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Cartier Granite

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Journal Article
Published: 26 June 2002
Canadian Journal of Earth Sciences (2002) 39 (6): 933–942.
...J.P. Siddorn; H.C. Halls Abstract Early Proterozoic Matachewan mafic dykes that cut the Archean Cartier granite – Levack Gneiss Complex north of the Sudbury Igneous Complex (SIC), Canada, are generally metamorphosed to lower amphibolite facies but exhibit locally unaltered plagioclase...
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Journal Article
Published: 01 April 2000
Canadian Journal of Earth Sciences (2000) 37 (1): 95–114.
..., at least at Rivière Héva, deformed by F 3 asymmetric folding. In contrast, mineralized quartz vein systems at Cartier Malartic are controlled by F 3 folding and overprinted by late-stage D 3 faults which host late quartz–tourmaline veins. Quartz vein textures are consistent with these timing relations...
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Journal Article
Published: 15 March 2021
Bulletin de la Société Géologique de France (2021) 192 (1): 7.
... dykes estimated around 329–315 Ma, suggesting a magmatic-hydrothermal transition for the ore-forming process. In the proposed model, the cooling of a hidden two-mica granitic pluton could have generated a magmatic fluid, and acted as the heat source responsible for fluid flow towards inherited...
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Image
Figure 7. Chondrite-normalized rare earth element abundances in <b>granitic</b> bl...
Published: 01 November 2005
Figure 7. Chondrite-normalized rare earth element abundances in granitic blocks compared to footwall granites from the South Range (Creighton and Murray) and the North Range (Cartier). The granite blocks (gray-shaded region) are similar to the nearby South Range plutons and are distinct from
Journal Article
Published: 01 March 2015
Bulletin de la Société Géologique de France (2015) 186 (2-3): 63–91.
... characterised by migmatites and granites, the coastal South Armorican domain, offers an opportunity to study deep-orogenic processes and more particularly, to understand the role of partial-melting for the late-evolution of the Variscan belt. To date, time-constraints are scarce hindering the understanding...
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Journal Article
Published: 01 May 2009
Bulletin de la Société Géologique de France (2009) 180 (3): 231–246.
... deformation and shear zone patterns in the Massif Armoricain and the French Massif Central. The synthesis of granite emplacement ages associated to granite deformation fields, allow us to propose a geodynamic model for the tectonic evolution of this part of the Variscan belt between 370 Ma – 320 Ma (Late...
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Journal Article
Published: 01 April 2000
The Canadian Mineralogist (2000) 38 (2): 287–317.
... and microcontinents between 2720 and 2690 Ma. The distribution of metamorphic events and facies is the result of three interrelated patterns. 1) There is a relationship between subprovince type, metamorphic grade and age, with granite–greenstone subprovinces generally preserving older greenschist- to lower...
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Regional geology map of the Sudbury Structure locating main features. Tecto...
in > Geophysics
Published: 01 January 2001
F IG . 1. Regional geology map of the Sudbury Structure locating main features. Tectonic domains: Archean Superior province, Proterozoic Southern province, Late Proterozoic Grenville province. Rock Formations: BGB = Benny Greenstone belt, CGC = Cartier Granite complex, LG = Levack Gneiss complex
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.243.01.15
EISBN: 9781862394919
... P-T path during Carboniferous time; peak P-T was around 800 °C at 9 kbar. The strain field that emerged under subsolidus conditions during prograde metamorphism controlled the initial distribution of granite melt produced by suprasolidus mica breakdown; the limited retrograde reaction...
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Journal Article
Published: 01 October 2009
Bulletin de la Société Géologique de France (2009) 180 (6): 473–481.
... at the expense of ortho- and paragneiss. They form kilometer-sized septa within the foliated Goulles leucogranitic pluton, which is in turn intruded by the non-foliated Glény two micas granite pluton. Monazite grains extracted from these three rock-types have been dated by the EPMA chemical method. Three...
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Journal Article
Published: 01 March 2021
Bulletin de la Société Géologique de France (2021) 192 (1): 3.
...Clément Montmartin; Michel Faure; Hugues Raimbourg The Montagne Noire located in the southern part of the French Massif Central represents the northern part of the South-Variscan Foreland. It is subdivided into three parts. The granite-migmatite Axial Zone dome is surrounded by non- or weakly...
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Journal Article
Published: 16 June 2014
Canadian Journal of Earth Sciences (2014) 51 (8): 750–774.
... was followed by its deformation and the development of a penetrative gneissic fabric during the ca. 2415 − ca. 2219 Ma Blezardian Orogeny. New laser ablation – inductively coupled plasma – mass spectrometry (LA–ICP–MS) U–Pb zircon ages of 2343 ± 17 and 2344 ± 47 Ma on two granitic dikes that cut this fabric...
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Journal Article
Published: 01 May 2009
Bulletin de la Société Géologique de France (2009) 180 (3): 247–261.
... zone, defined here as the “Sarzeau shear zone” (SSZ), separates Carboniferous migmatites and the S te -Anne d’Auray type anatectic granite from highly retrogressed micaschists in its footwall and hangingwall, respectively. Late Carboniferous leucogranite dykes, called the Sarzeau granite that intrude...
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Series: Special Publications of the Society of Economic Geologists, Special Publications of the Society of Economic Geologists
Published: 01 January 2010
DOI: 10.5382/SP.15.2.12
EISBN: 9781629490403
... is exposed on the property. The sedimentary-volcanic protolith of this complex ( Dressler, 1984 ) experienced upper amphibolite to granulite facies metamorphism at 2.65 Ga ( Krogh et al., 1984 ; James et al., 1991 ). Metamorphism was followed by emplacement of the postorogenic Cartier Granite batholith...
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Image
Geological map of the northern margin of the Sudbury Basin. BGB, Benny Gree...
Published: 26 June 2002
Fig. 1. Geological map of the northern margin of the Sudbury Basin. BGB, Benny Greenstone Belt; BDZ, Benny Deformation Zone; CG, Cartier granites; GP, Grenville Province; LGC, Levack Gneiss Complex; RAG, Ramsey–Algoma Gneisses; SIC, Sudbury Igneous Complex; WG, Whitewater Group. Large squares
Journal Article
Journal: GSA Bulletin
Published: 01 November 2005
GSA Bulletin (2005) 117 (11-12): 1427–1450.
...Figure 7. Chondrite-normalized rare earth element abundances in granitic blocks compared to footwall granites from the South Range (Creighton and Murray) and the North Range (Cartier). The granite blocks (gray-shaded region) are similar to the nearby South Range plutons and are distinct from...
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Journal Article
Published: 01 April 2005
American Mineralogist (2005) 90 (4): 607–618.
... such precise information (i.e., more than 30–40 data). Using the examples of monazites from three migmatites and one granite, we show how to select the most efficient method of age calculation according to the U and Th geochemistry of the grains, or grain domains, that we are trying to date. Three situations...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2423(16)
... sequences, and finally, the emplacement of late Variscan granodiorites and granites. Although not totally understood, the advent of Paleozoic rifting that culminated in the opening of the Rheic Ocean (named after the Greek mythical goddess Rhea) and correlative basins began in Early...
Journal Article
Published: 01 October 2009
Bulletin de la Société Géologique de France (2009) 180 (6): 461–471.
... (511 ± 6 Ma, South-Veporic basement) granitic orthogneisses and calcalkaline rhyolitic (482 ± 6 Ma) and dacitic (476 ± 7 Ma) metavolcanics (Gemeric basement), indicating a magmatic immature back arc setting. The ages point to Middle/Late Cambrian, Early and Late Ordovician magmatic phases, coeval...
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Journal Article
Published: 27 November 2018
Canadian Journal of Earth Sciences (2019) 56 (3): 321–334.
... isotope compositions of the shale show that the provenance is predominantly Grenvillian granite–gneissic rocks, which were widely exposed north of the basin, with little contribution from Taconic igneous rocks. The bulk composition and the presence of detrital kaolinite suggest that the Grenvillian source...
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