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U‐Pb evidence for polymetamorphic history of Huronian rocks within the Grenville Front Tectonic Zone east of Sudbury, Ontario, Canada
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The Grenville orogeny affected the SE sector of the Sudbury impact structure to yield a polydeformed upper amphibolite facies terrain with local evidence of anatexis.
“This affected the SE sector of the impact structure to yield a polydeformed upper amphibolite facies terrain with local evidence of anatexis (Corfu and Easton 2000).”
From Tectonic influences on the morphometry of the Sudbury impact structure: Implications for terrestrial cratering and modeling (2004) · cites this paper as Corfu and Easton 2000
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Research works printed but not linked: 68
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Cited by
Sorted by citations
Spray, J. G., Butler, H. R., & Thompson, L. M. (2004) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2004.tb00341.x · Cited by 75
Rousell, D. H., James, R. S., & Roth, T. M. (2025) · Canadian Journal of Earth Sciences · doi:10.1139/cjes-2023-0010
Metadata
- Authors
- Corfu, F., & Easton, R. M.
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2001-02
- Volume
- 172
- Issue
- 1-2
- Pages
- 149-171
- ISSN
- 0009-2541
- Cited by
- 36
- References
- 1
- Language
- en
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