The stratigraphy and structure of the"Keno hill quartzite" in Tombstone area, Central Yukon.
New stratigraphic evidence strongly suggests that the areally extensive "Lower Schist" and "Keno Hill Quartzite" (informal names), formerly included in the Precambrian Yukon Group, are Jurassic and Lower Cretaceous respectively. [.]
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| Format: | Thesis |
| Language: | English |
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McGill University
1966
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=67502 |
| Summary: | New stratigraphic evidence strongly suggests that the areally extensive "Lower Schist" and "Keno Hill Quartzite" (informal names), formerly included in the Precambrian Yukon Group, are Jurassic and Lower Cretaceous respectively. [.] |
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