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Syn-orogenic magmatism over 100 m.y. in high crustal levels of the central Grenville Province: Characteristics, age and tectonic significance

Groulier, Pierre-Arthur, Indares, Aphrodite, Dunning, Gregory, Moukhsil, Abdelali, Jenner, George·2018·Lithos
DOI 10.1016/j.lithos.2018.04.025
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  • Data from the Escoumins supracrustal belt show a ca.1037 Ma age for the amphibolite-facies metamorphism (overgrowth on detrital zircon in quartzite).

    “and data from the Escoumins supracrustal belt (Fig. 3) show a ca.1037 Ma age for the amphibolite-facies metamorphism (overgrowth on detrital zircon in quartzite; Groulier et al. 2018)”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Groulier et al. 2018

  • In Quebecia and vicinity, there is an assortment of smaller granite/monzonite, mangerite and alkaline bodies emplaced intermittently between ca.1.08 and 1.02 Ga, the oldest of which (ca. 1086 Ma Bon-Desir granite) is exposed in the low-P Escoumins supracrustal Belt.

    “In Quebecia and vicinity, there is also an assortment of smaller granite/monzonite, mangerite and alkaline bodies emplaced intermittently between ca.1.08 and 1.02 Ga, the oldest of which (ca. 1086 Ma Bon-Desir granite) is exposed in the low-P Escoumins supracrustal Belt (Groulier et al. 2018).”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Groulier et al. 2018

  • Documented occurrences of S-type granites are limited to two Rigolet-age cases: two-mica granites in the low-P Escoumins supracrustal belt, suggesting crustal melting at depth, and peraluminous granitic pegmatites in the Mid-P segment above the Parautochthonous Belt in Manicouagan, linked to melting of underlying Paleoproterozoic and Archean crust.

    “Documented occurrences are limited to two Rigolet-age cases: two-mica granites in the low-P Escoumins supracrustal belt, suggesting crustal melting at depth (Groulier et al. 2018), and peraluminous granitic pegmatites in the Mid-P segment above the Parautochthonous Belt in Manicouagan, linked to melting of underlying Paleoproterozoic and Archean crust (Turlin et al. 2019).”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Groulier et al. 2018

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Metadata

Authors
Groulier, P.-A., Indares, A., Dunning, G., Moukhsil, A., & Jenner, G.
Venue
Lithos
Publisher
Elsevier BV
Published
2018-07
Volume
312-313
Pages
128-152
ISSN
0024-4937
DOI
10.1016/j.lithos.2018.04.025
Cited by
16
References
0
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Funders
  • Ministère de l'Énergie et des Ressources naturelles of Quebec (8449-2017-2018-01)
  • NSERC (200386)

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