Uppermost Ordovician through Lower Silurian conodont biostratigraphy of the Cape Phillips Formation, Cornwallis Island, Canadian Arctic Islands
Lower Silurian conodont biostratigraphy is poorly known and not well correlated with the parallel graptolite biozonation. The Cape Phillips Formation contains a continuous record of sedimentation, and exceptionally well preserved faunas in the unstable shelf region of the Franklinian miogeoclinal su...
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Format: | Thesis |
Language: | English |
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2000
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Online Access: | http://hdl.handle.net/1828/2946 |