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1.1 Ga K-rich alkaline plutonism in the SW Grenville Province: U−Pb constraints for the timing of subduction-related magmatism

Corriveau, Louise, Heaman, Larry M., Marcantonio, Franco, van Breemen, Otto·1990·Contributions to Mineralogy and Petrology
DOI 10.1007/bf00286834
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  • Magmatism at ca. 1090 to 1080 Ma occurring in the Elzevir domain is not recorded in the Bancroft domain and the abundant syenites and pegmatites that intruded the Bancroft domain from 1075 to 1045 Ma have no known equivalents in the Elzevir domain.

    “Magmatism at ca. 1090 to 1080 Ma occurring in the Elzevir domain (Corriveau 1990;Corriveau et al. 1990) is not recorded in the Bancroft domain and the abundant syenites and pegmatites that intruded the Bancroft domain from 1075 to 1045 Ma (Table 1) have no known equivalents in the Elzevir domain.”

    From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Corriveau et al. 1990

  • Based on the sphene ages, metamorphism of the Sharbot Lake domain is contemporaneous with metamorphism in the Frontenac domain but not the Elzevir domain as previously implied.

    “Based on the sphene ages, metamorphism of the Sharbot Lake domain is contemporaneous with metamorphism in the Frontenac domain but not the Elzevir domain as previously implied (e.g., Davidson 1986;Corriveau 1990;Corriveau et al. 1990).”

    From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Corriveau et al. 1990

  • 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.”

    From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Corriveau et al. 1990

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Metadata

Authors
Corriveau, L., Heaman, L. M., Marcantonio, F., & van Breemen, O.
Venue
Contributions to Mineralogy and Petrology
Publisher
Springer Science and Business Media LLC
Published
1990-09
Volume
105
Issue
4
Pages
473-485
ISSN
  • 0010-7999
  • 1432-0967
DOI
10.1007/bf00286834
Cited by
42
References
1
Language
en
Licence
www.springer.com/tdm (tdm)

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