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U–Pb constraints for the plutonic and tectonometamorphic evolution of Lake Melville terrane, Labrador and implications for basement reworking in the northeastern Grenville Province

Corrigan, D, Rivers, T, Dunning, G·2000·Precambrian Research
DOI 10.1016/s0301-9268(99)00054-6
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  • Anatectic metapelites are also reported in other locations of the Mid-P segment, including the 1.1Ga St Boniface group and the Lac Melville terrane, but their metamorphic history is poorly known.

    “Anatectic metapelites are also reported in other locations of the Mid-P segment, including the 1.1Ga St Boniface group (Corrigan and van Breemen1997) and the Lac Melville terrane (Corrigan et al. 2000) but their metamorphic history is poorly known.”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Corrigan et al. 2000

  • In the eastern and western parts of the Grenville Province, the Parautochthonous Belt and the adjacent part of the hinterland share similarities in ages and formation settings of protoliths and represent portions of similar crustal age domains reworked at different depths and times during the Grenvillian orogeny.

    “in the eastern and western parts of the Grenville Province the Parautochthonous Belt and the adjacent part of the hinterland share similarities in terms of ages and formation settings of protoliths (ex.Brit / Kiosk domains, e.g., Culshaw et al. 2016; Groswater Bay / Lac Melville / Mealy Mountain terranes, Corrigan et al. 2000) (Fig. 2) and represent portions of similar crustal age domains reworked”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Corrigan et al. 2000

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Metadata

Authors
Corrigan, D., Rivers, T., & Dunning, G.
Venue
Precambrian Research
Publisher
Elsevier BV
Published
2000-01
Volume
99
Issue
1-2
Pages
65-90
ISSN
0301-9268
DOI
10.1016/s0301-9268(99)00054-6
Cited by
34
References
1
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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