Relevant bibliographies by topics / Tasiujaq

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  2. Dissertations / Theses
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Academic literature on the topic 'Tasiujaq'

Author: Grafiati
Published: 25 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Tasiujaq"

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GRANDMONT, KATERINE, JEFFREY A. CARDILLE, DANIEL FORTIER, and TANIA GIBÉRYEN. "ASSESSING LAND SUITABILITY FOR RESIDENTIAL DEVELOPMENT IN PERMAFROST REGIONS: A MULTI-CRITERIA APPROACH TO LAND-USE PLANNING IN NORTHERN QUEBEC, CANADA." Journal of Environmental Assessment Policy and Management 14, no. 01 (March 2012): 1250003. http://dx.doi.org/10.1142/s1464333212500032.

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Northern Quebec (Nunavik) presents an important intersection between population growth and climate change. The Inuit population of Nunavik has the fastest growth rate in any region of Canada. Land-use planning is an urgent and pressing need for northern communities built on permafrost, where there are considerable risks to development in areas where permafrost may thaw. As northern communities work to adapt to climate changes, they will be in great need of confident recommendations about locations of future development projects. This paper presents a case-study of the community of Tasiujaq and assesses the probability of thaw settlement of the surface, a process seriously affecting infrastructure stability. A method is developed for quantifying uncertainty in the resulting map, expressed as a function of judgmentbased uncertainty in the various factors that can influence eventual map quality. The best estimate of vulnerability and of the confidence in that estimate can be expressed in a single, simple map that allows an analyst to convey both of these vital aspects of the assessment process.
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Omari, Khalid, René Chenier, Ridha Touzi, and Mesha Sagram. "Investigation of C-Band SAR Polarimetry for Mapping a High-Tidal Coastal Environment in Northern Canada." Remote Sensing 12, no. 12 (June 16, 2020): 1941. http://dx.doi.org/10.3390/rs12121941.

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Synthetic Aperture Radar (SAR) has been used in characterizing intertidal zones along northern Canadian coastlines. RADARSAT-2, with its full polarimetric information, has been considered for monitoring these vulnerable ecosystems and helping enhance the navigational safety of these waters. The RADARSAT Constellation Mission (RCM) will ensure data continuity with three identical SAR satellites orbiting together, providing superior revisit capabilities. The three satellites are equipped with multiple configurations, including single-polarization (HH, HV, VV), conventional (HH-HV, VV-VH, and HH-VV), hybrid (i.e., compact) dual polarization, and fully polarimetric (FP) modes. This study investigates the potential of the compact polarimetric (CP) mode for mapping an intertidal zone located at Tasiujaq village on the southwest shore of Ungava Bay, Quebec. Simulated RCM data were generated using FP RADARSAT-2 images collected over the study site in 2016. Commonly used tools for CP analysis include Raney m-delta classification and the hybrid dual polarizations RH-RV (where the transmitter is right-circular and the receivers are horizontal and vertical linear polarizations) and RR-RL (where the transmitter is right circular and the receivers are right-circular and left-circular polarizations). The potential of CP is compared with single, conventional dual-pol, and FP. The Freeman–Durden and Touzi discriminators are used for FP analysis. The random forest classifier is used as a classification approach due to its well-documented performance compared to other classifiers. The results suggest that the hybrid compact (RR-RL and RH-RV) dual polarizations provide encouraging separability capacities with overall accuracies of 61% and 60.7%, respectively, although they do not perform as well as conventional dual-pol HH-HV (64.4%). On the other hand, the CP polarimetric m-delta decomposition generated slightly less accurate classification results with an overall accuracy of approximately 62% compared to the FP Freeman–Durden (67.08%) and Touzi discriminators (71.1%).
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Feininger, Tomas, and Ingo Ermanovics. "Geophysical interpretation of the Torngat orogen along the North River – Nutak transect, Labrador." Canadian Journal of Earth Sciences 31, no. 4 (April 1, 1994): 722–27. http://dx.doi.org/10.1139/e94-064.

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A 19.3 mGal (1 Gal = 1 cm/s2) positive Bouguer gravity anomaly and a broad aeromagnetic low coincide with the Tasiuyak domain of the early paleo-Proterozoic Torngat orogen. The domain evolved during the collision of the western margin of the Archean Nain Province with an inferred, eastward-facing, platform-to-rise, sedimentary wedge sited on a proto-continent of Churchill (Rae) Province.A density contrast of +0.065 g∙cm−3 was measured between rocks of the Tasiuyak domain and those of the flanking Lac Lomier complex of the orogen and Nain Province. Using this contrast, a two and one-half dimensional model shows that rocks of Tasiuyak domain constitute a triangular prismatic body with maximum thickness of 13 km adjacent to Nain Province, which thins westward to a feather edge. The model is compatible, qualitatively, with the aeromagnetic anomaly and consonant with geological interpretation of an eastward-facing and thickening continental slope deposit. Deep exhumation of the Torngat orogen may account for the absence of paired gravity anomalies characteristic of many sutures elsewhere in the Canadian Shield.
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Edwards, Kevin J., J. Edward Schofield, and Dmitri Mauquoy. "High resolution paleoenvironmental and chronological investigations of Norselandnámat Tasiusaq, Eastern Settlement, Greenland." Quaternary Research 69, no. 1 (January 2008): 1–15. http://dx.doi.org/10.1016/j.yqres.2007.10.010.

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High-resolution paleoenvironmental data from a peat profile with a small pollen source area are used to reconstruct the impacts oflandnámon vegetation and soils at a Norse farm complex (∅2 at Tasiusaq) comprising two farms in the Eastern Settlement of Greenland. Analyses include the AMS14C dating of plant macrofossil samples and the use of Bayesian radiocarbon calibration to construct improved age–depth models for Norse cultural horizons. The onset of a regionallandnámmay be indicated by the clearance ofBetula pubescenswoodland immediately prior to local settlement. The latter is dated to AD 950–1020 (2σ) and is characterised by possible burning ofBetula glandulosascrub to provide grassland pasture for domestic stock. Clearance and grazing resulted in accelerated levels of soil erosion at a westerly farm. This was followed by an easterly migration of settlement and agriculture. Site constraints prevent an assessment of the demise of the easterly farm, but pressures of overgrazing and land degradation may have been the major factors responsible for the abandonment of the earlier farm.
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Panagiotakopulu, Eva, and Paul Christopher Buckland. "Late Holocene environmental change in southwest Greenland - fossil insect assemblages from Tasiusaq." Boreas 42, no. 1 (September 28, 2012): 160–72. http://dx.doi.org/10.1111/j.1502-3885.2012.00277.x.

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Mitchell, R. K., A. Indares, and B. Ryan. "High to ultrahigh temperature contact metamorphism and dry partial melting of the Tasiuyak paragneiss, Northern Labrador." Journal of Metamorphic Geology 32, no. 6 (April 17, 2014): 535–55. http://dx.doi.org/10.1111/jmg.12086.

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Tettelaar, Tanya, and Aphrodite Indares. "Granulite-facies regional and contact metamorphism of the Tasiuyak paragneiss, northern Labrador: textural evolution and interpretation." Canadian Journal of Earth Sciences 44, no. 10 (October 1, 2007): 1413–37. http://dx.doi.org/10.1139/e07-029.

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The Tasiuyak paragneiss at the western margin of the Nain Plutonic Suite has been subjected to two granulite-facies metamorphic events: (i) regional metamorphism during the Paleoproterozoic Torngat orogeny, and (ii) contact metamorphism due to emplacement of the Mesoproterozoic Nain Plutonic Suite. Regional metamorphism led to partial melting of pelitic rocks and the development of a locally well-preserved sequence of prograde and retrograde textures. These textures are partly controlled by bulk composition and formed in the pressure–temperature (P–T) field of the continuous reaction: biotite + sillimanite + plagioclase + quartz = garnet + K-feldspar + melt, along a hairpin P–T path with peak conditions of ~8–10 kbar (0.8–1.0 GPa) and up to 870 °C in the NaKFMASH (Na2O–K2O–FeO–MgO–Al2O3–SiO2–H2O) system. These textures controlled the development of the contact metamorphic assemblages. Contact metamorphism of the pelitic rocks between the Tessiarsuyungoakh intrusion and the Makhavinekh Lake pluton led to growth of orthopyroxene-cordierite symplectite after garnet–biotite, and cordierite–spinel symplectite after garnet–sillimanite. These phase associations attest to reactions in specific microtextural settings, some of which produced a second generation of partial melt. Maximum temperatures were above ~750 °C and pressures were lower than those of the regional metamorphism. The aureole around the Makhavinekh Lake pluton is ~4 km wide and shows a progressive development of the contact metamorphic assemblages toward the pluton. In contrast, the contact metamorphic overprint is incipient around the Tessiarsuyungoakh intrusion, which developed a ~20 m wide contact aureole and is most prominent in screens of paragneiss within that intrusion.
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Andersen, Tom. "Age and petrogenesis of the Qassiarsuk carbonatite-alkaline silicate volcanic complex in the Gardar rift, South Greenland." Mineralogical Magazine 61, no. 407 (August 1997): 499–513. http://dx.doi.org/10.1180/minmag.1997.061.407.03.

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AbstractThe Qassiarsuk (formerly spelled Qagssiarssuk) complex is located in a roughly E–W trending graben structure between Qassiarsuk village and Tasiusaq settlement in the northern part of the Precambrian Gardar rift, South Greenland. The complex comprises a sequence of alkaline silicate tuffs and extrusive carbonatites interlayered with sandstones, and their subvolcanic equivalents, which represent possible feeders for the extrusive rocks. The Rb-Sr, Sm-Nd and Pb isotopic characteristics of 65 samples of extrusive carbonatite- and silicate tuffs and carbonatite diatremes have been determined by mass spectrometry. The Qassiarsuk complex can be dated to c. 1.2 Ga by Rb-Sr and Pb-Pb isochrons on whole-rocks and mineral separates, agreeing with previous isotopic ages for the volcanic rocks of the Eriksfjord formation in the Eriksfjord area of the Gardar rift, but not with previous, indirect age estimates of >1.31 Ga for assumed Eriksfjord equivalents in the Motzfeldt area further east. Recalculated isotopic compositions at 1.2 Ga indicate that the Qassiarsuk carbonatite- and alkaline-silicate magmas were comagmatic and derived from a depleted mantle source (εNd>4, εSr<−13, time-integrated, single- stage 238U/204Pb ≤ 7.4). The mantle-derived magmas were contaminated with crustal material, equivalent to the local, pre-Gardar granites and gneisses and sediments derived from these. The crustal component has a depleted mantle Nd model age of 2.1-2.6 Ga; at 1.2 Ga it was characterized by εSr = +76, εNd = −8.4, time-integrated, single- stage 238U/204Pb = 8.2−8.3. Strong decoupling of the Pb from the Sr and Nd isotopic systems suggests that the contamination happened only after carbonatitic and alkaline-silicate magmas had evolved from a common parent, by processes such as liquid immisicibility and/or fractional crystallization. Post-magmatic hydrothermal alteration (oxidation, hydration of mafic silicates, carbonatization of melilite) may have contributed further to the contamination of the carbonatite and alkaline silicate rocks of the Qassiarsuk complex.
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Digonnet, Stéphane, Normand Goulet, James Bourne, Ross Stevenson, and Doug Archibald. "Petrology of the Abloviak Aillikite dykes, New Québec: evidence for a Cambrian diamondiferous alkaline province in northeastern North America." Canadian Journal of Earth Sciences 37, no. 4 (April 3, 2000): 517–33. http://dx.doi.org/10.1139/e00-008.

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A dozen ultramafic lamprophyre dykes have been identified in the eastern part of Ungava Bay, Québec. The dark grey dykes are composed of macrocrysts of olivine and phlogopite featuring tetraferriphlogopite rims. These minerals are included in a matrix consisting of fine-grained phlogopite, olivine, spinel, and interstitial carbonate. The geochemical composition, mineral assemblage, chemical analyses of the xenocrysts and phenocrysts and Sm-Nd isotopic signature indicate that these rocks are carbonated ultramafic lamprophyre dykes. The chemical zonation of the micas and the presence of andradite suggest a complex sequence of crystallization. An Ar isotope correlation analysis indicates an age of approximately 550 Ma. The dykes have intruded the Tasiuyak gneiss, a suite of Paleoproterozoic metasedimentary rocks. This unit occupies the Torngat Orogen collision zone between the Rae Province and the Nain Province. The dykes are considered to have been emplaced within tension gashes during reactivation of major Paleoproterozoic structures and fractures associated with the opening of the Iapetus Ocean. They are possibly related to a mantle plume that simultaneously caused both the rupture of the Laurentia and the formation of the ultramafic magma. The Abloviak lamprophyres have quite similar analogues in southwest Greenland. The age, geochemical characteristics, isotopic signature common to all these dykes, the geological environment of the southwest Greenland are all comparable with the data presented here for the Abloviak lamprophyres. Furthermore their pre-drift geographical proximity, prior to the opening of the Labrador Sea, suggests that they are related to a common magmatic event which constitutes a diamondiferous alkaline province located in northeastern North America.
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Scott, David J., Richard A. Stern, Marc R. St-Onge, and Sarah M. McMullen. "U–Pb geochronology of detrital zircons in metasedimentary rocks from southern Baffin Island: implications for the Paleoproterozoic tectonic evolution of Northeastern Laurentia." Canadian Journal of Earth Sciences 39, no. 5 (May 1, 2002): 611–23. http://dx.doi.org/10.1139/e01-093.

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A geochronological investigation of metasedimentary rocks from southern Baffin Island using the Geological Survey of Canada SHRIMP II (sensitive high-resolution ion microprobe) has characterized the ages of detrital zircon populations to determine their provenance, bracket timing of deposition, and distinguish potentially distinct sequences of rocks. Four lithologically and structurally distinct metasedimentary packages have been identified; each appears to have been derived from a different source region. In the structurally lowest package, all analysed zircons are Archean, and > 90% have ages between 2.83 and 2.63 Ga; these rocks are interpreted as the northernmost exposures of the Paleoproterozoic Povungnituk Group of the Cape Smith Belt, northern Quebec, with detritus derived from the Superior craton. Occupying the intermediate structural levels, the most abundant supracrustal rocks on southern Baffin Island are siliciclastic and carbonate units of the Lake Harbour Group, and the Tasiuyak paragneiss. Five samples show a dominantly Paleoproterozoic signature (2.2–1.9 Ga), with only rare Archean zircons; the provenance of this detritus is uncertain. In the distinct package of feldspathic quartzite and pelite that stratigraphically overlies the Lake Harbour Group, all of the analysed detrital grains are Archean, ~80% are > 2.83 Ga, with a small proportion of the grains in excess of 3.0 Ga; all of this material is thought to be derived from the Archean craton exposed on the Hall Peninsula east of the study area. Finally, at the highest structural level, a sample associated with the Hall Peninsula orthogneisses contains zircons with prominent modes at 2.92, 2.82, and 2.77 Ga, consistent with derivation from the surrounding orthogneisses.
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Dissertations / Theses on the topic "Tasiujaq"

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Lanouette, Florence. "Stabilisation thermique des remblais construits sur le pergélisol sensible au dégel à l'aide d'une approche de conception tenant compte de l'accumulation de la neige." Master's thesis, Université Laval, 2021. http://hdl.handle.net/20.500.11794/69363.

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Dans les régions nordiques, l'accumulation préférentielle d'un couvert neigeux isolant en bordure des infrastructures de transport linéaires limite l'extraction de la chaleur en hiver. En terrain pergélisolé, cette modification de l'équilibre thermique peut être une cause importante de la dégradation du pergélisol sous-jacent affectant grandement les propriétés structurales de la chaussée. Puisque les transferts de chaleur dans le manteau neigeux sont essentiellement gouvernés par le mécanisme de conduction, son effet isolant peut être contré en diminuant l'épaisseur de neige présente sur les pentes et aux pieds du remblai. Pour ce faire, l'adoucissement de la pente des talus favorise un écoulement laminaire du vent qui souffle plus facilement la neige loin du remblai et minimise son accumulation. Les présents travaux de recherche ont pour objectif de mettre au point une méthode de conception visant la stabilisation thermique des infrastructures de transport linéaires construites sur le pergélisol en optimisant la géométrie du remblai de façon à prendre en compte l'accumulation de neige préférentielle. L'approche générale de l'étude repose sur l'utilisation d'un modèle bidimensionnel, réalisé à l'aide du logiciel de modélisation géothermique TEMP/W, qui simule l'effet du couvert neigeux sur le sol sous-jacent. L'instrumentation d'un transect de la piste d'atterrissage de Tasiujaq, au Nunavik, a permis d'y documenter le régime thermique du sol et l'évolution du couvert neigeux. À partir de ces données, le facteur n de gel a pu être exprimé en fonction de la hauteur de neige suivant une équation logarithmique. Cette relation empirique sert de condition limite à la surface du modèle géothermique. Le modèle, calibré et validé à l'aide de températures collectées au site d'essai de Tasiujaq, permet de quantifier l'impact de la géométrie du remblai sur le gradient de température dans le sol d'infrastructure. Ce dernier est calculé à partir de la température à l'interface entre le remblai et le sol et celle à la profondeur de variation d'amplitude annuelle nulle. Un gradient de température nul ou négatif est visé afin de préserver le pergélisol. Un tel régime thermique est obtenu en corrigeant la température à l'interface. Ainsi, afin d'obtenir les températures à l'interface correspondantes, des simulations numériques sont effectuées pour six pentes de talus variant de 45 à 14% (11H : 5V à 7H : 1V), et ce, pour trois hauteurs de remblai. Ultimement, ces résultats sont présentés sous la forme d'un outil de calcul de la pente requise pour assurer la stabilité thermique d'un remblai en fonction de la hauteur du remblai pour des sites où le vent et l'orientation favorise l'accumulation de neige.
In northern regions, preferential accumulation of an insulating snowpack along linear transportation infrastructures prevents the extraction of heat in winter. In permafrost terrain, this thermal equilibrium modification can be a significant cause of the underlying permafrost degradation, which affects the structural properties of the roadway. Since heat transfers through the snowpack are essentially controlled by the mechanism of conduction, its insulating effect can be counteracted by decreasing the thickness of snow on the slopes and at the toe of the embankment. To achieve this goal, the gentle slope promotes a laminar wind flow that blows snow away easily and, therefore, minimizes its accumulation. The main objective of this research project is to develop a design method aiming for thermal stabilization of linear transportation infrastructures built on permafrost by optimizing the embankment geometry to consider the preferential accumulation of snow. The general approach of the study relies on the use of a 2D model (produced with the modeling software TEMP/W) simulating the snowpack effect on the underlying ground. The monitoring of a transect at Tasiujaq airstrip, in Nunavik, documents the thermal regime in the ground and the evolution of the snowpack. Based on those data, the freezing n-factor was expressed as a function of the snow thickness following a logarithmic equation. This empirical relation is used as an upper boundary of the geothermal model. Once calibrated and validated with the data collected at theTasiujaq test site, the model allows to quantify the impact of the embankment geometry on the temperature gradient in the natural subgrade ground. This gradient is calculated from the temperature at the interface between the embankment and the ground and the temperature at the depth of zero annual amplitude. A temperature gradient of zero or less is aimed to preserve the permafrost. This ground thermal regime is obtained by correcting the temperature at the interface. Therefore, numeric simulations are run for six slopes between 45 and 14% and for three embankment thickness. Finally, these results are presented through an engineering tool calculating the slope needed to assure the thermal stability of the infrastructure depending of the embankment height.
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Ficheur, Alban. "Expérimentation de techniques de mitigation des effets de la fonte du Pergelisol sur les infrastructures de transport du Nunavik : Aéroport de Tasiujaq." Thesis, Université Laval, 2011. http://www.theses.ulaval.ca/2011/28205/28205.pdf.

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Vinet, Frédéric. "Géomorphologie, stratigraphie et évolution du niveau marin holocène d'une vallée soumise à des conditions macrotidales en régression forcée, région de Tasiujaq, Nunavik." Thesis, Université Laval, 2008. http://www.theses.ulaval.ca/2008/25059/25059.pdf.

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Tettelaar, Tanya Anne. "Emplacement history of the Pearly Gates anorthosite pluton and spatially related Tessiarsuyungoakh intrusion, and metamorphic petrology of the adjacent Tasiuyak paragneiss, northern Labrador /." Internet access available to MUN users only, 2004. http://collections.mun.ca/u?/theses,61302.

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Grandmont, Katerine. "Utilisation de systèmes d'information géographique pour l'évaluation des risques liés à la dégradation du pergélisol. Étude de cas : Tasiujaq, Nunavik, Québec." Thèse, 2013. http://hdl.handle.net/1866/10585.

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Les régions nordiques à pergélisol seront largement affectées par l'augmentation prévue des températures. Un nombre croissant d’infrastructures qui étaient autrefois construites avec confiance sur des sols gelés en permanence commencent déjà à montrer des signes de détérioration. Les processus engendrés par la dégradation du pergélisol peuvent causer des dommages importants aux infrastructures et entrainer des coûts élevés de réparation. En conséquence, le contexte climatique actuel commande que la planification des projets dans les régions nordiques s’effectue en tenant compte des impacts potentiels de la dégradation du pergélisol. Ce mémoire porte sur l’utilisation de systèmes d’information géographique (SIG) appliqués à l’évaluation du potentiel d’aménagement des territoires situés en milieu de pergélisol. En utilisant une approche SIG, l’objectif est d’élaborer une méthodologie permettant de produire des cartes d'évaluation des risques afin d’aider les collectivités nordiques à mieux planifier leur environnement bâti. Une analyse multi-échelle du paysage est nécessaire et doit inclure l'étude des dépôts de surface, la topographie, ainsi que les conditions du pergélisol, la végétation et les conditions de drainage. La complexité de l'ensemble des interactions qui façonnent le paysage est telle qu'il est pratiquement impossible de rendre compte de chacun d'eux ou de prévoir avec certitude la réponse du système suite à des perturbations. Ce mémoire présente aussi certaines limites liées à l’utilisation des SIG dans ce contexte spécifique et explore une méthode innovatrice permettant de quantifier l'incertitude dans les cartes d'évaluation des risques.
Northern regions underlain by permafrost will largely be affected by the projected increase in air temperature. A growing number of structures that were once built with great confidence on perennially frozen soils are already starting to show signs of deterioration. Processes caused by permafrost degradation can cause significant damages to infrastructure and require high costs of repair. The current climatic context therefore commands that the implementation of projects in permafrost regions follows a well-thought planning in order to account for the potential impacts of permafrost degradation. This thesis focuses on the use of geographic information systems (GIS) applied to the identification of the development potential of communities located in permafrost regions. Using a GIS approach, the goal is to develop a methodology to produce risk-assessment maps to help northern communities better plan their built environment. A multi-scale analysis of the landscape is necessary and should include the investigation of surficial deposits, topography, as well as permafrost, vegetation and drainage conditions. The complexity of all the interactions that shape the landscape is such that it is virtually impossible to account for all of them or to predict with certainty the response of the system following disturbances. This research also presents some of the limitations to the use of GIS in this specific context and explores an innovative method for quantifying uncertainty in risk-assessment maps.
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Vinet, Frédéric. "Géomorphologie, stratigraphie et évolution du niveau marin holocène d'une vallée soumise à des conditions macrotidales en régression forcée, région de Tasiujaq, Nunavik /." 2008. http://www.theses.ulaval.ca/2008/25059/25059.pdf.

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Books on the topic "Tasiujaq"

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Inuit Elders Conference (12th 1996 Tasiujaq, Nunavik). Nunavik Inuit Elders' Conference, Tasiujaq, Nunavik, August 26-30, 1996. [Inukjuak, Quebec]: Avataq Cultural Institute, 1996.

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Conference papers on the topic "Tasiujaq"

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Doré, G., A. Ficheur, A. Guimond, and M. Boucher. "Performance and Cost-Effectiveness of Thermal Stabilization Techniques Used at the Tasiujaq Airstrip." In Cold Regions Engineering 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412473.004.

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Hernández, M. F. Barón, C. Lemieux, and G. Doré. "Long-Term Monitoring of Mitigation Techniques of Permafrost Thaw Effects at Tasiujaq Airport in Nunavik, Canada." In 18th International Conference on Cold Regions Engineering and 8th Canadian Permafrost Conference. Reston, VA: American Society of Civil Engineers, 2019. http://dx.doi.org/10.1061/9780784482599.058.

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Jo/rgensen, Anders Stuhr, and Guy Doré. "Experimentation of Several Mitigation Methods in Tasiujaq Airport to Minimize the Effects Caused by the Melting of Permafrost." In 14th Conference on Cold Regions Engineering. Reston, VA: American Society of Civil Engineers, 2009. http://dx.doi.org/10.1061/41072(359)20.

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Reports on the topic "Tasiujaq"

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van Rooyen, D. Multiple phases of deformation and metamorphism in the Kuujjuaq-Tasiujaq area of the New Quebec Orogen, Quebec; evidence from preliminary U-Pb geochronology and structural studies. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/302771.

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