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The Laurentide and Innuitian ice sheets during the Last Glacial Maximum
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The relatively constant HI around 0.5 is interpreted as a product of peneplanation during glaciation that eroded and flattened the morphology in the study area.
“We interpret this result to be a product of peneplanation during glaciation that eroded and flattened the morphology in the study area”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Dyke et al. 2002
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El Niño-Like Climate Teleconnections in New England During the Late Pleistocene
Rittenour, T. M., Brigham-Grette, J., & Mann, M. E. (2000) · Science · doi:10.1126/science.288.5468.1039 · Cited by 112
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Metadata
- Authors
- Dyke, A. S., Andrews, J. T., Clark, P. U., England, J. H., Miller, G. H., Shaw, J., & Veillette, J. J.
- Venue
- Quaternary Science Reviews
- Publisher
- Elsevier BV
- Published
- 2002-01
- Volume
- 21
- Issue
- 1-3
- Pages
- 9-31
- ISSN
- 0277-3791
- Cited by
- 711
- References
- 1
- Language
- en
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