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Hawthorne, F.C. (1982) The crystal structure of boggildite. The Canadian Mineralogist: 20: 263-270.

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Year1982
Original EntryHawthorne, F.C. (1982) The crystal structure of boggildite. The Canadian Mineralogist: 20: 263-270.
Mindat Ref. ID16103463Long-form Identifiermindat:1:5:16103463:4
GUID0
Full ReferenceHawthorne, F.C. (1982) The crystal structure of boggildite. The Canadian Mineralogist: 20: 263-270.
Plain TextHawthorne, F.C. (1982) The crystal structure of boggildite. The Canadian Mineralogist: 20: 263-270.

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MineralCitation Details
Bøggildite

See Also

These are possibly similar items as determined by title/reference text matching only.

Hawthorne, F.C. (1979) The crystal structure of morinite. The Canadian Mineralogist: 17: 93–102.
Cooper, M.A., Hawthorne, F.C. (1996) The crystal structure of spiroffite. The Canadian Mineralogist: 34: 821-826.
Cooper, M.A. & Hawthorne, F.C. (1997): The crystal structure of wicksite. The Canadian Mineralogist, 35, 777-784.
Hawthorne, F.C. and Burns, P.C. (1997) The crystal structure of jørgensenite. Canadian Mineralogist: 35: 1509-1513.
Cooper, M.A., Hawthorne, F.C. (1997) A note on the crystal structure of marshite. The Canadian Mineralogist: 35: 785-786.
Canadian Mineralogist (1998): 36: 817-822.
Hawthorne, F.C., Ferguson, R.B. (1975) Anhydrous sulphates. II. Refinement of the crystal structure of anhydrite. The Canadian Mineralogist: 13: 289-292.
Selway, J.B., Cooper, M.A., and Hawthorne, F.C. (1997) Refinement of the crystal structure of burangaite. The Canadian Mineralogist: 35: 1515-1522.
Burns, P.C., Hawthorne, F.C. (1995) Rietveld refinement of the crystal structure of olivenite: a twinned monoclinic structure. The Canadian Mineralogist: 33: 885-888.
Burns, P.C., Hawthorne, F.C., MacDonald, D.J., Della Ventura, G., Parodi, G.C. (1993) The crystal structure of stillwellite. The Canadian Mineralogist: 31: 147-152.
Groat, L.A., Hawthorne, F.C., Ercit, T.S. (1992) The role of fluorine in vesuvianite; a crystal-structure study. The Canadian Mineralogist: 30: 1065-1075.
 
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