Cited by 84Geological and Geochemical AnalysisGeological Studies and ExplorationGeological and Geophysical Studies

SW Grenville Province, Canada: the case against post–1.4 Ga accretionary tectonics

Hanmer, S., Corrigan, D., Pehrsson, S., Nadeau, L.·2000·Tectonophysics

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Crossref · 10.1016/s0040-1951(99)00317-0

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1 of 1 references verified0 citation errors · 0 not checkable

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  • The Frontenac-Adirondack belt and contiguous parts of the Composite Arc belt carry evidence for penetrative deformation and greenschist- to granulite-facies metamorphism at 1190-1140 Ma (Shawinigan orogeny), suggesting that they were amalgamated at that time.

    “The Frontenac-Adirondack belt and contiguous parts of the Composite Arc belt carry evidence for penetrative deformation and greenschist- to granulite-facies metamorphism at 1190-1140 Ma (Shawinigan orogeny), suggesting that they were amalgamated at that time (Carr et al. 2000; Hanmer et al. 2000).”

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Authors
Hanmer, S., Corrigan, D., Pehrsson, S., & Nadeau, L.
Affiliations
Geological Survey of Canada (CA)
Corresponding author
Hanmer, S.
Venue
Tectonophysics
Publisher
Elsevier BV
Published
2000-03
Volume
319
Issue
1
Pages
33-51
ISSN
0040-1951 (ISSN-L)
OpenAlex
W2150572861
Cited by
84
References
1
Citations by year
2025: 1 · 2021: 6 · 2020: 5 · 2018: 2 · 2016: 3 · 2015: 3 · 2014: 4 · 2013: 8 · 2012: 6
FWCI
4.05
Type
journal article
Language
en
Open access
closed
Locations
Tectonophysics (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological Studies and Exploration
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
Keywords
Grenville orogen, accretionary tectonics, Mesoproterozoic, Central Metasedimentary Belt, Central Gneiss Belt, Adirondack Highlands, Mauricie, continental arc, Andean-type margin, Laurentia, granitoids, Precambrian crust

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