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Zussman, J. (1956) Antigorite: Superlattice and structural formula. American Mineralogist, 41 (1-2) 148-151

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Reference TypeJournal (article/letter/editorial)
TitleAntigorite: Superlattice and structural formula
JournalAmerican Mineralogist
AuthorsZussman, J.Author
Year1956Volume41
Issue1-2
PublisherMineralogical Society of America
Download URLhttp://www.minsocam.org/ammin/AM41/AM41_148.pdf+
Mindat Ref. ID522752Long-form Identifiermindat:1:5:522752:9
GUID0
Full ReferenceZussman, J. (1956) Antigorite: Superlattice and structural formula. American Mineralogist, 41 (1-2) 148-151
Plain TextZussman, J. (1956) Antigorite: Superlattice and structural formula. American Mineralogist, 41 (1-2) 148-151
In(1956) American Mineralogist Vol. 41 (1-2) Mineralogical Society of America

See Also

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Brindley, G. W. (1954) The structural formula of an antigorite from Venezuela. American Mineralogist, 39 (3-4) 391-392
Nagy, Bartholomew, Faust, George T. (1956) Serpentines: Natural mixtures of chrysotile and antigorite. American Mineralogist, 41 (11-12) 817-838
(1956) Book reviews. American Mineralogist, 41 (1-2) 162
Fleischer, M. (1956) New mineral names. American Mineralogist, 41 (1-2). 163-168
Donnay, Gabrielle, Kracek, F. C., Rowland, W. R. Jr. (1956) The chemical formula of empressite. American Mineralogist, 41 (9-10) 722-723
Brindley, G. W., Zussman, J. (1959) Infra-red absorption data for serpentine minerals. American Mineralogist, 44 (1-2) 185-188
McConnell, Duncan (1956) An unusual palagonite tuff. American Mineralogist, 41 (1-2) 153-155
Weibel, Max (1956) Amblygonite, cassiterite, and associated minerals from Caceres, Western Spain. American Mineralogist, 41 (1-2). p.41-48.
Hess, H. H., Smith, R. J., Dengo, and G. (1952) Antigorite from the vicinity of Caracas, Venezuela. American Mineralogist, 37 (1-2) 68-75
Wolff, G. A. (1956) Faces and habits of diamond type crystals. American Mineralogist, 41 (1-2) 60-66
Miyashiro, Akiho (1956) Osumilite, a new silicate mineral and its crystal structure. American Mineralogist, 41 (1-2) 104-116
 
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