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Supracrustal faults of the St. Lawrence rift system, Québec: kinematics and geometry as revealed by field mapping and marine seismic reflection data
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The Ottawa-Bonnechere Graben is part of the Saint Lawrence failed rift segment with a complex tectonic history spanning several billion years.
“The OBG is a part of the Saint Lawrence failed rift segment that has a complex tectonic history spanning several billion years (Lamontagne et al. 2003, Tremblay et al. 2003, Tarayoun et al. 2018).”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Tremblay et al. 2003
The OBG fault zone is an aulacogen with vertically dominated slip and a poorly constrained lateral component.
“The OBG fault zone is an aulacogen with vertically dominated slip and a poorly constrained lateral component”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Tremblay et al. 2003
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Cited by
Sorted by citations
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
- Tremblay, A., Long, B., & Massé, M.
- Venue
- Tectonophysics
- Publisher
- Elsevier BV
- Published
- 2003-07
- Volume
- 369
- Issue
- 3-4
- Pages
- 231-252
- ISSN
- 0040-1951
- Cited by
- 40
- References
- 0
- Language
- en
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