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G. W. W., (1921) Geology of the Ningi Hills. Geological Magazine, 58 (2) 96 doi:10.1017/s0016756800090270

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Reference TypeJournal (article/letter/editorial)
TitleGeology of the Ningi Hills
JournalGeological Magazine
AuthorsG. W. W., Author
Year1921 (February)Volume58
Issue2
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800090270
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Mindat Ref. ID280044Long-form Identifiermindat:1:5:280044:2
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Full ReferenceG. W. W., (1921) Geology of the Ningi Hills. Geological Magazine, 58 (2) 96 doi:10.1017/s0016756800090270
Plain TextG. W. W., (1921) Geology of the Ningi Hills. Geological Magazine, 58 (2) 96 doi:10.1017/s0016756800090270
In(1921, February) Geological Magazine Vol. 58 (2) Cambridge University Press (CUP)

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Williams, Gerard W. (1921) Geology of the Ningi Hills. Geological Magazine, 58 (2) 94-95 doi:10.1017/s0016756800090269
Falconer, J. D. (1921) Geology of the Ningi Hills. Geological Magazine, 58 (5) 237 doi:10.1017/s0016756800090828
Williams, Gerard W., Rastall, R. H. (1920) Preliminary Notes on the Geology of the Ningi Hills Northern Nigeria. Geological Magazine, 57 (10) 434-447 doi:10.1017/s001675680010679x
Falconer, J. D. (1920) Geology of the Ningi Hills. Geological Magazine, 57 (11) 526-527 doi:10.1017/s0016756800107034
Lamplugh, G. W. (1921) The Age of the Shenley Limestone. Geological Magazine, 58 (3) 140 doi:10.1017/s0016756800090440
Jackson, J. Wilfrid (1921) Carboniferous Spiriferina. Geological Magazine, 58 (2) 96 doi:10.1017/s0016756800090282
Walker, W. T. (1921) Liverpool Geological Society. Geological Magazine, 58 (5) 236 doi:10.1017/s0016756800090798
Tyrrell, G. W. (1921) Some Points in Petrographic Nomenclature. Geological Magazine, 58 (11) 494-502 doi:10.1017/s0016756800105047
Gregory, J. W. (1921) The Glaciation of Ireland. Geological Magazine, 58 (5) 239 doi:10.1017/s0016756800090853
Walker, W. T. (1921) Liverpool Geological Society. Geological Magazine, 58 (6) 286-287 doi:10.1017/s0016756800091032
Evans, John W. (1921) The Staddon Grits. Geological Magazine, 58 (5) 239-240 doi:10.1017/s0016756800090865
 
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