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Relevant bibliographies by topics / Churchill Province

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Academic literature on the topic 'Churchill Province'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "Churchill Province"

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Fueten, Frank, and Pierre-Yves F. Robin. "Structural petrology along a transect across the Thompson Belt, Manitoba: dip slip at the western Churchill–Superior boundary." Canadian Journal of Earth Sciences 26, no. 10 (1989): 1976–89. http://dx.doi.org/10.1139/e89-167.

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Early Proterozoic rocks and Archean gneisses of the Thompson Belt, east of the Churchill Province – Superior Province boundary, record the history of the Hudsonian Orogeny in this area. A structural study has been undertaken along a 45 km long corridor cutting across the width of the belt.Three blocks are defined along this transect, each characterized by a specific structural style and metamorphic history, Foliation and lineation data and the analysis of kinematic indicators from these blocks show that (i) the Thompson Belt has been an area of predominantly dip-slip movement for its recogniza

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Frost, C. D., and R. A. Burwash. "Nd evidence for extensive Archean basement in the western Churchill Province, Canada." Canadian Journal of Earth Sciences 23, no. 9 (1986): 1433–37. http://dx.doi.org/10.1139/e86-135.

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To determine the extent of reworked Archean crust in the western Churchill Province, we have examined Sm–Nd crustal residence ages of basement cores in southern Alberta and southwestern Saskatchewan along with crustal residence ages calculated for other Sm–Nd data available from the Churchill Province. The deep drill hole samples from the Interior Platform give Sm–Nd crustal residence ages that average 2.8 Ga. Granulites from northeastern Alberta and composite gneisses from northern Saskatchewan also provide Archean crustal residence ages. These data demonstrate that the presence of reworked A

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Gwiazda, Roberto H., Sidney R. Hemming, Wallace S. Broecker, Tullis Onsttot, and Chris Mueller. "Evidence from 40Ar/39Ar Ages for a Churchill province source of ice-rafted amphiboles in Heinrich layer 2." Journal of Glaciology 42, no. 142 (1996): 440–46. http://dx.doi.org/10.3189/s0022143000003427.

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Abstract40Ar/39Ar ages of most single ice-ratted amphiboles from Heinrich layer 2 (H2) from a core in the Labrador Sea, a core in the eastern North Atlantic and a core in the western North Atlantic range from 1600 to 2000 Ma. This range is identical to that for K/Ar ages from the Churchill province of the Canadian Shield that outcrops at Hudson Strait and forms the basement of the northern part of Hudson Bay. The ambient glacial sediment includes some younger and older grains derived from Paleozoic, Mesoproterozoic and Archean sources, but still the majority of the amphiboles have ages in the

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Gwiazda, Roberto H., Sidney R. Hemming, Wallace S. Broecker, Tullis Onsttot, and Chris Mueller. "Evidence from 40Ar/39Ar Ages for a Churchill province source of ice-rafted amphiboles in Heinrich layer 2." Journal of Glaciology 42, no. 142 (1996): 440–46. http://dx.doi.org/10.1017/s0022143000003427.

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Abstract40Ar/39Ar ages of most single ice-ratted amphiboles from Heinrich layer 2 (H2) from a core in the Labrador Sea, a core in the eastern North Atlantic and a core in the western North Atlantic range from 1600 to 2000 Ma. This range is identical to that for K/Ar ages from the Churchill province of the Canadian Shield that outcrops at Hudson Strait and forms the basement of the northern part of Hudson Bay. The ambient glacial sediment includes some younger and older grains derived from Paleozoic, Mesoproterozoic and Archean sources, but still the majority of the amphiboles have ages in the

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McNicoll, Vicki J., Réginald J. Thériault, and Michael R. McDonough. "Taltson basement gneissic rocks: UPb and Nd isotopic constraints on the basement to the Paleoproterozoic Taltson magmatic zone, northeastern Alberta." Canadian Journal of Earth Sciences 37, no. 11 (2000): 1575–96. http://dx.doi.org/10.1139/e00-034.

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The Taltson magmatic zone is a 300 km long, northerly trending belt of Archean to Paleoproterozoic granitic basement gneiss, amphibolite, supracrustal gneissic rocks, and voluminous Paleoproterozoic magmatic rocks underlying northeastern Alberta and the southwestern portion of the Northwest Territories. Taltson basement gneissic rocks exposed in the southern Taltson magmatic zone in northeastern Alberta are composed of a lithologically diverse suite of banded gneissic rocks, including amphibolitic gneiss, paragneiss, and metaplutonic gneiss. Metaplutonic gneissic rocks are predominant; six new

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Wardle, Richard J., Donald T. James, David J. Scott, and Jeremy Hall. "The southeastern Churchill Province: synthesis of a Paleoproterozoic transpressional orogen." Canadian Journal of Earth Sciences 39, no. 5 (2002): 639–63. http://dx.doi.org/10.1139/e02-004.

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The Paleoproterozoic southeastern Churchill Province (SECP) is located in the northeastern Canadian Shield of Labrador and Quebec. The SECP formed through the oblique collisions of the Archean Nain and Superior cratons with a third intervening Archean block, the core zone. The belt has a tripartite structure, comprising the Torngat Orogen (TO) formed by Nain craton core zone collision in the east, the core zone in the centre, and the New Quebec Orogen (NQO) formed by Superior craton core zone collision in the west. The SECP thus records transpressional development on the flanks of the Supe

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Corrigan, David, Natasha Wodicka, Christopher McFarlane, et al. "Lithotectonic Framework of the Core Zone, Southeastern Churchill Province, Canada." Geoscience Canada 45, no. 1 (2018): 1–24. http://dx.doi.org/10.12789/geocanj.2018.45.128.

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The Core Zone, a broad region located between the Superior and North Atlantic cratons and predominantly underlain by Archean gneiss and granitoid rocks, remained until recently one of the less well known parts of the Canadian Shield. Previously thought to form part of the Archean Rae Craton, and later referred to as the Southeastern Churchill Province, it has been regarded as an ancient continental block trapped between the Paleoproterozoic Torngat and New Quebec orogens, with its relationships to the adjacent Superior and North Atlantic cratons remaining unresolved. The geochronological data

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James, D. T., J. N. Connelly, H. A. Wasteneys, and G. J. Kilfoil. "Paleoproterozoic lithotectonic divisions of the southeastern Churchill Province, western Labrador." Canadian Journal of Earth Sciences 33, no. 2 (1996): 216–30. http://dx.doi.org/10.1139/e96-019.

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The southeastern Churchill Province (SECP) is a Paleoproterozoic system of orogens that formed during collision of the Nain and Superior cratons with a composite lithotectonic terrane that now forms the medial, metamorphic–plutonic core zone of the SECP. In western Labrador, the core zone consists of reworked Archean gneisses, Paleoproterozoic supracrustal rocks, and variably deformed 1.83–1.81 Ga granitic plutons. It is subdivided into three Paleoproterozoic lithotectonic domains (McKenzie River, Crossroads, and Orma), which are separated from each other by dextral transpressive high-strain z

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Patterson, Judith G. "The Amer Belt: remnant of an Aphebian foreland fold and thrust belt." Canadian Journal of Earth Sciences 23, no. 12 (1986): 2012–23. http://dx.doi.org/10.1139/e86-186.

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Aphebian supracrustal sequences occur as outliers throughout the northwestern portion of the Churchill Structural Province of the Canadian Shield. In the Amer Lake area, medium- to high-grade, polydeformed Archean rocks are unconformably overlain by the Amer supracrustal sequence, which comprises quartzite, carbonate, mafic volcanic, and meta-arkose and meta-pelitic units. This supracrustal sequence is interpreted as having been deposited under miogeoclinal conditions, transitional to exogeoclinal.The Amer sequence crops out in a broad, west-southwest-plunging synclinorium and contains evidenc

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Klasner, J. S., and E. R. King. "Precambrian basement geology of North and South Dakota." Canadian Journal of Earth Sciences 23, no. 8 (1986): 1083–102. http://dx.doi.org/10.1139/e86-109.

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Combined analysis of drill-hole, gravity, and magnetic data indicates that the buried Precambrian basement rocks of the Dakotas can be divided into several lithotectonic terranes. Eastern North Dakota and northeastern South Dakota are underlain by Archean gneiss. Except for the Black Hills region of South Dakota, where Archean rocks are also exposed, the western third of both Dakotas is underlain mainly by Early Proterozoic gneiss and metasedimentary rocks. Part of this region is underlain by Archean crust with an Early Proterozoic tectonic overprint. A broad transition zone of strongly overpr

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Dissertations / Theses on the topic "Churchill Province"

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Sanborn-Barrie, Mary. "Geology, geothermobarometry and geochronology of the high-P granulite-facies Kramanituar Complex, Western Churchill Province." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0016/NQ48336.pdf.

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Sanborn-Barrie, Mary Carleton University Dissertation Earth Sciences. "Geology, geothermobarometry and geochronology of the high-P granulite-facies Kramanituar Complex, Western Churchill Province." Ottawa, 1999.

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Godet, Antoine, and Antoine Godet. "Styles métamorphique et tectonique au Paléoprotérozoïque : exemple du sud-est de la province du Churchill, Québec, Canada." Doctoral thesis, Université Laval, 2020. http://hdl.handle.net/20.500.11794/38191.

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L’évolution progressive des conditions thermiques enregistrées dans les roches métamorphiques suggère que la géodynamique globale est passée d’un régime archéen peu mobile à la tectonique des plaques moderne telle que nous la connaissons. La présence de styles tectonométamorphiques contrastés au Paléoprotérozoïque implique que cette période est clé et transitoire, mais le moment de l’initiation de la transition, sa durée et son expression géologique sont encore largement débattus. Un des éléments de réponse se trouve dans la croûte moyenne à inférieure qui joue un rôle primordial lors de la c

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Vanier, Marc-Antoine, and Marc-Antoine Vanier. "Caractérisation des zones de cisaillement du sud-est de la Province de Churchill, Québec : un cas d'écoulement latéral en croûte-moyenne." Master's thesis, Université Laval, 2019. http://hdl.handle.net/20.500.11794/37137.

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Cette contribution présente une approche combinant les résultats de traitements et d’interprétations de données aéromagnétiques, d’une étude structurale de terrain, d’une analyse des axes-c du quartz et de la géochronologie U-Pb. Les résultats révèlent les caractéristiques principales de trois zones de cisaillement du sud-est de la Province de Churchill (SEPC) : i) une foliation subverticale et une linéation d’étirement subhorizontale, ii) une cinématique dextre le long des zones de cisaillement N-S, iii) une cinématique senestre le long des zones de cisaillement WNW-ESE et iv) des tectonites

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Peats, Jennifer. "Aviat diamonds: a window into the deep lithospheric mantle beneath the Northern Churchill Province." Master's thesis, 2011. http://hdl.handle.net/10048/1966.

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The northern Churchill Province is an intensely explored, yet poorly researched target area for diamonds. I examined the mantle sources and residence history of diamonds from Aviat, located on the Melville Peninsula. Aviat diamonds display a δ13C range extending far below the average mantle value of -5‰ indicating eclogitic sources must be present. Crustal protoliths, carrying the organic matter implied by strongly 13C depleted diamond compositions, likely were supplied via subduction. The main population of diamonds around -5‰ may be either eclogitic or peridotitic. The CL patterns and variat

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Pedreira, Pérez Rocio. "La Suite mafique-ultramafique de Nuvulialuk : une nouvelle séquence ophiolitique dans l’arrière-pays de la Zone Noyau du sud-est de la Province de Churchill (Québec)." Thèse, 2017. http://constellation.uqac.ca/4429/1/PedreiraPxE9rez_uqac_0862N_10387.pdf.

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La Suite mafique-ultramafique de Nuvulialuk est localisée près du contact entre la Zone Noyau et l’Orogène des Torngat, dans la partie sud-est de la Province de Churchill. Cette suite est formée de plusieurs corps plurikilométriques, orientés grossièrement N-S et distribués le long du Couloir de Déformation de Blumath. Une cartographie et un échantillonnage systématique de la Suite mafique-ultramafique de Nuvulialuk ont été effectués pendant l’été 2014. Ces travaux montrent qu’elle est composée de deux types de faciès : des roches ultramafiques et des roches mafiques, et qu’elles sont métamorp

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Books on the topic "Churchill Province"

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Anderson, Raymond R. Southern extension of the Churchill Province (Trans-Hudson orogenic belt) midcontinent strategic and critical minerals project: 1985 workshop report. U.S. Dept. of the Interior, Geological Survey, 1987.

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Winston, Churchill. The story of the Malakand field force. Dover Publications, 2010.

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Siracusa, Joseph M. Diplomatic History: A Very Short Introduction. 2nd ed. Oxford University Press, 2021. http://dx.doi.org/10.1093/actrade/9780192893918.001.0001.

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Diplomacy: A Very Short Introduction introduces the subject of diplomatic history, the critical study of the management of relations between nation-states. Based on significant historical case studies—the diplomacy of the American Revolution, the diplomatic origins of the Great War and its aftermath Versailles, the personal summitry behind the night Stalin and Churchill divided Europe, George W. Bush and the coming of the Iraq War, and diplomacy in the age of globalization—there are concrete examples of diplomacy in action while locating the universal role of negotiations. Through these exampl

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Faulkner, Marcus, and Christopher M. Bell, eds. Decision in the Atlantic. University Press of Kentucky, 2019. http://dx.doi.org/10.5810/kentucky/9781949668001.001.0001.

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The Battle of the Atlantic was the longest campaign of the Second World War. This volume highlights the scale and complexity of this bitterly contested campaign, one that encompassed far more than just attacks by German U-boats on Allied shipping. The team of leading scholars assembled here situate the German assault on seaborne trade within the wider Allied war effort and provide a new understanding of its place within the Second World War. Individual chapters offer original perspectives on a range of neglected or previously-overlooked subjects: how Allied grand strategy shaped the war at sea

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Book chapters on the topic "Churchill Province"

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Baxter, Colin F. "Lord Beaverbrook, RDX, and the Ministry of Supply." In The Secret History of RDX. University Press of Kentucky, 2018. http://dx.doi.org/10.5810/kentucky/9780813175287.003.0002.

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By the spring of 1940, Germany had won an overwhelming victory. The battle for France was lost, and in the summer of 1940 the Battle of Britain raged between the Luftwaffe and “The Few” for supremacy in the skies over Britain. Winston Churchill looked to the bomber as Britain’s only offensive weapon; however, British Bomber Command lacked numbers, and its bombs were small and deficient in explosive power. Lord Beaverbrook made strenuous efforts to obtain the explosive RDX developed at the Woolwich Arsenal, but the Ministry of Supply was unable to provide the huge quantities needed by Bomber Command.

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Dron, Jon. "Self-Organization in Social Software for Learning." In Social Computing. IGI Global, 2010. http://dx.doi.org/10.4018/978-1-60566-984-7.ch023.

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The Internet has long been touted as an answer to the needs of adult learners, providing a wealth of resources and the means to communicate in many ways with many people. This promise has been rarely fulfilled and, when it is, often by mimicking traditional instructor-led processes of education. As a large network, the Internet has characteristics that differentiate it from other learning environments, most notably due to its size: the sum of the value of a network increases as the square of the number of members (Kelly, 1998), even before aggregate effects are considered. Churchill (1943) said, “We shape our dwellings and afterwards our dwellings shape us.” If this is true of buildings then it is even more so of the fluid and ever-changing virtual environments made possible by the Internet. Our dwellings are no longer fixed but may be molded by the people that inhabit them. This article discusses a range of approaches that make use of this affordance to provide environments that support groups of adult learners in their learning needs.

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Young, Kenneth R., and Blanca León. "Tropical and Subtropical Landscapes of the Andes." In The Physical Geography of South America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195313413.003.0020.

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The Andes represent Earth’s longest mountain system and include some of the world’s highest peaks. The rugged relief found above 1,000 m elevation produces strong environmental gradients tied to dramatic changes in temperature, moisture, and atmospheric pressure. These physical factors provide the background to understanding Andean landforms and land cover. In this chapter, we review these factors and patterns, and the complicating influences of geology and human land use, for the tropical and subtropical portions of the Andes, above 1,000 m and from 11°N to 24°S, in Venezuela, Colombia, Ecuador, Perú, Bolivia, and northernmost Argentina and Chile. The tropical Andes are recognized as one of the most important regions in the world from the viewpoint of biodiversity conservation (Myers et al., 2000; Brooks et al., 2002). They are home to ancient human settlements and early civilizations (Burger, 1992; Bruhns, 1994; Dillehay, 1999), and large indigenous populations (Maybury-Lewis, 2002) living in some of the highest permanent settlements in the world. As a result, a better understanding of the physical geography of this complex region is important for sustainable development initiatives and other global environmental concerns. Historically important overviews have been written for this region by von Humboldt (1807), Troll (1931), and Ellenberg (1958). Country-level studies include those for Venezuela (Monasterio, 1980), Colombia (Cuatrecasas, 1958; Rangel, 2000), Ecuador (Whymper, 1896; Acosta Solís, 1968; Jørgensen and León-Yánez, 1999), Perú (Weberbauer, 1945; Young and León, 2001), and Bolivia (Navarro and Maldonado, 2002). Luteyn (1999) has assembled information on the plants of the high elevations of the northern Andes, Luteyn and Churchill (2000) have examined the plant communities of the tropical Andes, and Kappelle and Brown (2001) have provided descriptive accounts of the montane forests. Inspiring chronicles can be found in Steele (1964) and Botting (1973). In this chapter, we first describe the relationships among the physical environments and natural landscapes of the tropical and subtropical Andes. We then discuss the natural vegetation types to be found, as typified by the forests, shrublands, grasslands, high Andean types, and wetlands. Finally, we summarize key aspects of the role of historical biogeography and human influences on and within those landscapes.

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Copeland, Jack, and David Bolam. "Dollis Hill at War." In Colossus. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780192840554.003.0033.

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The Dollis Hill building was erected in 1933 as the headquarters of the Post Office Engineering Department Research Station. Here T. H. Flowers pioneered digital electronics. The imposing brick building looks out from its hilltop site over the suburbs of North London (see photograph 41). It housed what was probably the most active telecommunications research centre in Europe. The building still stands today. Now converted into condominiums, it flanks a road named Flowers Close. Dollis Hill (DH) supplied much of the cryptanalytical machinery for Bletchley Park. Another of its roles was to provide an emergency alternative to the underground Cabinet War Rooms in Whitehall. Early in the war a secret underground citadel was excavated at DH. A massive structure of reinforced concrete, the citadel extended three floors into the ground. It is said that Churchill took against the new bunker, and the War Cabinet met at DH only once. Gil Hayward joined the Post Office Research Station in 1934. He describes the ethos of the new research laboratory: I went to DH at the age of 16, straight from school. The Research Station had existed in permanent form for less than two years, having previously been accommodated in a series of wooden huts. ‘Research is the Door to Tomorrow’ was inscribed in stone above the main entrance to the new building. The atmosphere at DH was unique. Original thinking was encouraged and there was a substantial amount of freedom. Norman Thurlow entered the Engineering Department of the Post Office as a recruit some three years before the war. In 1942, he joined the Dollis Hill group and participated in Flowers’ engineering revolution. The Post Office included the post and telephone businesses. The Engineering Department served both operations for all engineering work, including R&D. The Research Branch at Dollis Hill consisted of several different groups. Among them were the telegraph, switching, and physics groups, headed by Frank Morrell, Tom Flowers, and Eric Speight, respectively. These three groups all became involved in some way with the Bletchley Park operation. The state of the art was defined by the telephone and telegraph systems.

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"construing the Berne Convention to say that all that was required was a positive right to claim authorship which the author may exercise as he wishes. Normally this will be by placing his name on copies of the work. The Green Paper noted that s 43 of the 1956 Act provided a useful remedy where the plaintiff is not a professional writer and could not therefore recover damages for loss of goodwill in a passing off action; the provision survives as s 84 of the 1988 Act. The Berne Convention also contains some latitude as to the right of integrity since Article 6 bis requires a right to object in cases only where actions in relation to an author’s work would be prejudicial to his honour or reputation. The government agreed with Whitford that exceptions such as the permitting of reasonable modifications (as in the Netherlands Copyright Act) should be made and that they would be in accordance with the Berne Convention. The Green Paper therefore proposed that the legislation should provide that no change should be made in any literary, dramatic, musical, artistic or cinematographic work without the author’s consent, with the exception of changes to which the author could not in good faith refuse consent. The Act embraces this principle by implication, not expressly, as it adopts the wording of the Berne Convention rather than that of the Green Paper. The Green Paper went on to propose that the rights would be exerciseable only by the author or, after his death, by his personal representative. Contravention of the rights would be actionable as a breach of statutory duty. The rights would not be assignable. However, the author would be permitted to waive his moral rights and such waiver would be binding on his successors in title. The moral rights would exist for the same period as economic rights. The White Paper promised legislation along the lines foreshadowed in the Green Paper, noting that while Whitford had doubted whether UK law had complied with the Brussels text of the Berne Convention, there was no doubt that amendment of the law was necessary to comply with the Paris text. Chapter 4 of the Act sets out the new rights. The rights to be protected are the minimum required to be protected by Berne – paternity and integrity. There is no equivalent to the French droit de divulgation (the right to control circulation of a work prior to its being completed for publication), the droit d’accès (mainly of artists to their paintings after sale), the droit de repentir (the right of withdrawal after publication, subject in German law to the payment of compensation to the publisher, of a work of which its author no longer approves). Nor is there a right to reacquire a work of which the author has disposed – such as Graham Sutherland might have found useful in the case of his portrait of Churchill – or a right of publication. The possibility of." In Sourcebook on Intellectual Property Law. Routledge-Cavendish, 1997. http://dx.doi.org/10.4324/9781843142928-70.

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Conference papers on the topic "Churchill Province"

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Behnia, P., J. Kerswill, G. Bonham-Carter, and J. Harris. "Prospectivity mapping for gold deposits hosted by iron formation, in a portion of Western Churchill Province that includes Melville Peninsula, Nunavut, Canada." In 2009 17th International Conference on Geoinformatics. IEEE, 2009. http://dx.doi.org/10.1109/geoinformatics.2009.5293437.

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van Rooyen, Deanne, and David Corrigan. "PLATE TECTONICS DURING THE 1.9 – 1.7 GA ASSEMBLY OF NUNA; EXAMPLES OF MODERN CRUSTAL COLLISION AND TRANSPORT PROCESSES FROM THE SOUTHEASTERN CHURCHILL PROVINCE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-353342.

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Webber, Jeffrey R., Michael L. Williams, Laurie L. Brown, Anna Ternova, Tim Shamus, and Michael J. Jercinovic. "FROM THIN SECTION TO AEROMAGNETIC ANOMALY, LINKING PETROLOGIC DATA AND GEOPHYSICAL SURVEYS TO HELP CONSTRAIN THE RETROGRADE HISTORY OF THE WESTERN CHURCHILL PROVINCE, CANADA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290628.

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Regan, Sean P., M. L. Williams, Lisa J. Grohn, et al. "TWO TRANSECTS ACROSS THE SNOWBIRD TECTONIC ZONE, WESTERN CHURCHILL PROVINCE: EXPLORING THE CONTINUITY OF THE RAE-HEARNE BOUNDARY AND ITS ROLE DURING THE GROWTH OF LAURENTIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286834.

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Tang, Weiyu, Wei Li, and Jianxin Zhou. "Evaluation of Frictional Pressure Drop Correlations During Flow Boiling of Refrigerants in Micro-Fin Tubes." In ASME 2020 Fluids Engineering Division Summer Meeting collocated with the ASME 2020 Heat Transfer Summer Conference and the ASME 2020 18th International Conference on Nanochannels, Microchannels, and Minichannels. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/fedsm2020-20130.

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Abstract Due to the widely commercial application of micro-fin tube and eco-friendly refrigerants, more general frictional pressure drop correlations is demanded for better prediction, and this study is aimed at compared existing correlations and provide guides for the furthermore improvement. Experimental data points for frictional pressure drop during flow boiling of refrigerants in horizontal micro-fin tubes were extracted from literature and our previous experimental work to evaluate numerous existing frictional pressure drop correlations and specify their applicability to meet the urgent

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Reports on the topic "Churchill Province"

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Gordon, T. M. Geochronology in the Churchill Province. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127276.

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Miller, A. R. Gold Metallogeny, Churchill Structural Province. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133345.

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Berman, R. G. Metamorphic map of the western Churchill Province, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/287320.

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Zaleski, E., S. Pehrsson, N. Duke, et al. Quartzite sequences and their relationships, Woodburn Lake group, western Churchill Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211098.

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Spratt, J. E., B. Roberts, D. Kiyan, and A. G. Jones. Magnetotelluric soundings from the Central Rae Domain of the Churchill Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292237.

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Peterson, T. D., S. Pehrsson, T. Skulski, and H. Sandeman. Compilation of Sm-Nd isotope analyses of igneous suites, western Churchill Province. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/285360.

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Janvier, V., S. Castonguay, P. Mercier-Langevin, et al. Geology of the banded iron formation-hosted Meadowbank gold deposit, Churchill Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296646.

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Paul, D., S. Hanmer, S. Tella, T. D. Peterson, and A N LeCheminant. Compilation, bedrock geology of part of the western Churchill Province, Nunavut - Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213530.

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Davis, W. J., and E. Zaleski. Geochronological investigations of the Woodburn Lake group, western Churchill Province, Northwest Territories: preliminary results. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/210060.

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Relf, C., C. Scott, I. Lépine, and A. Labelle. Geology and deformation history of the Nowyak Lake area, western Churchill Province, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208633.

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