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Thermal and rheological constraints on the earthquake depth distribution in the Charlevoix, Canada, intraplate seismic zone
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Seismicity in eastern Canada is dominated by reactivation of inherited structures, including paleo-plate boundaries.
“In addition, seismicity in eastern Canada is dominated by reactivation of inherited structures, which includes paleo-plate boundaries (Kumarapeli 1978, Lamontagne and Ranalli 1996, Rimando and Benn 2005, Rimando and Peace 2021).”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Lamontagne and Ranalli 1996
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Rheology of the lithosphere: Selected topics
Kirby, S. H., & Kronenberg, A. K. (1987) · Reviews of Geophysics · doi:10.1029/rg025i006p01219 · Cited by 695
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Gusti, U. K., Peace, A. L., & Rimando, J. (2023) · Canadian Journal of Earth Sciences · doi:10.1139/cjes-2022-0137 · Cited by 7
Metadata
- Authors
- Lamontagne, M., & Ranalli, G.
- Venue
- Tectonophysics
- Publisher
- Elsevier BV
- Published
- 1996-05
- Volume
- 257
- Issue
- 1
- Pages
- 55-69
- ISSN
- 0040-1951
- Cited by
- 57
- References
- 1
- Language
- en
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