A Climate Model of the Deep (Neoproterozoic) Past
It has been commonly recognized that a series of global glaciation events occurred during the late Neoproterozoic Era (800 - 540 million years ago (Ma)). However, the extent of these glaciations continues to be hotly debated, namely whether the whole Earth was ice covered (ie. a “hard snowball”) or...
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| Language: | en_ca |
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2011
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| Online Access: | http://hdl.handle.net/1807/29792 |