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Landes, Kenneth K. (1933) Origin and classification of pegmatites. American Mineralogist, 18 (2) 33-55

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Reference TypeJournal (article/letter/editorial)
TitleOrigin and classification of pegmatites
JournalAmerican Mineralogist
AuthorsLandes, Kenneth K.Author
Year1933Volume18
Issue2
PublisherMineralogical Society of America
Download URLhttp://www.minsocam.org/ammin/AM18/AM18_33.pdf+
Mindat Ref. ID520061Long-form Identifiermindat:1:5:520061:4
GUID0
Full ReferenceLandes, Kenneth K. (1933) Origin and classification of pegmatites. American Mineralogist, 18 (2) 33-55
Plain TextLandes, Kenneth K. (1933) Origin and classification of pegmatites. American Mineralogist, 18 (2) 33-55
In(1933) American Mineralogist Vol. 18 (2) Mineralogical Society of America

See Also

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

Landes, Kenneth K. (1933) Origin and classification of pegmatites (Concluded)-Classification of pegmatites. American Mineralogist, 18 (3) 95-103
Landes, K. K. (1933), Origin and Classification of Pegmatites (concluded): Journal of Mineralogical Society of America, Vol. 18, No. 2, p.96
Landes, Kenneth K. (1935) Age and distribution of pegmatites. American Mineralogist, 20 (2) 81-105
Landes, Kenneth K. (1935) Colorado pegmatites. American Mineralogist, 20 (5) 319-333
Landes, Kenneth K. (1937) Pegmatites and hydrothermal veins. American Mineralogist, 22 (5) 551-560
Landes, Kenneth K. (1935) Age and distribution of pegmatites. American Mineralogist, 20 (3) 153-175
Landes, Kenneth K. (1925) The paragenesis of the granite pegmatites of central Maine. American Mineralogist, 10 (11) 355-411
Landes, Kenneth K. (1938) Origin of the Quebec phlogopite-apatite deposits. American Mineralogist, 23 (6) 359-390
Landes, Kenneth K. (1931) A paragenetic classification of the Magnet Cove minerals. American Mineralogist, 16 (8) 313-326
Landes, Kenneth K. (1929) E. E. Hesnard. American Mineralogist, 14 (5) 202
Landes, Kenneth K. (1946) Geological mineralogy. American Mineralogist, 31 (3-4) 131-134
 
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