The Paleoproterozoic Sokoman Formation (ca. 1.88 Ga) of the Labrador Trough, eastern Canada, is a ca. 100-m-thick succession of interbedded iron formation and fine-grained, terrigenous clastic sedimentary rocks.Detailed examination of drill cores and outcrops indicates a dynamic paleoshelf where an oxygen-stratified water column, coastal upwelling of hydrothermally derived Fe and Si, as …

Labrador is the ring of Aphebian sedimentary and volcanic rocks surrounding the Superior Province (Fig. 1). Erosional remnants of the Circum-Ungava Geosyncline in the Belcher Fold Belt, the Cape Smith Belt and the Labrador Trough encircle the Archean gneisses of the Ungava Craton on the west, north, and east, re-spectively (Dimroth et al. 1970).

The Labrador Trough forms the western part of the larg- er New Québec Orogenic belt, which records the oblique convergence and collision of the Archean Superior Craton to

The Denault Formation was deposited in the southwestern portion of the Labrador Trough near Schefferville, Québec (Fig. 1, Fig. 2).The Labrador Trough is a belt of Paleoproterozoic rocks that extends from Ungava Bay southeast to Labrador City, which is located ca. 120 km south of Schefferville (Fig. 1; Gross, 1968, Dimroth, 1978, Wardle and Bailey, 1981, Clark and Wares, 2006).

A bit on the Geology. The Labrador Trough, or New Quebec Orogen, is a volcano-sedimentary fold-and-thrust belt that formed when the Southern Rae Craton accreted onto the Superior Craton at around 1.88 to 1.86 billion years ago. Three cycles of passive margin sedimentation in-filled extensional rift basins during the docking, which were later ...

GENERAL GEOLOGY Introduction The region offers a nearly complete cross-section through the Labrador Trough; the western boundary of the Trough enters the area at the southeastern corner of the Lace Lake sheet, from where it continues to the northwest and west-north-west, southwest of Lace lake and south of Pistolet lake. It

Bergeron, R. 1965. Geology and Mineral Resources of the Labrador Trough. Transactions of the New York Academy of Sciences, June: 842-843. Brown, J. 2018. Email to A. Krim, 13 December. Compass. 2017. The Move to the New Labrador City Hospital has Begun, 29 September. Dorion, H. 1991. Henri Dorion Debunks the Ten Great Myths about the Labrador ...

map The geology of the eastern margin Labrador Trough is comprised of a series of Paleoproterozoic (2.17 to 1.87 Ga) sedimentary and volcanic rocks, which have been subdivided into a series of distinct lithotectonic zones. Numerous mineral occurrences are known …

Exploration in Labrador has been concentrated in two areas: the Labrador Trough, in the western part of Churchill Province, and the "Central Mineral Belt" of Labrador, which extends eastward across the southern parts of Churchill and Nain Provinces. Mining in the Labrador portion of the Trough accounts for about half of Canada's iron ore ...

Labrador Trough, Canada ConNnus KUIN Department of Geology, Indianq Uniuersity Bl oomingt on, Indiana 4 740 I Abstract The Proterozoic iron-formation in the south-central part of the Labrador Trough is the product of primary sedimentation and of diagenesis, but south of the Grenville Front this

Geology Geologically, the Huckleberry Property is found within the Labrador Trough, a Paleoproterozoic supracrustal sequence located at the eastern margin of the Superior Province. The sequence was folded and metamorphosed during the New Quebec Orogen, which represents the collision between the Superior Craton and the Core Zone of the ...

• Magnetite ore with simple geology, and low in impurities • Naturally suited for production of high quality pellets and pellet feed • Comprehensive feasibility studies carried out on . LabMag. ... Labrador Trough have had a strong focus on . corporate responsibility, the …

The geology of the eastern Labrador Trough has previ-ously been mapped as part of regional mapping projects (Donaldson, 1966; Frarey, 1967; Wardle, 1982) and the Howse Lake area was mapped, in detail, by Findlay et al. (1990). The first geological exploration in the Labrador Trough was conducted in the 1890s by A.P. Low who noted the

Ore Geology Reviews, 65: 900-915. (Corresponding author) 10. Chung D, Zhou M-F, Gao J-F, Chen WT. (2015) In-situ LA–ICP-MS trace elemental analyses of magnetite: The late Palaeoproterozoic Sokoman Iron Formation in the Labrador Trough, Canada. Ore Geology Reviews, 65: 917-928 . 11.

Deposit Types. Deposit Types . The Labrador Trough contains four main types of iron deposits: Soft iron ores formed by supergene leaching and enrichment of the weakly metamorphosed cherty iron formation; they are composed mainly of friable fine-grained secondary iron oxides (hematite, goethite, limonite).. Taconites, the fine-grained, weakly metamorphosed iron formations with above average ...

Director of Geoscience - Firebag In Situ. Suncor Energy Inc. 2011 - Present10 years. Manage all aspects of geology and geophysics within a 180,000+ bopd producing property, including development planning and execution, wind-down, production support, regulatory, reserves, growth, and exploration.

Labrador Trough - Quebec.ca

connecting Labrador City to Happy Valley t Goose Bay. The staging area is easily accessible by truck. Geology and Mineralization The Labrador Trough consists of Paleoproterozoic (2.17 to 1.87 Ga) sedimentary and volcanic rocks, which extend along the eastern margin of the Archean Superior Craton to Ungava Bay. The Labrador Trough

General geology The Labrador Trough constitutes the western part of the New Québec Orogen (Hoffman, 1988), which is located east of the Archean Superior Province and is part of the Circum-Ungava Geosyn-cline. Together, the Circum-Ungava Geosyncline and …

The western half of the Labrador Trough, consisting of a thick sedimentary sequence, can be divided into three sections based on changes in lithology and metamorphism (North, Central and South). The Trough is comprised of a sequence of Proterozoic sedimentary rocks including iron formation, volcanic rocks and mafic intrusions known as the ...

Paleoenvironmental and taphonomic controls on the occurrence of Paleoproterozoic microbial communities in the 1.88 Ga Ferriman Group, Labrador Trough, Canada Precambrian Research March 25, 2012

Section snippets Regional geology. The Proterozoic 2.17–1.87 Ga fold and thrust belt of the Labrador Trough (Clark & Wares, 2006), extending 1100-km from the south of Ungava Bay to Grenville Front, is bounded by the northeastern margin of the Archean Superior Province and the southwestern margin of the Churchill Province (Fig. 1).The fold belt has an Archean basement represented by the ...

The Labrador Trough consists of Paleoproterozoic sedimentary and volcanic rocks that extends for more than 1100 km, from the northwest corner of Ungava Bay south to Lake Pletpi. It forms the western part of a larger orogenic belt called the New Québec Orogen¸ which records the oblique convergence and collision of the Archean Superior Craton ...

The Labrador Trough is located in western Labrador and northeastern Québec and contains several world-class iron-ore deposits. Several large coarse-grained metamor-phosed iron deposits (metataconites) are located in the Labrador City/Wabush area, and have been mined continu-ously since the 1960s. Current production comes from Carol

Geology. The Ungava Peninsula, ... The supracrustal rocks comprise nappes that form part of the Ungava and Labrador troughs. In the zone east of the Labrador Trough axis, the Paleoproterozoic deformation reworked the Archean rocks of the Douglas Harbour Domain, as well as the Paleoproterozoic diabase dykes. ...

Iron Ore exploration continues throughout the iron-rich Labrador trough and . The Provincial Department of Natural Resources can provide more details on Labrador's spectacular geology. Labrador West is open for business. Experience the opportunity. Experience the energy. Live large in Labrador West!

Regional Geology Labrador Trough 16 Geology of the Schefferville Area 17 Property Geology and mineralization 20 Iron Ore Deposit Types 20 . III. 2011 PROGRAM RESULTS . Prospecting and Sampling 22 Summary, Conclusions, and Recommendations 23 . References 24 . Assessment Report on Porky Lake Project, Western Labrador ...

To the west, the contact style is similar to the Labrador Trough and is formed by the Pointe-Reef, Lac Hérodier and Lac Keato faults. At its southern end, the Rachel-Laporte Domain pinches off at the Gill Lake Fault, which then directly brings the rocks of the Labrador Trough into contact with those of the Baleine Lithotectonic Domain.

Other articles where Labrador Trough is discussed: mineral deposit: Iron deposits: …of Michigan and Minnesota, the Labrador Trough deposits of Canada, Serra dos Carajas in Brazil, the Transvaal Basin deposits of South Africa, and the Hamersley Basin of Australia.

The Labrador Trough (or New Québec Orogen) is a NNW-SSE oriented fold-and-thrust belt, primarily composed of Archaean to Palaeoproterozoic volcanic and metasedimentary rocks (Hoffman, 1990, Henrique-Pinto et al., 2019). Pervasive westward imbricate thrusting occurred during oblique collision between the Superior and Southern Rae craton at 1.84 ...

History and Geology of the Labrador Trough. Par Serge Perreault, Géo., M.Sc., Paul Dumas, Géo., MBA. Focus Labrador Trough. Iron is one of the most abundant elements on Earth. Many types of mineral deposits contain iron associated with other elements and a wide range of minerals.

Let's talk geology . The Labrador Trough is a metavolcano-sedimentary fold-and-thrust belt that formed when the core zone accreted onto the Superior Craton at around 1.88 to 1.86 billion years ago. The rocks comprise a thick sedimentary sequence that consists of three cycles of passive margin sedimentation that in-fill transtensional rift ...

The New Quebec orogen, also known as the Labrador Trough, lies at the northeastern portion of the Superior craton and is related to ocean closure and collision with the southeastern portion of the Rae craton. At 1,900 and 1,800 million years ago, an ocean closure and collision with the Wisconian arc terrane resulted in the creation of the ...

The world-class Labrador Trough iron mining district has long been a bastion of stability in the often uncertain world of mining. Having produced more than 2 billion tonnes of ore over 50 years of continuous production, "The Trough" can claim a prominent place in the Canadian mining sector. Currently, with new mine openings, major expansions at existing operations, and key port and rail ...

Geology of the Arnaud River Region, Superior (Minto) and Churchill (Labrador Trough) Provinces, Kangirsuk Area, Nunavik, Quebec, CanadaProject for NTS sheets 24M, 24N, 25C and 25DCarl Bilodeau and Emmanuel Caron-CôtéBG 2018-04