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(1876) Carboniferous and Post-Tertiary Polyzoa. Geological Magazine, S. 2 Vol. 3 (11) 522-523 doi:10.1017/s0016756800155645

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Reference TypeJournal (article/letter/editorial)
TitleCarboniferous and Post-Tertiary Polyzoa
JournalGeological Magazine
Year1876 (November)Series:Volume2:3
Issue11
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800155645
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Mindat Ref. ID264008Long-form Identifiermindat:1:5:264008:6
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Full Reference(1876) Carboniferous and Post-Tertiary Polyzoa. Geological Magazine, S. 2 Vol. 3 (11) 522-523 doi:10.1017/s0016756800155645
Plain Text(1876) Carboniferous and Post-Tertiary Polyzoa. Geological Magazine, S. 2 Vol. 3 (11) 522-523 doi:10.1017/s0016756800155645
In(1876, November) Geological Magazine S. 2 Vol. 3 (11) Cambridge University Press (CUP)

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(1876) South Australian Post-Tertiary Foraminifera and Ostracoda. Geological Magazine, S. 2 Vol. 3 (7) 334-335 doi:10.1017/s0016756800154949
(1880) IV.—On the Carboniferous Polyzoa. Geological Magazine, S. 2 Vol. 7 (11) 501-512 doi:10.1017/s0016756800151532
(1876) The “Sarsen Stones.”. Geological Magazine, S. 2 Vol. 3 (11) 523 doi:10.1017/s0016756800155657
(1876) Formation of Rock-Basins. Geological Magazine, S. 2 Vol. 3 (11) 523-525 doi:10.1017/s0016756800155669
(1876) Glacial Origin of Lake-Basins. Geological Magazine, S. 2 Vol. 3 (11) 521-522 doi:10.1017/s0016756800155633
(1887) Re “Explosive Slickensides”. Geological Magazine, S. 3 Vol. 4 (11) 522-523 doi:10.1017/s0016756800190521
(1887) Chert in Irish Carboniferous Rocks. Geological Magazine, S. 3 Vol. 4 (11) 521-522 doi:10.1017/s001675680019051x
(1876) II.—Notes on Carboniferous Mollusca. Geological Magazine, S. 2 Vol. 3 (4) 150-156 doi:10.1017/s0016756800154366
(1907) Reports and Proceedings. Geological Magazine, S. 5 Vol. 4 (11) 522-523 doi:10.1017/s0016756800133990
(1908) VI.—Geological Literature for 1907. Geological Magazine, S. 5 Vol. 5 (11) 522-523 doi:10.1017/s0016756800139123
(1890) IV.—Tertiary and Post-tertiary Stratigraphy. Geological Magazine, S. 3 Vol. 7 (9) 397-401 doi:10.1017/s0016756800188053
 
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