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Rénia Complex
Stratigraphic label: [arch]rea
Map symbol: Area

First published: 13 January 2020
Last modified:

 

 

 

  DISCLAIMER: This English version is translated from the original French. In case of any discrepancy, the French version shall prevail. 

Informal subdivision(s)
Numbering does not necessarily reflect the stratigraphic position.
 
Area2 Amphibolitized diorite and gabbro
Area1 Granitic gneiss
 
Author: Simard et al., 2013
Age: Archean
Stratotype: None
Type area: Kuujjuaq area (NTS sheet 24K)
Geological province: Churchill Province
Geological subdivision: Rachel-Laporte Lithotectonic Domain
Lithology: Gneiss
Category: Lithodemic
Rank: Complex
Status: Formal
Use: Active
Related unit(s)

None

Background

The Rénia Complex was described by Gélinas (1965) as a gneissic dome within the metasedimentary cover of the Rachel-Laporte Lithotectonic Domain. The author proposes that these gneiss form a structural dome exposing older rocks on younger rocks. The Rénia Complex groups rocks of the Rénia and Moyer complexes described by Gélinas (1965) and Simard et al. (2013), as well as part of the “Scattered Gneiss” described by Moorhead and Hynes (1990). These three units were once considered to be part of different thrust sheets (Moorhead and Hynes, 1990). However, the work of Lafrance et al. (2014) demonstrates that these units form a single large gneiss unit now assigned to the Rénia Complex. Thus, the terms “Moyer Complex” and “Scattered Gneiss” were abandoned.

 

Description

The Rénia Complex consists of two units: mostly granitic gneiss (Area1), and amphibolitized diorite and gabbro (Area2).

 

Rénia Complex 1 (Area1): Granitic Gneiss

Gneiss of unit Area1 is similar to that of Ungava Complex unit ApPung4, located directly to the east in the Baleine Domain. It is a granitic gneiss, more locally tonalitic, characterized by alternating grey and pink granitic bands, medium-grained, millimetre to centimetre-wide. A late granitic phase, coarse-grained to pegmatitic, possibly Paleoproterozoic, cuts gneiss on most outcrops. This phase injects parallel to gneissosity, accentuating banding. Unit Area1 gneiss contains brown to green biotite (5-15%) aligned with gneissosity, epidote (<3%) and muscovite. The main accessory minerals are chlorite, sphene, apatite, opaque minerals, hematite, zircon, allanite and carbonates. Granitic injections contain <5% ferromagnesian minerals, mostly magnetite and biotite.

 

Rénia Complex 2 (Area2): Amphibolitized Diorite and Gabbro

Amphibolitized diorite and gabbro of unit Area2 form enclaves and dismembered or boudinaged layers in unit Area1 gneiss. These enclaves and layers are decimetric to metric, but in places reach several hundred metres thick. The rock is homogeneous, foliated, medium to fine grained and dark greenish grey. It is mainly composed of green hornblende (30-60%) and granoblastic plagioclase; in several areas, there is also a significant garnet content (20-30%). Clinopyroxene has been observed locally and the main accessory minerals are biotite, sulphides, magnetite, epidote, chlorite, sphene and apatite.

 

Thickness and distribution

The Rénia Complex is located in the NW portion of the Saffray Lake area (Lafrance et al., 2014), where it forms a thrust sheet ~57 km long by 18 km wide. It is elongated in a NW-SE direction within the Rachel-Laporte Lithotectonic Domain.

 

Dating

Dating of a tonalitic gneiss sample, previously assigned to the Moyer Complex, yielded an early Neoarchean age of ~2883 Ma and a Paleoproterozoic metamorphic age of ~1793 Ma related to the New Quebec Orogenesis (Machado et al., 1989). Dating of a muscovite granitic gneiss sample of the Rénia Complex yielded a late Neoarchean age of ~2692 Ma and confirmed metamorphism around 1790 Ma. Archean ages are interpreted as those of gneiss protoliths and suggest a geological context similar to that of the Archean craton of the Superior Province, directly west of the Labrador Trough, where ancient tonalites are cut by younger granitic plutons (Simard et al., 2008).

Unit Sample Number Isotopic System Mineral Crystallization Age (Ma) (+) (-) Metamorphic Age (Ma)     Reference(s)
Area1 Moyer dome U-Pb Zircon 2883 6 6 1793 13 13 Machado et al., 1989
Area1 2012-MS-0063A U-Pb Zircon 2692 4 4 1790 20 20 Davis et al., 2015

Stratigraphic Relationship(s)

The Highfall Complex is part of a large thrust sheet separated in half by a thrust fault delineating two complexes: the Rénia Complex in the north and the Highfall Complex in the south. This sheet is composed of rocks that would originate from the Archean basement, and would have been emplaced within Paleoproterozoic volcano-sedimentary rocks of the Rachel-Laporte Lithotectonic Domain during the New Quebec Orogenesis (1.82-1.77 Ga). It is therefore in fault contact with Laporte Supersuite units. The northern section of the sheet is interpreted as having partially overthrusted the southern section towards the end of deformation. On the edge of the Lac Turcotte Fault, a granitic intrusion of the Mercier Suite (pPmrc2) cuts Archean rocks of the Rénia and Highfall complexes.

Paleontology

Does not apply.

References

Author(s) Title Year of Publication Hyperlink (EXAMINE or Other)

DAVIS, D.W. – MOUKHSIL, A., – LAFRANCE, I. – HAMMOUCHE, H. – GOUTIER, J. – PILOTE, P. – TALLA TAKAM, F.

Datations U-Pb dans les provinces du Supérieur, de Churchill et de Grenville effectuées au JSGL en 2012-2013. Ministère de l’Énergie et des Ressources naturelles, Québec; RP 2014-07, 56 pages.

2015 RP 2014-07
GÉLINAS, L. Région de la région de Fort Chimo et des lacs Gabriel et Thévenet, Nouveau-Québec. Thèse de doctorat, Université Laval, Québec; 212 pages. 1965
LAFRANCE, I. – SIMARD, M. – BANDYAYERA, D. Géologie de la région du lac Saffray (SNRC 24G-24F). Ministère des Ressources naturelles, Québec; RG 2014-02, 49 pages. 2014 RG 2014-02
MACHADO, N. – GOULET, N. – GARIEPY, C. U-Pb geochronology of reactivated Archean basement and of Hudsonian Trough. Canadian Journal of Earth Sciences, volume 26, pages 1–15. 1989
SIMARD, M. – LABBÉ, J.-Y. – MAURICE, C. – LACOSTE, P. – LECLAIR, A. – BOILY, M. Synthèse du nord-est de la Province du Supérieur (M. Simard, coordonnateur). Ministère des Ressources naturelles et de la Faune et des Parcs, Québec; MM 2008-02, 196 pages, 8 plans. 2008 MM 2008-02
SIMARD, M. – LAFRANCE, I. – HAMMOUCHE, H. – LEGOUIX, C. Géologie de la région de Kuujjuaq et de la Baie d’Ungava (SNRC 24J et 24K). Ministère des Ressources naturelles, Québec; RG 2013-04, 60 pages. 2013 RG 2013-04

 

 

 

10 février 2020