Precambrian Research 133 (2004) 223–247 A sedimentary prelude to Marinoan glaciation, Cryogenian
Continental margin deposition between the Sturtian- and Marinoan-aged global glacial periods is represented in NW Canada by a siliciclastic-to-carbonate grand cycle. The Keele Formation, a 300–600 m thick carbonate and siliciclastic deposit, comprises the upper part of this interglacial cycle. Sedim...
Main Authors: | , , , , |
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Format: | Text |
Language: | English |
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2003
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.9640 http://geol.queensu.ca/people/narbonne/DayJamesNarbonneDalrymple_PCResearch_2004.pdf |