A Late devonian reef tract on northeastern Banks Island, N.W.T.
Bibliography: p. 116-118. The exposed Upper Devonian succession on northeastern Banks Island, N.W.T. is 3700 feet thick and has been correlated with the Griper Bay Formation. It consists mainly of terrigenous elastic rocks which were deposited in a marine shelf to coastal complex environment. The so...
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Format: | Master Thesis |
Language: | English |
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University of Calgary
1970
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Online Access: | http://hdl.handle.net/1880/13661 https://doi.org/10.11575/PRISM/22817 |