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EMMONS, S. F. (1904) Theories of ore deposition historically considered. Geological Society of America Bulletin, 15 (1) 1-28 doi:10.1130/gsab-15-1

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Reference TypeJournal (article/letter/editorial)
TitleTheories of ore deposition historically considered.
JournalGeological Society of America Bulletin
AuthorsEMMONS, S. F.Author
Year1904 (January 1)Volume15
Issue1
PublisherGeological Society of America
DOIdoi:10.1130/gsab-15-1
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Mindat Ref. ID45694Long-form Identifiermindat:1:5:45694:8
GUID0
Full ReferenceEMMONS, S. F. (1904) Theories of ore deposition historically considered. Geological Society of America Bulletin, 15 (1) 1-28 doi:10.1130/gsab-15-1
Plain TextEMMONS, S. F. (1904) Theories of ore deposition historically considered. Geological Society of America Bulletin, 15 (1) 1-28 doi:10.1130/gsab-15-1
In(1904, January) Geological Society of America Bulletin Vol. 15 (1) Geological Society of America

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(1904) Index to Volume 15. Geological Society of America Bulletin, 15 (1) 619-636 doi:10.1130/gsab-15-619
Emmons, S. F. (1905) Theories of Ore Deposition Historically Considered. Scientific American, 60 (1563) 25046-25047 doi:10.1038/scientificamerican12161905-25046supp
Emmons, S. F. (1905) Theories of Ore Deposition Historically Considered. Scientific American, 60 (1564) 25062-25064 doi:10.1038/scientificamerican12231905-25062supp
Emmons, S. F. (1905) Theories of Ore Deposition Historically Considered. Scientific American, 60 (1565) 25078-25080 doi:10.1038/scientificamerican12301905-25078supp
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EMMONS, S. F. (1907) Uinta mountains. Geological Society of America Bulletin, 18 (1) 287-302 doi:10.1130/gsab-18-287
STEVENSON, J. J. (1904) Carboniferous of the Appalachian basin. Geological Society of America Bulletin, 15 (1) 37-210 doi:10.1130/gsab-15-37
CROOK, A. R. (1904) Molybdenite at Crown Point, Washington. Geological Society of America Bulletin, 15 (1) 283-288 doi:10.1130/gsab-15-283
EMMONS, S. F. (1890) Orographic Movements in the Rocky Mountains. Geological Society of America Bulletin, 1 (1) 245-286 doi:10.1130/gsab-1-245
 
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