Origin of Porewater Sulfate in an Ordovician Aquiclude of the Michigan Basin, Ontario: Insights from Stable Isotopes.
Low-permeability Ordovician shale and limestone formations of the Michigan Basin are a target of interest for a deep geological repository for the long-term isolation of low and intermediate-level radioactive waste. Porewater studies contribute to an understanding of the age and evolution of paleofl...
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| Format: | Others |
| Language: | en |
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Université d'Ottawa / University of Ottawa
2019
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| Online Access: | http://hdl.handle.net/10393/38742 http://dx.doi.org/10.20381/ruor-22994 |