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High-P metamorphism in the Mesoproterozoic: Petrochronological insights from the Grenville Province
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Dated garnet in metamafic rocks from the interior of the High-P segment yielded Lu-Hf ages at 1033-1013 Ma, inferred to represent garnet growth.
“Dated garnet in metamafic rocks from the interior of this segment yielded Lu-Hf ages at 1033-1013 Ma, inferred to represent garnet growth, and younger Sm-Nd ages at ca. 1005 and 1003 Ma (Lotout et al. 2023).”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Lotout et al. 2023
Dated garnet in metamafic rocks from the interior of the High-P segment yielded younger Sm-Nd ages at ca. 1005 and 1003 Ma.
“Dated garnet in metamafic rocks from the interior of this segment yielded Lu-Hf ages at 1033-1013 Ma, inferred to represent garnet growth, and younger Sm-Nd ages at ca. 1005 and 1003 Ma (Lotout et al. 2023).”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Lotout et al. 2023
Taken together, the data are indicative of local late-Ottawan crustal thickening at the front of the Ottawan orogen, as it progressed against a rigid Archean ramp.
“Taken together, the data are indicative of local late-Ottawan crustal thickening at the front of the Ottawan orogen, as it progressed against a rigid Archean ramp (Lotout et al. 2023;Indares 2020).”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Lotout et al. 2023
On the hinterland side, the metamorphic age range of the High-P segment in central Grenville Province is late-to post-Ottawan, while extrusion of this segment over the Parautochthonous Belt occurred shortly after, during the Rigolet.
“On the hinterland side, the metamorphic age range of the High-P segment in central Grenville Province is late-to post-Ottawan (e.g., Lotout et al. 2023), while extrusion of this segment over the Parautochthonous Belt D r a f t 30 occurred shortly after, during the Rigolet (Labat et al. 2020).”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Lotout et al. 2023
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Cawood, P. A., & Hawkesworth, C. J. (2014) · Geology · doi:10.1130/g35402.1 · Cited by 232
Orogenic quiescence in Earth’s middle age
Tang, M., Chu, X., Hao, J., & Shen, B. (2021) · Science · doi:10.1126/science.abf1876 · Cited by 220
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The Grenville Province: revisiting the orogenic framework and integrating recent findings
Indares, A. (2025) · Canadian Journal of Earth Sciences · doi:10.1139/cjes-2023-0143 · Cited by 11
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Metadata
- Authors
- Lotout, C., Indares, A., Vervoort, J., & Deloule, E.
- ORCID
- Lotout, Caroline
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 2023-12
- Volume
- 399
- Pages
- 107208
- ISSN
- 0301-9268
- Cited by
- 8
- References
- 2
- Language
- en
- Licence
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
- www.elsevier.com/legal/tdmrep-license (tdm)
- www.elsevier.com/open-access/userlicense/1.0/ (am, 350 d)
- doi.org/10.15223/policy-017 (stm-asf)
- doi.org/10.15223/policy-037 (stm-asf)
- doi.org/10.15223/policy-012 (stm-asf)
- doi.org/10.15223/policy-029 (stm-asf)
- doi.org/10.15223/policy-004 (stm-asf)
- Funders
- H2020 Marie Skłodowska-Curie Actions
- European Commission Marie Sklodowska-Curie Actions (896746)
- Horizon 2020 Framework Programme
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