A new Lower Devonian rock unit in the Canadian Arctic Islands
A thin, shelf-type carbonate unit with an abundant shelly fauna of Lower Devonian age is developed in the vicinity of Drake Bay, northwestern Prince of Wales Island where it rests on a dolomitic western facies of the dominantly clastic Peel Sound Formation. These limestones and shales which contrast...
Published in: | Canadian Journal of Earth Sciences |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1969
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Online Access: | http://dx.doi.org/10.1139/e69-112 http://www.nrcresearchpress.com/doi/pdf/10.1139/e69-112 |