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Bourbeau Sill
Stratigraphic label: [narc]bou
Map symbol: nAbou

First published: 3 April 2018
Last modified:

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Translation of original French

 

 

Informal subdivision(s)
Numbering does not necessarily reflect the stratigraphic position.
 
nAbou4 Granophyric quartz ferrogabbro and ferrodiorite
nAbou3 Diorite and quartz gabbro
nAbou2 Gabbro and leucogabbro
nAbou1 Websterite
 
Author:Duquette, 1970
Age:Neoarchean
Reference section:The typical Bourbeau Sill section described by Duquette (1982) consists of a north-south section on the road leading to the tower of Mount Cummings (UTM NAD83, Zone 18: 556398 mE, 5534753 mN). According to Duquette (1982, p. 22), the Bourbeau Sill includes in this section: “(a) a thin (0–25 m) layer of metaperidotite; (b) a thick (365 m) layer of leucometagabbro; and (c) a similarly thick layer of quartzic metaferrodiorite, dark green, changing in place to a white-patina sodic granophyry.”
Type area:None
Geological province:Superior Province
Geological subdivision:Abitibi Subprovince
Lithology:Mafic to ultramafic intrusive rocks
Type:Lithodemic
Rank:Lithodeme
Status:Formal
Use:Active

 

 

Background

The Bourbeau Sill stratigraphy was established by Duquette (1982) following mapping work in the Roy Township. Stratigraphic drillings east of Barlow Lake (Poitras, 1984) and the Cummings Lake roadway section were used to discuss petrology and geochemical characteristics. The study by Dubé and Guha (1987) details the stratigraphy and metallogenic potential of the Bourbeau Sill in the Cooke (Chapais) and Norbeau (Chibougamau) mines areas.

Description

The Bourbeau Sill (nAbou) consists of a thin layer of basal bronzite-clinopyroxene pyroxenite, overlain by massive subophitic leucogabbro and a large amount of ferrodiorite and quartz ferrogabbro. 

Bourbeau Sill 1 (nAbou1): Websterite

According to Duquette (1982, p. 23–24), websterite “consists of medium-grained crystals of uralitized augite (brownish ferrohastingite and green actinolite) and completely serpentinized olivine. The rock is dark green or black in fresh exposure but grey in altered surface”.

 

Bourbeau Sill 2 (nAbou2): Gabbro and Leucogabbro

According to Duquette (1982, p. 24): “Leucometagabbro, which varies in colour from whitish to greenish light grey, consists of cumulate equidimensional crystals, fine to medium-grained, of partially saussutirized andesine (An30-35) and a few larger crystals of highly uralitized and chloritized augite. All of these cumulates are coated with a fine mixture of leucoxenized sphene and ilmenite, quartz, chlorite, hornblende and epidote. Despite the presence of andesine in this rock, we preferred to call it metagabbro because its chemical composition, at least in its lower half, is clearly gabbroic. In its upper half, however, it may have an overall dioritic composition. As can be seen in most cumulates, leucometagabbro shows, in several places, a very well-developed rhythmic bedding, with each layer showing an abundance of augite crystals at its base and plagioclase at its summit. Likewise, the passage between these two types of mineral concentration occurs gradually throughout the same layer but abruptly from one layer to the next.” 

 

Bourbeau Sill 3 (nAbou3): Diorite and Quartz Gabbro

According to Duquette (1982, p. 25), the diorite and quartz diorite [quartz gabbro] unit “is a green rock that shows a widespread blasto-ophitic texture. Its main components are quartz, chlorite, epidote, carbonate and albite; the last three minerals come from plagioclase saussuritization and the two previous ones from pyroxene alteration. Accessory minerals are titanomagnetite, sphene and apatite. Quartz, which occurs in rock interstices, is easy to identify because it usually forms bluish grains that can reach 8 mm in diameter and occupy, near the top of the sill, up to 20% of the rock volume. Its abundance, however, gradually decreases as you move away from the top of the sill. In its lower half, quartzic metaferrodiorite [quartz gabbro] is consistently medium grained. Elsewhere, it varies considerably because, in many places, there are fine-grained dioritic phases across much coarser-grained phases or vice versa. This is clearly self-intrusion which, with the rock’s blastoophitic texture, demonstrates that it cannot be a cumulate.”

 

Bourbeau Sill 4 (nAbou4): Granophyric Quartz Ferrogabbro and Ferrodiorite

According to Duquette (1982, p. 25), granophyric ferrogabbro and ferrodiorite are “a microscopic quartz-albite-epidote intergrowth, spotted with small albite phenocrystals”. West of Chapais, in the Maryse Lake area (northeast of sheet 32G14-200-0101), the Bourbeau Sill consists of up to 20 m of pyroxenite (nAbou1) and 35  m to 70 m of ophitic gabbro (nAbou2). Its sommital part, which outcrops sporadically south of Kapunapotagen Lake (northern portion of sheet 32G14-200-0101), consists of approximately 400 m of diorite, gabbro and leucocratic gabbro (nAbou3). We also identified in the same area some quartz-rich granitoid outcrops, which is the most differentiated portion of the Bourbeau Sill. In thin section, plagioclase and quartz crystal intergrowth is obliterated by chloritization and sericitization, while the interstitial space is filled by a carbonate-chlorite-magnetite-iron oxide assemblage.

 

Thickness and distribution

The Bourbeau Sill is 450 m to 750 m thick (Poitras, 1984). It is observed on both sides of the Chibougamau Anticline over 85 km (Duquette, 1982; Poitras, 1984).

Dating

A sample of quartz ferrodiorite collected east of the Norbeau Mine was dated 2716.7 +1.0/-0.4 Ma (Mortensen, 1993). 

Isotopic SystemMineralCrystallization Age (Ma)(+)(-)Reference(s)
U-PbZircon2716.71.00.4Mortensen, 1993

Stratigraphic Relationship(s)

The Bourbeau Sill overlays the Ventures Sill (Aven) and cut volcaniclastic and metasedimentary rocks of the Blondeau Formation. Peperitic textures observed at Marianne Lake and on the section of Cummings Lake imply that the Blondeau Formation sediments were not yet consolidated at the time of the Bourbeau Sill intrusion (Lefebvre, 1991; Bédard et al., 2009). Deposition of these sediments can therefore be considered synchronous to the intrusion (i.e., 2716.7 +1.0/-0.4 Ma). 

Paleontology

Does not apply.

References

Author(s)TitleYear of PublicationHyperlink (EXAMINE or Other)
BÉDARD, J.H. – LECLERC, F. – HARRIS, L.B. – GOULET, N.Intra-sill magmatic evolution in the Cummings Complex, Abitibi greenstone belt: Tholeiitic to calc-alkaline magmatism recorded in a subvolcanic conduit system. Lithos; volume 111, pages 47-712009Source
DUBÉ, B. – GUHA, J.Étude métallogénique du filon-couche de Bourbeau. Les indices aurifères – région de Chibougamau. Ministère de l’Énergie et des Ressources, Québec; MB 87-03, 37 pages.1987MM 87-03
DUQUETTE, G.Stratigraphie de l’Archéen et relations métallogéniques dans la région de Chibougamau. Ministère des Richesses naturelles, Québec; ES 008, 25 pages, 1 plan.1970ES 008
DUQUETTE, G.Demie nord des cantons de McKenzie et de Roy et quart nord-ouest du canton de McCorkill. Ministère de l’Énergie et des Ressources, Québec; DPV 837, 80 pages, 4 plans.1982DPV 837
LEFEBVRE, C.Étude de la genèse des pépérites et de leur contexte volcano-sédimentaire, Formation de Blondeau, Chibougamau, Québec. Université du Québec à Chicoutimi; Masters Thesis, 215 pages.1991Source
MORTENSEN, J.K.U-Pb geochronology of the eastern Abitibi subprovince. Part 1: Chibougamau – Matagami – Joutel region. Canadian Journal of Earth Sciences; volume 30, pages 11-28.1993Source
POITRAS, A.Caractérisation géochimique du Complexe de Cummings, région de Chibougamau-Chapais, Québec. Université du Québec à Montréal; Masters Thesis, 159 pages.1984

 

 

 

 

8 mai 2019