Cited by 3

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U-Pb zircon and baddeleyite ages from the Central Gneiss Belt, Ontario

van Breemen, O, Davidson, A·1990

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Crossref · 10.4095/129074

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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).”
  • 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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Authors
van Breemen, O., & Davidson, A.
Affiliations
Natural Resources Canada
Published
1990
Cited by
3
References
0

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