
Background
The term Kovik Antiform was introduced by Lamothe (2007) in order to describe Archean rocks forming the internal northern basement within the Ungava Orogen (units AKOV1 to AKOV10; Lamothe, 2007). However, this nomenclature adopted for a formal lithodemic unit does not comply with the North American Stratigraphic Code (NACSN, 1983, 2005). The units were thus reassigned to the Kovik Complex, Archean to Paleoproterozoic in age (Charette and Beaudette, 2018). The Kovik Antiform is the lithotectonic domain which contains rocks of the Kovik Complex. The unit was formally renamed the Kovik Lithotectonic Domain by Vanier and Lafrance (2020). The Kovik Complex consists of ten units (Appkvk1 to Appkvk10; Lamothe, 2007) that were aligned with the new nomenclature. As the Ministère’s mapping work is carried out, units of the Kovik Domain will be better defined and reassigned to separate suites according to their composition and genetic class, thus completely replacing the Kovic Complex.
Description
The Kovik Lithotectonic Domain forms an E-W oriented strip ~50 km wide in the central part of the Ungava Orogen. It is bordered to the south by the Ungava Trough (Northern and Southern domains). The northern contact, with the Narsajuaq Lithotectonic Domain, is marked by the Sugluk Shear Zone. Its longitudinal extension is poorly defined since rocks of the domain extend under the Hudson Bay to the west and under the Hudson Strait to the east.
Geology
All units in this lithotectonic domain were previously assigned to the Kovik Complex. This complex is an Archean to Paleoproterozoic package of orthogneiss, paragneiss and intrusive rocks. This package mainly includes tonalite or biotite ± hornblende ± epidote ± titanite ± allanite granodiorite (ApPkvk4, ApPkvk5 and ApPkvk6 units) displaying varying proportions of mafic and metasedimentary rock enclaves (Taylor, 1982; St-Onge and Lucas, 1990, 1992; St-Onge et al., 1992). In the western part of the domain, these lithologies are commonly migmatized and intruded by white to pinkish granitoids. Rare klippes of highly deformed silicoclastic metasedimentary rock (ApPkvk3) and extrusive or intrusive mafic igneous rock (Akvk1) are present in or near tonalitic intrusions. Late intrusions, metric to kilometric in width and ranging in composition from tonalitic to syenogranitic (ApPkvk7 to ApPkvk10), intrude into tonalites and granodiorites (St-Onge and Lucas, 1992).
New units were introduced in the Cape Wolstenholme (Charette and Beaudette, 2018) and Sirmiq Lake (Vanier and Lafrance, 2020) areas to better distinguish lithologies that were previously entirely grouped in the Kovic Complex. All the Kovik Domain units in these areas have been standardized using this new nomenclature. These units are presented in the table below.
ARCHEAN AND PALEOPROTEROZOIC UNITS | ||
pPnat | Nunatak Suite | Massive to slightly foliated granite, monzonite and quartz monzonite |
pPdrv | Derville Suite | Gabbro and ultramafic rocks, massive to slightly foliated |
pPgan | Gastrin Suite | Monzogabbro, gabbro and amphibolitized diorite; monzodiorite, diorite and monzonite |
pPuka | Uvikkaq Suite | Tonalite, quartz diorite and granodiorite |
pPavi | Arviq Suite | Porphyroid granodiorite, monzogranite and quartz monzodiorite |
pPgch | Guichaud Suite | Garnet anatectic granite |
pPcry | Crony Suite | Variably migmatized paragneiss, metatexite , diatexite, quartzite a nd amphibolite |
nAjin | Jinikkut Suite | Speckled quartz monzonite, monzonite and monzodiorite |
Anuk | Nanuk Complex | Felsic to intermediate gneiss and migmatites |
Geological Evolution
The Kovik Domain is a lithotectonic division of the Churchill Province. It is interpreted as a window on the parautochtonous Archaean basement, equivalent to rocks of the Superior Craton, resulting from their late uplift during the Ungava Orogeny (Lucas and St-Onge, 1992). Historically, three Archean ages (2882-2737 Ma) were obtained by Parrish (1989) and Scott and St-Onge (1995) from tonalite samples collected in the Kovik Domain. A Paleoproterozoic emplacement age obtained by Davis and Sutcliffe (2018) in one of the main units of the Kovik Lithotectonic Domain indicates that the latter does not consist solely of Archean units. Further dating is needed to properly define this lithotectonic package, the nature of which remains uncertain.
Similar to the conclusions of Baragar (2015), Charette and Beaudette (2018) note that the new field observations do not support the presence of a continuous fine imbrication of volcanic or metasedimentary rocks of the Povungnituk Group along the Kovik Domain, as suggested by St-Onge and Lucas (1992). Klippes of highly deformed, migmatized paragneiss were observed only in some areas where the Povungnituk Group had been mapped. According to the authors, it is not impossible that these are Archean paragneiss klippes.
References
Publications Available Through SIGÉOM Examine
CHARETTE, B., BEAUDETTE, M. 2018. Géologie de la région du cap Wolstenholme, Orogène de l’Ungava, Province de Churchill, sud-est d’Ivujivik, Québec, Canada. MERN. BG 2018-03, 2 plans.
DAVIS, D W., SUTCLIFFE, C N. 2018. U-Pb Geochronology of Zircon and Monazite by LA-ICPMS in Samples from Northern Quebec. UNIVERSITY OF TORONTO. MB 2019-01, 113 pages.
LAFRANCE, I., VANIER, M.-A., GÉLINAS, T.-K. 2023. Géologie de la région d’Amarurtuuq, Orogène de l’Ungava, Nunavik, Québec, Canada. MRNF; BG 2023-08, 1 plan.
LAMOTHE, D. 2007. LEXIQUE STRATIGRAPHIQUE DE L’OROGENE DE L’UNGAVA. MRNF. DV 2007-03, 66 pages and 1 plan.
VANIER, M.-A., LAFRANCE, I. 2020. Géologie de la région du lac Sirmiq, Orogène de l’Ungava, Nunavik, Québec, Canada. MERN. BG 2020-02, 1 plan.
Other Publications
BARAGAR, W.R.A., 2015. Geology of part of Kovik Bay map area (35-F). Geological Survey of Canada; Open File 7846, 21 pages. https://doi.org/10.4095/296431
LUCAS, S.B., ST-ONGE, M.R., 1992. Terrane accretion in the internal zone of the Ungava orogen, northern Quebec. Part 2: Structural and metamorphic history. Revue canadienne des sciences de la Terre; 1992, volume 29, n°4, pages 765-782. https://doi.org/10.1139/e92-065
NORTH AMERICAN COMMISSION OF STRATIGRAPHIC NOMENCLATURE (NACSN), 1983. North American Stratigraphic Code. American Association of Petroleum Geologists Bulletin, volume 67, pages 841-875. http://archives.datapages.com/data/bulletns/1982-83/data/pg/0067/0005/0800/0841.htm
NORTH AMERICAN COMMISSION OF STRATIGRAPHIC NOMENCLATURE (NACSN), 2005. North American Stratigraphic Code. American Association of Petroleum Geologists Bulletin, volume 89, pages 1547-1591. http://dx.doi.org/10.1306/07050504129
PARRISH, R.R., 1989. U-Pb geochronology of the Cape Smith Belt and Sugluk block, nothern Quebec. Geoscience Canada; volume 16, number 3, pages 126-130. https://journals.lib.unb.ca/index.php/GC/article/view/3609
SCOTT, D. J., ST-ONGE, M, R., 1995. Constraints on Pb closure temperature in titanite based on rocks from the Ungava orogen, Canada: Implications for U-Pb geochronology and PTt path determinations. Geology; volume 23, pages 1123-1126. https://doi.org/10.1130/0091-7613(1995)023%3C1123:COPCTI%3E2.3.CO;2
ST-ONGE, M.R., LUCAS, S.B., 1990. Evolution of the Cape Smith belt: Early Proterozoic continental underthrusting, ophiolite obduction and thick-skinned folding. In: The Early Proterozoic Trans-Hudson Orogen of North America (Lewry, J.F. and Stauffer, M.R., editors). Geological Association of Canada; special paper 37, pages 313-351.
ST-ONGE, M.R., LUCAS, S.B., 1992. New insight on the crustal structure and tectonic history of the Ungava Orogen, Kovik Bay and Cap Wolstenholme, Quebec. Geological Survey of Canada; Paper 92-1C, pages 31-41. https://doi.org/10.4095/132846
ST-ONGE, M.R., LUCAS, S.B., PARRISH, R.R., 1992. Terrane accretion in the internal zone of the Ungava orogen, nothern Quebec. Part 1: Tectonostratigraphic assemblages and their tectonic implications. Canadian Journal of Earth Sciences; volume 29, pages 746-764. http://doi.org/10.1139/e92-064
TAYLOR, F.C., 1982. Reconnaissance geology of a part of the Canadian Shield, northern Quebec and Northwest Territories. Commission géologique du Canada; Mémoire 399, 32 pages. http://dx.doi.org/10.4095/109241
Suggested Citation
Ministère des Ressources naturelles et des Forêts (MRNF). Kovik Lithotectonic Domain. Quebec Structural Lexicon. https://gq.mines.gouv.qc.ca/lexique-stratigraphique/province-de-churchill/antiforme-de-kovik_en [accessed on Day Month Year].
Contributors
First Publication |
Benoit Charette, P. Geo., M.Sc. benoit.charette@mern.gouv.qc.ca; Mélanie Beaudette, GIT, B.Sc. melanie.beaudette@mern.gouv.qc.ca (redaction) Mehdi A. Guemache, P. Geo., Ph.D. (coordination); Mélina Langevin, GIT, B.Sc. (critical review); Simon Auclair, P. Geo., M.Sc. (editing); Céline Dupuis, P. Geo., Ph.D. (English version); Ricardo Escobar Moran (HTML editing). |
Revision(s) |
Isabelle Lafrance, P. Geo., M.Sc. isabelle.lafrance@mern.gouv.qc.ca; Marc-Antoine Vanier, Eng., M.Sc. marc-antoine.vanier@mern.gouv.qc.ca (redaction) Mehdi A. Guemache, P. Geo., Ph.D. (coordination); Benoit Charette, P. Geo., M.Sc. (critical review); Simon Auclair, P. Geo., M.Sc. (editing); Céline Dupuis, P. Geo., Ph.D. (English version); Ricardo Escobar Moran (HTML editing). |