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Isotopic evidence for the crustal evolution of the Frontenac Arch in the Grenville Province of Ontario, Canada

Marcantonio, F., McNutt, R.H., Dickin, A.P., Heaman, L.M.·1990·Chemical Geology

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Crossref · 10.1016/0009-2541(90)90286-g

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  • Several granitic intrusions from the Frontenac domain yielded zircons with crystallization ages of 1173 to 1162 Ma and are up to 25 Ma older than granitic intrusions from the Lowlands.

    “Several granitic intrusions from the Frontenac domain yielded zircons with crystallization ages of 1173 to l162Ma (Marcantonio et al. 1990;van Breemen and Davidson 1990) and are up to 25 Ma older than granitic intrusions from the Lowlands (McLelland et al. 1988).”
  • Based on the occurrence of geochemically similar K-rich plutons belonging to an ultrapotassic to shoshonitic suite that intruded the northern segment of the Frontenac domain as well as the Sharbot Lake and the Elzevir domain at 1090 to 1076 Ma, these domains were assembled prior to the intrusion of the K-rich plutons.

    “Based on the occurrence of geochemically similar K-rich plutons belonging to an ultrapotassic to shoshonitic suite that intruded the northern segment of the Frontenac domain as well as the Sharbot Lake and the Elzevir domain at 1090 to 1076 Ma (Marcantonio et al. 1990;Corriveau 1990;Corriveau et al. 1990), these domains were assembled prior to the intrusion of the K-rich plutons.”
  • Elsewhere, the similarity of U-Pb zircon ages with the U-Pb sphene ages presented in this study and the peak metamorphic temperatures of ca. 700°C in the Frontenac domain indicate that initial cooling rates may have been as high as 10°C/Ma.

    “Elsewhere, the similarity of U-Pb zicron ages (e.g., Marcantonio et al. 1990;van Breemen and Davidson 1990) with the U-Pb sphene ages presented in this study and the peak metamorphic temperatures of ca.700~ in the Frontenac domain indicate that initial cooling rates may have been as high as 10~”

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Research works printed but not linked: 43

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Metadata

Authors
Marcantonio, F., McNutt, R. H., Dickin, A. P., & Heaman, L. M.
Venue
Chemical Geology
Publisher
Elsevier BV
Published
1990-06
Volume
83
Issue
3-4
Pages
297-314
ISSN
0009-2541
Cited by
69
References
0
Language
en

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