Lithotectonic elements of the Grenville Province: review and tectonic implications
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The arc and (or) back-arc terranes comprising the Composite Arc belt were assembled outboard of Laurentia at c45 1250-1225 Ma during the Elzevirian orogeny, shortly before their accretion to Laurentia.
“This nomenclature reflects current understanding that the arc and (or) back-arc terranes comprising the Composite Arc belt were assembled outboard of Laurentia at c45 1250-1225 Ma during the Elzevirian orogeny, shortly before their accretion to Laurentia (see also Rivers 1997; Corriveau and van Breemen 2000; Rivers and Corrigan 2000; Hanmer et al. 2000).”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Rivers 1997
Mesoproterozoic modifications to the architecture in the vicinity of cross-section E included continental-margin arc-related intrusions and supracrustal rocks and a prominent mafic dyke swarm (Shabogamo gabbro) that stitched several crustal elements.
“Mesoproterozoic modifications to this architecture included continental-margin arc-related intrusions and supracrustal rocks (not shown) and a prominent mafic dyke swarm (Shabogamo gabbro) that stitched several of the crustal elements (Rivers 1997; Rivers and Corrigan 2000).”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Rivers 1997
Prior to the Grenvillian collision, in the vicinity of cross-section E, the Laurentian margin had Labradorian metasediments (metamorphosed c45 1660 Ma) lying outboard of granitoid rocks of the Trans-Labrador batholith (emplaced at 1650 Ma), which lay outboard of Archean basement with an undeformed Paleoproterozoic supracrustal cover.
“The configuration of the Laurentian margin in the vicinity of cross-section E prior to the Grenvillian collision is schematically shown in Fig. 11A, with Labradorian metasediments (metamorphosed c45 1660 Ma) lying outboard of granitoid rocks comprising the Trans-Labrador batholith (emplaced at 1650 Ma), which in turn lay outboard of the Archean basement with a Paleoproterozoic supracrustal cover”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Rivers 1997
The province-wide Ottawa orogeny was a result of continent-continent collision.
“If the province-wide Ottawa orogeny was a result of continent-continent collision, as is commonly inferred (e.g., McLelland et al. 1996, 2001; Rivers 1997; Carr et al. 2000)”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Rivers 1997
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Mesoproterozoic paleogeography: Supercontinent and beyond
Pisarevsky, S. A., Elming, S.-Å., Pesonen, L. J., & Li, Z.-X. (2014) · Precambrian Research · doi:10.1016/j.precamres.2013.05.014 · Cited by 481 · see citing works
Bédard, J. H., Brouillette, P., Madore, L., & Berclaz, A. (2003) · Precambrian Research · doi:10.1016/s0301-9268(03)00181-5 · Cited by 118 · see citing works
The High Pressure belt in the Grenville Province: architecture, timing, and exhumation
Rivers, T., Ketchum, J., Indares, A., & Hynes, A. (2002) · Canadian Journal of Earth Sciences · doi:10.1139/e02-025 · Cited by 124 · see citing works
Self-citation
- Authors
- Rivers, T.
- Affiliations
- Memorial University of Newfoundland (CA)
- Corresponding author
- Rivers, Toby
- ORCID
- Rivers, Toby
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 1997-12
- Volume
- 86
- Issue
- 3-4
- Pages
- 117-154
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W2071578732
- Cited by
- 558
- References
- 0
- Citations by year
- 2026: 11 · 2025: 9 · 2024: 12 · 2023: 16 · 2022: 17 · 2021: 23 · 2020: 23 · 2019: 19 · 2018: 15 · 2017: 26 · 2016: 17 · 2015: 19 · 2014: 20 · 2013: 17 · 2012: 18
- FWCI
- 14.95
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (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 Province, Grenville orogeny, continental collision, subduction-accretion, magmatic arc, back-arc basin, accretionary orogeny, crustal shortening, Ottawan orogeny, Hastings group, anorthosite, alkali granite, Laurentian margin, Mesoproterozoic
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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