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Ribera Pluton
Stratigraphic label: [narc]rib
Map symbol: nArib

First published: 5 June 2018
Last modified:

 

 

 

 

 

 

 

 

 

 

 

 

Translation of original French

Informal subdivision(s)
Numbering does not necessarily reflect the stratigraphic position.
 
None
 
Author: Talla Takam et al., in preparation
Age: Neoarchean
Reference section: None
Type area: Emmanuel Lake area (NTS sheet 33A)
Geological province: Superior Province
Geological subdivision: Opatica Subprovince
Lithology: Biotite-magnetite granite
Type: Lithodemic
Rank: Lithodeme
Status: Formal
Use: Active

Background

The Ribera Pluton was introduced by Talla Takam et al. (in preparation) in the Emmanuel Lake (NTS sheet 33A09) and Léran Lake (sheet 23D12) areas to describe an elongated, highly magnetic granite intrusion along the Opinaca – Opatica contact. Previously, this pluton was part of the Misasque River massif described by Hocq (1985), a large felsic package of tonalite, granodiorite and granite.

Description

The Ribera Pluton mainly consists of massive granite, leucocratic, light grey-white in altered surface and pinkish grey-white in fresh exposure. It is medium to coarse grained and slightly foliated in places. The main minerals are quartz, plagioclase, microcline and magnetite. Quartz shows subgrains with undulatory extinction resulting from the effect of regional constraints. Microcline displays characteristic mesh polysynthetic twins and is observed in greater proportion than in other granites of the region. The rock is slightly sericitized and regularly shows myrmekite zones and perthitic or even antiperthitic textures in thin section. Biotite is rather scarce (0-3%) and partially to completely chloritized. The most common accessory minerals are epidote, sphene and apatite. To the west, the proportion of plagioclase increases with the appearance of hornblende, giving the rock a more granodioritic composition.

Thickness and Distribution

The Ribera Pluto extends E-W for ~50 km and has a maximum width of 10 km. Located between paragneiss and migmatites of the Laguiche Complex (nAlgi) to the north and foliated tonalites of the Misasque Complex (Amiq) to the south, it follows the Opinaca – Opatica contact in sheets 33A09 and 23D12.

Dating

None.

Stratigraphic Relationship(s)

The Ribera Pluton is late tectonic and was emplaced after the Laguiche and Misasque complexes. However, contacts between these units were not observed on outcrops.

Paleontology

Does not apply.

References

Author(s) Title Year of Publication Hyperlink (EXAMINE or Other)
HOCQ, M. Géologie de la région des lacs Campan et Cadieux, territoire-du-Nouveau-Québec. Ministère de l’Énergie et des Ressources, Québec; ET 83-05, 188 pages, 4 cartes. 1985 ET 83-05
TALLA TAKAM, F. – BEAUCHAMP, A.-B. – MASSEI, F. Géologie de la région des lacs Emmanuel et Léran, Ministère de l’Énergie et des Ressources naturelles, Québec. In preparation
15 octobre 2019