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Articoli di riviste sul tema "Geology - Research - Eastern Canada"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 27 luglio 2025

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1

Goda, Katsuichiro, and Solomon Tesfamariam. "Financial risk evaluation of non-ductile reinforced concrete buildings in eastern and western Canada." International Journal of Disaster Risk Reduction 33 (February 2019): 94–107. http://dx.doi.org/10.1016/j.ijdrr.2018.09.013.

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2

Hugenholtz, Chris H., and Denis Lacelle. "Geomorphic Controls on Landslide Activity in Champlain Sea Clays along Green’s Creek, Eastern Ontario, Canada." Géographie physique et Quaternaire 58, no. 1 (2006): 9–23. http://dx.doi.org/10.7202/013108ar.

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AbstractLandslides in Champlain Sea clays have played an important role in shaping Eastern Ontario’s landscape. Despite extensive research, there is a limited understanding of the relations between landslide activity, climatic controls, and the geomorphic evolution of river valleys in Champlain Sea clay deposits. With these issues in mind, a study was undertaken to determine the controls on the spatio-temporal distribution of contemporary landslide activity in valley slopes composed of Champlain Sea clay. The study area was the Green’s Creek valley located in the east end of Ottawa, Ontario. O

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3

Brown, A., N. M. Soonawala, R. A. Everitt, and D. C. Kamineni. "Geology and geophysics of the Underground Research Laboratory site, Lac du Bonnet Batholith, Manitoba." Canadian Journal of Earth Sciences 26, no. 2 (1989): 404–25. http://dx.doi.org/10.1139/e89-037.

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The lease area of the Atomic Energy of Canada Limited Underground Research Laboratory covers 3.8 km2 and is located 2.5 km north of the south contact of the Lac du Bonnet Batholith. A shaft to 255 m and 130 boreholes up to 1100 m deep expose the third dimension.The underlying granite is largely of two types: (i) pink porphyritic, which may be biotite rich, gneissic, and (or) xenolithic; and (ii) grey homogeneous and equigranular. Composition layering, including xenolith-rich zones, outlines domes along an antiform trending north-northeast through the western part of the lease area. The southea

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4

Tremblay, Hélène, Serge Leroueil, and Jacques Locat. "Mechanical improvement and vertical yield stress prediction of clayey soils from eastern Canada treated with lime or cement." Canadian Geotechnical Journal 38, no. 3 (2001): 567–79. http://dx.doi.org/10.1139/t00-119.

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The method of soil stabilization is well known and has been used throughout the world for many decades to improve some soil properties. Although many researchers have studied the effect of adding a cementing agent to a soil, not many of these researchers have explored the effect of treatment on the resulting properties of high water content soils like dredged material. Also, there has been little work concerning the prediction of the mechanical changes to the soil. Therefore, this paper summarizes the results of a research project conducted to define the general mechanical behavior of high wat

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5

m ABU EL-LEIL ALI, Ibrahim, Abdellah Sadek TOLBA, Hamdy Ahmed Mohamed AWAD, Aleksey Valer’evich NASTAVKIN, Sayed Ahmed OMAR, and Mohamed Galal EL-FEKY. "Geological and geochemical studies on El-Missikat granites, Central Eastern Desert, Egypt." NEWS of the Ural State Mining University, no. 4 (December 20, 2020): 7–18. http://dx.doi.org/10.21440/2307-2091-2020-4-7-18.

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Objective. The present work deals with the detailed investigations of the geology, geochemistry, and tectonic setting of the studied granitic rocks. Research methods. This work involves both field work (Collection samples and drawing of a new geological map) and laboratory work (preparation of thin sections for petrographic studies by polarizing microscope), Atomic absorption, X-ray Fluorescence analysis (XRF) in the Central Laboratories of the Acme in Canada and Mass-Spectrometer with Inductively Coupled Plasma (ICPMS). Result. The study area restricted in the Central Eastern Desert of Egypt

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6

Honsberger, Ian W., Angela Ford, and Daniel McDonald. "National-Scale Geospatial Modelling of Pyrrhotite in Bedrock Across Canada: A Pilot Study." Geoscience Canada 51, no. 3 (2024): 147–59. http://dx.doi.org/10.12789/geocanj.2024.51.213.

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The most abundant iron sulphide minerals in igneous, metamorphic, and some sedimentary rocks are FeS2 (pyrite/marcasite) and Fe1-xS (pyrrhotite). The oxidation of pyrite and pyrrhotite in bedrock aggregates and mine tailings is undesirable to infrastructure and the environment because such chemical reactions are linked with concrete deterioration and acid mine drainage, respectively. The oxidation rate of pyrrhotite is up to one hundred times greater than that of pyrite; thus, pyrrhotite oxidation is of particular concern to society. Pyrrhotite-bearing concrete aggregates may lead to rapid exp

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7

Goulet, Christine A., Tadahiro Kishida, Timothy D. Ancheta, et al. "PEER NGA-East database." Earthquake Spectra 37, no. 1_suppl (2021): 1331–53. http://dx.doi.org/10.1177/87552930211015695.

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This article documents the earthquake ground motion database developed for the NGA-East Project, initiated as part of the Next Generation Attenuation (NGA) research program and led by the Pacific Earthquake Engineering Research Center (PEER). The project was focused on developing a ground motion characterization model (GMC) model for horizontal ground motions for the large region referred to as Central and Eastern North America (CENA). The CENA region covers most of the U.S. and Canada, from the Rocky Mountains to the Atlantic Ocean and is characterized tectonically as a stable continental reg

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8

Grant, A. C., K. D. McAlpine, and J. A. Wade. "Offshore Geology and Petroleum Potential of Eastern Canada." Energy Exploration & Exploitation 4, no. 1 (1986): 5–52. http://dx.doi.org/10.1177/014459878600400103.

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9

Jutras, Pierre, Gilbert Prichonnet, and Steven McCutcheon. "Alleghanian deformation in the eastern Gaspé Peninsula of Quebec, Canada." Geological Society of America Bulletin 115, no. 12 (2003): 1538. http://dx.doi.org/10.1130/b25306.1.

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10

Shaw, J., and D. P. Potter. "A glacial landform assemblage in Placentia Bay, Newfoundland, eastern Canada." Geological Society, London, Memoirs 46, no. 1 (2016): 139–42. http://dx.doi.org/10.1144/m46.141.

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11

AMOS, CARL L., and ANN A. L. MILLER. "The Quaternary stratigraphy of southwest Sable Island Bank, eastern Canada." Geological Society of America Bulletin 102, no. 7 (1990): 915–34. http://dx.doi.org/10.1130/0016-7606(1990)102<0915:tqsoss>2.3.co;2.

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12

Gower, Charles F., Larry M. Heaman, W. Dale Loveridge, Urs Schärer, and Robert D. Tucker. "Grenvillian magmatism in the eastern Grenville Province, Canada." Precambrian Research 51, no. 1-4 (1991): 315–36. http://dx.doi.org/10.1016/0301-9268(91)90106-k.

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13

Ver Straeten, Charles. "An introduction to the Devonian Period, and the Devonian in New York State and North America." Bulletins of American Paleontology, no. 403-404 (July 2023): 11–102. http://dx.doi.org/10.32857/bap.2023.403.03.

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The Devonian strata in New York State were the standard section for North America for over 100 years, and remain a significant reference for regional to global correlation and research. Since publication of L. V. Rickard’s (1975) New York Devonian correlation chart, various higher-resolution stratigraphic analyses have been employed, sometimes at bed-by-bed scale. These include sequence-, bio-, event-, chemo-, and other -stratigraphic approaches, along with increasingly finer-resolution geochronologic dating of airfall volcanic tephras. Results have led to many new interpretations and insights

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14

Grant, Jonathan, Craig W. Emerson, Barry T. Hargrave, and Jeannette L. Shortle. "Benthic oxygen consumption on continental shelves off eastern Canada." Continental Shelf Research 11, no. 8-10 (1991): 1083–97. http://dx.doi.org/10.1016/0278-4343(91)90092-k.

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15

Lajeunesse, P. "Late Wisconsinan grounding-zone wedges, northwestern Gulf of St Lawrence, eastern Canada." Geological Society, London, Memoirs 46, no. 1 (2016): 227–28. http://dx.doi.org/10.1144/m46.91.

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16

Piper, D. J. W., D. C. Campbell, and D. C. Mosher. "Mid-latitude complex trough-mouth fans, Laurentian and Northeast fans, eastern Canada." Geological Society, London, Memoirs 46, no. 1 (2016): 363–64. http://dx.doi.org/10.1144/m46.93.

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17

RUZ, MARIE-HELENE, and MICHEL ALLARD. "Sedimentary structures of cold-climate coastal dunes, Eastern Hudson Bay, Canada." Sedimentology 42, no. 5 (1995): 725–34. http://dx.doi.org/10.1111/j.1365-3091.1995.tb00405.x.

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18

Donovan, Stephen K., and David G. Keighley. "A ‘British’ Silurian crinoid from Quinn Point, New Brunswick, eastern Canada." Proceedings of the Geologists' Association 126, no. 2 (2015): 226–31. http://dx.doi.org/10.1016/j.pgeola.2015.01.006.

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19

Hamouche, K. K., S. Leroueil, M. Roy, and A. J. Lutenegger. "In situ evaluation of K0 in eastern Canada clays." Canadian Geotechnical Journal 32, no. 4 (1995): 677–88. http://dx.doi.org/10.1139/t95-067.

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An approximate value of the horizontal effective stress in an overconsolidated clay deposit is often determined from an estimate of the effective stress ratio, K0, using the equation [Formula: see text]. It is also generally considered that the α parameter is approximately equal to sin [Formula: see text]. For evaluating K0 in sensitive clays of eastern Canada, a testing program has been initiated on three different sites representing a large range of overconsolidation ratios. Three different in situ devices were used: the Cambridge self-boring pressuremeter, the flat dilatometer, and hydrauli

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20

Normandeau, Alexandre, D. Calvin Campbell, David J. W. Piper, and Kimberley A. Jenner. "Are submarine landslides an underestimated hazard on the western North Atlantic passive margin?" Geology 47, no. 9 (2019): 848–52. http://dx.doi.org/10.1130/g46201.1.

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AbstractThe western North Atlantic passive margin is considered relatively stable, with few slope instabilities recognized during the Holocene. However, new multibeam bathymetry mapping and sediment core acquisition off eastern Canada indicate that previously unidentified, large, submarine landslide events occurred during the Late Holocene, between 4 and 1.5 ka. The recognition of these new gravitational events, in addition to the well-known C.E. 1929 Grand Banks earthquake-induced landslide, indicates that approximately one large landslide event per 1000 years has occurred offshore eastern Ca

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21

Knaust, Dirk, and André Desrochers. "Exceptionally preserved soft-bodied assemblage in Ordovician carbonates of Anticosti Island, eastern Canada." Gondwana Research 71 (July 2019): 117–28. http://dx.doi.org/10.1016/j.gr.2019.01.016.

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22

Beltrami, Hugo, and Jean-Claude Mareschal. "Ground temperature changes in eastern Canada: borehole temperature evidence compared with proxy data." Terra Nova 5, no. 1 (1993): 21–28. http://dx.doi.org/10.1111/j.1365-3121.1993.tb00222.x.

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23

Harland, T. L., and R. K. Pickerill. "A review of Middle Ordovician sedimentation in the St. Lawrence Lowland, eastern Canada." Geological Journal 17, no. 2 (2007): 135–56. http://dx.doi.org/10.1002/gj.3350170205.

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24

Danard, M. B., M. I. El‐Sabh, and T. S. Murty. "Recent trends in precipitation in Eastern Canada: Research note." Atmosphere-Ocean 28, no. 1 (1990): 140–45. http://dx.doi.org/10.1080/07055900.1990.9649370.

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25

SHARMA, SAJAL, GEORGE R. DIX, and MIKE VILLENEUVE. "Petrology and potential tectonic significance of a K-bentonite in a Taconian shale basin (eastern Ontario, Canada), northern Appalachians." Geological Magazine 142, no. 2 (2005): 145–58. http://dx.doi.org/10.1017/s001675680400041x.

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A 6 cm thick K-bentonite, herein defined as the Russell Bed, occurs in an Upper Ordovician deep-basin shale succession in eastern Ontario, Canada, forming part of the distal Taconic foreland in eastern North America. The bed lies within the pygmaeus graptolite Biozone, which is about 451 to 452 Ma in age. Although some bentonites are reported from this interval in eastern North America, we are reporting the first set of compositional data for a bentonite of this age. Gamma-log correlation identifies a potential minimum distribution area of <2×105 km2 for the K-bentonite, covering part of so

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26

Trenhaile, Alan S., Neil J. Porter, and Jacob I. Kanyaya. "Shore Platform Processes in Eastern Canada." Géographie physique et Quaternaire 60, no. 1 (2007): 19–30. http://dx.doi.org/10.7202/016362ar.

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Abstract This research is conducted on a mesotidal, argillite shore platform at Mont Louis in Gaspé, Québec, and on macrotidal platforms in the basalts of Scots Bay and the sandstones of Burncoat Head in Nova Scotia. Rock samples have been subjected to wetting and drying and to salt weathering cycles. The platforms were surveyed; rock hardness was determined with a Rock Test Hammer; waves were recorded in the field; and downwearing rates were measured at 56 micro-erosion meter stations over 1 to 3 years. Weathering is the dominant process at Mont Louis, although the horizontal platform may hav

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27

Normandeau, Alexandre, and D. Calvin Campbell. "Recurrence of turbidity currents on glaciated continental margins: A conceptual model from eastern Canada." Journal of Sedimentary Research 90, no. 10 (2020): 1305–21. http://dx.doi.org/10.2110/jsr.2020.66.

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ABSTRACT Turbidity currents in submarine canyons transport large volumes of sediment and carbon to the deep sea and are known to present a major risk to submarine infrastructure. Understanding the origin, the triggers, the recurrence, and the timing of these events is important for predicting future events and mitigating their impact. Depending on the morphological and latitudinal setting of submarine canyons, different external controls will govern the recurrence of turbidity currents. Here, we assess the recurrence of turbidity currents in shelf-incising submarine canyons off eastern Canada

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28

Gouiza, M., J. Hall, and G. Bertotti. "Rifting and pre-rift lithosphere variability in the Orphan Basin, Newfoundland margin, Eastern Canada." Basin Research 27, no. 4 (2014): 367–86. http://dx.doi.org/10.1111/bre.12078.

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29

Kalkreuth, Wolfgang, Claus Andreasen, Henrik I. Petersen, and Lars Stemmerik. "The petrology and provenance of coal artifacts from Thule settlements in north-eastern Greenland." Bulletin Volume 60 – 2012 60 (February 24, 2012): 1–13. http://dx.doi.org/10.37570/bgsd-2012-60-01.

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Coal petrographic techniques have been used to trace the origin of coal used to produce artifacts by the Thule people in north-eastern Greenland. The coal artifacts were collected from the north-east coast settlements between 76°55'–80°18'N and date back to the 15th century A.D. The petrographic data suggest that they have a common source, the Middle Jurassic coals outcropping south of 75°15' in north-eastern Greenland. It is thus evident that the Thule people used local material rather than bringing the coal from the known “mines” in Arctic Canada. It also implies that contemporaneous Thule p

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Nastev, Miroslav, Michel Parent, Nicolas Benoit, Martin Ross, and Danielle Howlett. "Regional VS30model for the St. Lawrence Lowlands, Eastern Canada." Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards 10, no. 3 (2016): 200–212. http://dx.doi.org/10.1080/17499518.2016.1149869.

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Fulton, R. J., P. F. Karrow, P. LaSalle, and D. R. Grant. "Summary of Quaternary Stratigraphy and history, Eastern Canada." Quaternary Science Reviews 5 (January 1986): 211–28. http://dx.doi.org/10.1016/0277-3791(86)90188-5.

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32

Xu, X., A. H. Manson, C. E. Meek, et al. "Vertical and interhemispheric links in the stratosphere-mesosphere as revealed by the day-to-day variability of Aura-MLS temperature data." Annales Geophysicae 27, no. 9 (2009): 3387–409. http://dx.doi.org/10.5194/angeo-27-3387-2009.

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Abstract. The coupling processes in the middle atmosphere have been a subject of intense research activity because of their effects on atmospheric circulation, structure, variability, and the distribution of chemical constituents. In this study, the day-to-day variability of Aura-MLS (Microwave Limb Sounder) temperature data are used to reveal the vertical and interhemispheric coupling processes in the stratosphere-mesosphere during four Northern Hemisphere winters (2004/2005–2007/2008). The UKMO (United Kingdom Meteorological Office) assimilated data and mesospheric winds from MF (medium freq

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33

Addison, J. A., A. L. Einfeldt, N. N. Kang, and S. J. Walde. "Small-scale genetic structure in a stream-dwelling caddisfly in eastern Canada." Marine and Freshwater Research 66, no. 5 (2015): 459. http://dx.doi.org/10.1071/mf13268.

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We used mitochondrial DNA (cytochrome c oxidase subunit I) to examine the population genetic structure and phylogeography for 12 populations of a widely distributed predatory caddisfly (Rhyacophila minor) in small, unconnected streams along a 45-km stretch of North Mountain, Nova Scotia, Canada. We detected patterns of strong genetic subdivision (FST=0.312) with streams separated by >3.5km being significantly different whereas adjacent streams were not (no significant FST values), suggesting some, but very limited, current overland dispersal by adults. A significant phylogeographic break wa

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34

Ho, K. M., T. M. Choo, and R. A. Martin. "AC Maple barley." Canadian Journal of Plant Science 82, no. 1 (2002): 93–94. http://dx.doi.org/10.4141/p00-154.

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AC Maple is a six-rowed spring feed barley (Hordeum vulgare L.) cultivar bred at the Eastern Cereal and Oilseed Research Centre, Agriculture and Agri-Food Canada, and evaluated by the Eastern Canada Barley Breeding Group. It was selected from a Chapais/CIMMYT-6 cross and has high yield. AC Maple is suitable for growing in the Maritime Region of Canada. Key words: Hordeum vulgare L., six-rowed barley, feed barley, high yield

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Leslie-Panek, Jennifer, and Margot McMechan. "A seismic structural overview of Liard Basin, Northeast British Columbia, Canada." Interpretation 9, no. 2 (2021): T523—T532. http://dx.doi.org/10.1190/int-2020-0078.1.

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The Liard Basin is an important subbasin of the Western Canada Sedimentary Basin located in Northeast British Columbia along the eastern margin of the Canadian Cordillera. It contains significant potential unconventional gas resources but is largely underrepresented in public literature. Using available-for-purchase 2D seismic data, a regional structural interpretation of the basin was completed providing the first seismically controlled, high-level overview of the structural features of the basin and its surrounding area. The shape of the Liard Basin largely reflects the orientation of older

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36

Álvarez-Vázquez, Carmen. "Alethopteris and Neuralethopteris from the lower Westphalian (Middle Pennsylvanian) of Nova Scotia and New Brunswick, Maritime Provinces, Canada." Atlantic Geology 56 (June 2, 2020): 111–45. http://dx.doi.org/10.4138/atlgeol.2020.005.

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A systematic revision of Alethopteris and Neuralethopteris from upper Namurian and lower Westphalian (Middle Pennsylvanian) strata of Nova Scotia and New Brunswick, eastern Canada, has demonstrated the presence of eight species: Alethopteris bertrandii, Alethopteris decurrens, Alethopteris cf. havlenae, Alethopteris urophylla, Alethopteris cf. valida, Neuralethopteris pocahontas, Neuralethopteris schlehanii and Neuralethopteris smithsii. Restudy of the Canadian material has led to new illustrations, observations and refined descriptions of these species. Detailed synonymies focus on records fr

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Donovan, Stephen K., and Randall F. Miller. "Silurian crinoids of the New Brunswick Museum, Saint John, Canada." Atlantic Geology 52 (November 26, 2016): 223. http://dx.doi.org/10.4138/atlgeol.2016.011.

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The New Brunswick Museum’s collection of Silurian crinoids from eastern Canada is small, and includes specimens from New Brunswick, Quebec and Nova Scotia. Material considered herein is, with one exception, from New Brunswick. Included are: the cladid Syndetocrinus dartae (Upper Silurian of Quebec); the camerates Scyphocrinites sp. (Pridoli or Lochkovian) and camerate crinoid arms gen. et sp. indet. (Lower Silurian); columnal morphotaxa Floricrinus (col.) sp. (Ludlow or Pridoli) and Lanxocolumnus (col.) sp. cf. L. chaleurensis Donovan and Keighley (probably Llandovery, Telychian); distal dendr

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Ruz, Marie-Hélène, and Michel Allard. "Foredune development along a subarctic emerging coastline, eastern Hudson Bay, Canada." Marine Geology 117, no. 1-4 (1994): 57–74. http://dx.doi.org/10.1016/0025-3227(94)90006-x.

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Wang, Baolin. "Failure mechanism of an ancient sensitive clay landslide in eastern Canada." Landslides 16, no. 8 (2019): 1483–95. http://dx.doi.org/10.1007/s10346-019-01198-4.

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Gower, Charles F. "The evolution of the Grenville Province in eastern Labrador, Canada." Geological Society, London, Special Publications 112, no. 1 (1996): 197–218. http://dx.doi.org/10.1144/gsl.sp.1996.112.01.11.

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Larue, Fanny, Alain Royer, Danielle De Sève, Alexandre Langlois, Alexandre Roy, and Ludovic Brucker. "Validation of GlobSnow-2 snow water equivalent over Eastern Canada." Remote Sensing of Environment 194 (June 2017): 264–77. http://dx.doi.org/10.1016/j.rse.2017.03.027.

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McCann, S. B., J. E. Dale, and P. B. Hale. "Subarctic tidal flats in areas of large tidal range, southern Baffin Island, eastern Canada." Géographie physique et Quaternaire 35, no. 2 (2011): 183–204. http://dx.doi.org/10.7202/1000436ar.

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Wide, boulder-strewn intertidal flats occur around the head of Frobisher Bay and along parts of the shoreline of Cumberland Sound, in southeast Baffin Island. The coastal environment is characterized by large tidal ranges, severe winter sea ice conditions, and a relative sea level history which involves rapid and then decreasing land emergence during the earlier part of the Holocene, succeeded by slight recent submergence. Summer field investigations were carried out at two sites, Koojesse Inlet on Frobisher Bay, where ice breakup conditions were also monitored, and Pangnirtung Fiord off Cumbe

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SHANMUGAM, G., and R. J. MOIOLA. "Sedimentary facies of the Nova Scotian upper and middle continental slope, offshore eastern Canada." Sedimentology 32, no. 3 (1985): 455. http://dx.doi.org/10.1111/j.1365-3091.1985.tb00524.x.

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Donovan, Stephen K., and David G. Keighley. "A ‘British’ silurian crinoid from Quinn Point, New Brunswick, Eastern Canada: Designation of types." Proceedings of the Geologists' Association 130, no. 6 (2019): 770–71. http://dx.doi.org/10.1016/j.pgeola.2019.09.003.

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Ho, K. M., T. M. Choo, R. A. Martin, C. D. Caldwell, D. Walker, and V. Rodd. "AC Vision barley." Canadian Journal of Plant Science 82, no. 3 (2002): 551–53. http://dx.doi.org/10.4141/p01-187.

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AC Vision is a six-rowed spring feed barley (Hordeum vulgare L.) cultivar bred at the Eastern Cereal and Oilseed Research Centre, Agriculture and Agri-Food Canada, and evaluated by the Eastern Canada Barley Breeding Group. It was selected from a Sabina/OAC Kippen cross. It has high yield, improved straw strength and resistance to powdery mildew. AC Vision is suitable for growing in areas II and IV of Ontario and in the Maritime Region of Canada. Key words: Hordeum vulgare L., feed barley, high yield, powdery mildew resistance

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Ho, K. M., W. L. Seaman, T. M. Choo, et al. "AC Legend barley." Canadian Journal of Plant Science 80, no. 1 (2000): 113–15. http://dx.doi.org/10.4141/p99-052.

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AC Legend is a six-rowed spring feed barley (Hordeum vulgare L.) cultivar bred at the Eastern Cereal and Oilseed Research Centre, Agriculture and Agri-Food Canada, and evaluated by the Easter Canada Barley Breeding Group. It was selected from a Chapais/CIMMYT-6 cross and is suitable for growing in eastern Canada, where it out-yielded the check cultivars AC Stephen, Chapais, Myriam, ACCA and AC Westech. AC Legend is resistant to scald. Key words: Hordeum vulgare L., six-rowed barley, feed barley, high yield, scald resistance

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47

Spalding, Jennifer, David A. Schneider, and Julie Brown. "Geochronology of calcite‐filled joints, southeast Canada: Insight into Late Cretaceous deformation of eastern North America." Terra Nova 32, no. 6 (2020): 425–33. http://dx.doi.org/10.1111/ter.12479.

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48

Dowdeswell, E. K., B. J. Todd, and J. A. Dowdeswell. "Canyons and slides on the continental slope seaward of a shallow bank, Labrador margin, eastern Canada." Geological Society, London, Memoirs 46, no. 1 (2016): 405–6. http://dx.doi.org/10.1144/m46.133.

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49

FitzGerald, D. J., H. Ugalde, B. Morris, and H. Holstein. "Three-dimensional geology from potential field geophysics: Applications to Bathurst Mining Camp, Eastern Canada." ASEG Extended Abstracts 2015, no. 1 (2015): 1–4. http://dx.doi.org/10.1071/aseg2015ab201.

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50

Swanton, C. J., K. N. Harker, and R. L. Anderson. "Crop Losses Due to Weeds in Canada." Weed Technology 7, no. 2 (1993): 537–42. http://dx.doi.org/10.1017/s0890037x00028049.

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Concerns about the effect of pesticides on our environment has stimulated questions about the direction of future research in weed science. Knowledge of crop losses due to weeds would be helpful in guiding research objectives by identifying areas of greatest need. A survey was conducted in 1991 to estimate losses due to weeds in 58 commodities in Canada. Data generated included: percent loss in production, quantity loss in production, and loss of production value (monetary value) for each commodity in each province. The estimated average annual losses caused by weeds in the 58 commodities were

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