter/editorial)
TitleNew data for lansfordite
JournalMineralogical MagazineISSN0026-461X
AuthorsHill, R. J.Author
Canterford, J. H.Author
Moyle, F. J.Author
Year1982 (December)Volume46
Issue341
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_46/46-341-453.pdf+
DOIdoi:10.1180/minmag.1982.046.341.08Search in ResearchGate
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Mindat Ref. ID3437Long-form Identifiermindat:1:5:3437:5
GUID0
Full ReferenceHill, R. J., Canterford, J. H., Moyle, F. J. (1982) New data for lansfordite. Mineralogical Magazine, 46 (341) 453-457 doi:10.1180/minmag.1982.046.341.08
Plain TextHill, R. J., Canterford, J. H., Moyle, F. J. (1982) New data for lansfordite. Mineralogical Magazine, 46 (341) 453-457 doi:10.1180/minmag.1982.046.341.08
In(1982, December) Mineralogical Magazine Vol. 46 (341) Mineralogical Society
Abstract/NotesAbstractEuhedral crystals of the low-temperature mineral lansfordite, MgCO3 · 5H2O, have been prepared from saturated magnesium bicarbonate solutions at temperatures below 10°C. The crystals are monoclinic P21/a with a = 12.4758(7), b = 7.6258(4), c = 7.3463(6)Å, β = 101.762(6)°, V = 684.24Å3, Dcalc. = 1.693 g cm−3, Dobs. = 1.70(1) g m−3. At room temperature, the crystals slowly effloresce to produce pseudomorphs of nesquehonite, MgCO3 · 3H2O. Dehydration is complete at 300°C, with decarbonation taking place in the interval to 560°C. A new X-ray powder diffraction pattern is presented, and details of the infra-red absorption spectrum are discussed.


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