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Petrogenesis of LREE-rich pegmatitic granite dykes in the central Grenville Province by partial melting of Paleoproterozoic-Archean metasedimentary rocks: Evidence from zircon U-Pb-Hf-O isotope and trace element analyses

Turlin, François, Vanderhaeghe, Olivier, Gervais, Félix, André-Mayer, Anne-Sylvie, Moukhsil, Abdelali, Zeh, Armin, Solgadi, Fabien, I.P.T.N.·2019·Precambrian Research
DOI 10.1016/j.precamres.2019.02.009
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  • 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 Turlin et al. 2019

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Authors
Turlin, F., Vanderhaeghe, O., Gervais, F., André-Mayer, A.-S., Moukhsil, A., Zeh, A., Solgadi, F., & I.P.T.N.
ORCID
Venue
Precambrian Research
Publisher
Elsevier BV
Published
2019-07
Volume
327
Pages
327-360
ISSN
0301-9268
DOI
10.1016/j.precamres.2019.02.009
Cited by
28
References
3
Language
en
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