Stable isotope ratios of carbonate and sulfide minerals from the Gunflint Formation: Evidence for the origin of iron formations.
The $\sim$1.9 Ga Gunflint Formation is a Lake Superior type iron-formation, located in the Thunder Bay district of northwestern Ontario, that was deposited on a shallow shelf analogous to modern carbonate environments. Carbonate minerals in the iron-rich lithofacies of the Gunflint Formation include...
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| Format: | Others |
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/5785 http://dx.doi.org/10.20381/ruor-14535 |