Field evidence suggests that the Palaeoproterozoic Gowganda Formation in Canada is non-glacial in origin
During more than a century since its original identification, the Gowganda Formation in Ontario (Canada) has gradually been reinterpreted from representing mainly subglacial tillites to secondary gravity flow and glaciomarine deposits. The main pieces of geological evidence advanced in favour of gla...
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| Format: | Article |
| Language: | English |
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Sciendo
2021-08-01
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| Series: | Geologos |
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| Online Access: | https://doi.org/10.2478/logos-2021-0009 |