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A Tectono-metamorphic Framework For Part of the Grenville Province, Parry Sound Region, Ontario
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The southern limit of the Shawanaga domain coincides with a narrow zone of migmatitic paragneisses and amphibolites previously assigned to the Parry Sound domain.
“The southern limit of the Shawanaga domain coincides with a narrow zone of migmatitic paragneisses and amphibolites previously assigned to the Parry Sound domain (Figure 2) [Wodicka et al., 1996; cf.Davidson et al., 1982].”
From Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust (1997) · cites this paper as cf.Davidson et al., 1982
The Moon River domain structurally overlies the Parry Sound and Go Home domains.
“The Moon River domain structurally overlies the Parry Sound and Go Home domains (Figures 2 and 3) [Davidson et aL, 1982;Culshaw et al., 1990;Schwerdtner and van Berkel, 1991].”
From Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust (1997) · cites this paper as Davidson et aL, 1982
The Shawanaga domain is dominated by quartzofeldspathic paragneiss, amphibolite, and migmatitic granitoid orthogneiss.
“The Shawanaga domain (Figure 2) is dominated by quartzofeldspathic paragneiss, amphibolite, and migmatitic granitoid orthogneiss [Davidson et al., 1982; Culshmv et al., 1994].”
From Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust (1997) · cites this paper as Davidson et al., 1982
The Moon River domain is bounded by high-strain zones that cut earlier structures in adjacent units.
“The Moon River domain is bounded by high-strain zones that cut earlier structures in adjacent units (Figures 2 and 3) [Davidson et al., 1982].”
From Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust (1997) · cites this paper as Davidson et al., 1982
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Culshaw, N. G., Jamieson, R. A., Ketchum, J. W. F., Wodicka, N., Corrigan, D., & Reynolds, P. H. (1997) · Tectonics · doi:10.1029/97tc02285 · Cited by 108
Self-citationSchwerdtner, W. M., & van Berkel, J. T. (1991) · Precambrian Research · doi:10.1016/0301-9268(91)90055-f · Cited by 19
Gower, R. J. W. (1992) · Precambrian Research · doi:10.1016/0301-9268(92)90052-p · Cited by 14
Metadata
- Authors
- Davidson, A., Culshaw, N. G., & Nadeau, L.
- Affiliations
- Natural Resources Canada
- Published
- 1982
- Cited by
- 14
- References
- 0
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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