UPb geochronological constraints on the tectonic evolution of the Grenville Province, western Labrador
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Molson Lake terrane consists principally of 1650 Ma granitoid gneisses, part of the Paleoproterozoic Trans-Labrador batholith, cut by dykes of the Mesoproterozoic Shabogamo gabbro.
“This terrane consists principally of 1650 Ma granitoid gneisses, part of the Paleoproterozoic Trans-Labrador batholith (Connelly and Heaman 1993; Connelly et al. 1995), cut by dykes of the Mesoproterozoic Shabogamo gabbro.”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Connelly and Heaman 1993
The age of HP metamorphism in Molson Lake terrane is not well constrained; two U/Pb (zircon) lower intercept ages of 1001 ± 10 Ma obtained on Shabogamo gabbro and Labradorian granite from the interior of the terrane are inferred to be minimum ages.
“The age of HP metamorphism in Molson Lake terrane is not well constrained; two U/Pb (zircon) lower intercept ages of 1001 ± 10 Ma (Connelly and Heaman 1993) obtained on Shabogamo gabbro and Labradorian granite from the interior of the terrane are inferred to be minimum ages.”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Connelly and Heaman 1993
Paleo- and Mesoproterozoic units in Gagnon terrane display evidence for a single metamorphism dated at about 1000 Ma (Rigolet orogeny).
“Paleo- and Mesoproterozoic units in Gagnon terrane display evidence for a single metamorphism that has been dated at about 1000 Ma (Connelly and Heaman 1993; Connelly et al. 1995; Schwarz 1998), i.e., Rigolet orogeny.”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Connelly and Heaman 1993
Subordinate rock types in Gagnon terrane include deformed and metamorphosed granitoid plutons and the distinctive 1459 ± 22/23 Ma Shabogamo gabbro, which forms sills and dykes in the Paleoproterozoic supracrustal succession.
“Subordinate rock types include deformed and metamorphosed granitoid plutons and the distinctive 1459 -+ 22 23 Ma Shabogamo gabbro, which forms sills and dykes in the Paleoproterozoic supracrustal succession (Connelly and Heaman 1993).”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Connelly and Heaman 1993
Lac Joseph terrane comprises a thin sheet of Paleoproterozoic sedimentary and plutonic rocks metamorphosed to upper amphibolite- to granulite-facies migmatitic gneiss during the Labradorian orogeny, with a window near the centre of the terrane through which the underlying HP belt is exposed.
“Lac Joseph terrane comprises a thin sheet of Paleoproterozoic sedimentary and plutonic rocks metamorphosed to upper amphibolite- to granulite-facies migmatitic gneiss during the Labradorian orogeny, with a window near the centre of the terrane through which the underlying HP belt is exposed (Fig. 3; Connelly and Heaman 1993).”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Connelly and Heaman 1993
Cited by
Sorted by citations
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
- Authors
- Connelly, J. N., & Heaman, L. M.
- Affiliations
- Memorial University of Newfoundland (CA)
- Royal Ontario Museum (CA)
- Corresponding author
- Connelly, J.N.
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 1993-09
- Volume
- 63
- Issue
- 1-2
- Pages
- 123-142
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W2037417788
- Cited by
- 70
- References
- 0
- Citations by year
- 2022: 1 · 2021: 2 · 2019: 1 · 2018: 2 · 2015: 1 · 2014: 1
- FWCI
- 4.99
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (publishedVersion)
- Funders
- Natural Sciences and Engineering Research Council of Canada
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological Studies and Exploration
- Social Sciences › Economics, Econometrics and Finance › Economics and Econometrics › Geochemistry and Geochronology of Asian Mineral Deposits
- Keywords
- Grenville orogeny, Grenville Province, U-Pb geochronology, ductile shear zones, migmatization, granitoid intrusion, Grenville Front, tectonic evolution
About these checks
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.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
