Увійти

Готові списки джерел за темами / Sudburg

Добірка наукової літератури з теми "Sudburg"

Автор: Grafiati

Опубліковано: 12 червня 2021

Оновлено: 1 лютого 2022

Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями

Оберіть тип джерела:

Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Sudburg".

Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.

Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.

Зміст

Статті в журналах
Дисертації
Книги
Частини книг
Тези доповідей конференцій
Звіти організацій

Статті в журналах з теми "Sudburg":

1

Hall, N. "George Greenstein and Arthur G. Zajonc, The Quantum Challenge. Sudburg, MA: Jones and Bartlett Publishers, 1997, cloth US$50.00, paper US$25.00. ISBN 0763704679 (cloth)." British Journal for the Philosophy of Science 50, no. 2 (June 1, 1999): 313–15. http://dx.doi.org/10.1093/bjps/50.2.313.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Kellett, R. L., and B. Rivard. "Characterization of the Benny deformation zone, Sudbury, Ontario." Canadian Journal of Earth Sciences 33, no. 9 (September 1, 1996): 1256–67. http://dx.doi.org/10.1139/e96-095.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Remote sensing imagery and geophysical data are well known as valuable tools for reconnaissance mapping in unknown areas, but they can also be used to reinterpret existing regional geological maps. A combination of airborne magnetic data and synthetic aperture radar images, at both a regional and a detailed scale, have been used to identify a wrench-fault system on the Canadian Shield north of the Sudbury structure. The 3–4 km wide deformation zone comprises a set of subparallel vertical faults bounding blocks of Archean granites, Archean metavolcanics of the Benny greenstone belt, and Paleoproterozoic metasediments of the Huronian supergroup. Using high-resolution airborne radar and magnetic data, the fault zone is found to extend for 40 km along the southern margin of the Benny greenstone belt. The wrench-fault system may have been tectonically active during several episodes throughout the Proterozoic. An interpretation of these data, supported by additional field mapping, indicates that the 1240 Ma Sudbury dyke swarm has been intruded through the deformation zone after its most active period of movement. Overprinting of Sudbary impact breccia at the southern edge of the deformation zone suggests that some movement occurred on the faults postdating the 1850 Ma meteorite impact. Lineaments that correlate spatially with the wrench-fault system can be traced across the southern Superior Province and the Cobalt Embayment on the regional images. However, more high-resolution studies are required to establish the same overprinting relationships along the length of the lineaments.

3

Braverman, Doreen. "Greater Sudbury / Grand Sudbury, Ontario." Raven: A Journal of Vexillology 18 (2011): 59–61. http://dx.doi.org/10.5840/raven20111834.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

4

Wu, Jianjun, Bernd Milkereit, and David Boerner. "Timing constraints on deformation history of the Sudbury Impact Structure." Canadian Journal of Earth Sciences 31, no. 11 (November 1, 1994): 1654–60. http://dx.doi.org/10.1139/e94-147.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Herein, we present new high-resolution seismic images of the Sudbury Impact Structure, acquired across the Sudbury Igneous Complex and its environs, which provide evidence for the relative timing of the deformation events that reshaped the initial Sudbury Structure. The seismic images show that the lower unit of the Sudbury basinal fill sediments, the Onwatin argillite, is penetrated by a set of blind, imbricated thrusts, whereas the overlying Chelmsford turbidites are unaffected by faulting. We interpret this observation to mean that the deposition of the Chelmsford sediments postdates the latest major deformation of the Sudbury Structure, suggesting that the uniform paleocurrent trends observed in the Chelmsford turbidites are not related to the initial shape of the Sudbury Structure.

5

Chubb, P. T., D. C. Vogel, D. C. Peck, R. S. James, and R. R. Keays. "Occurrences of pseudotachylyte at the East Bull Lake and Shakespeare–Dunlop intrusions, Ontario, Canada." Canadian Journal of Earth Sciences 31, no. 12 (December 1, 1994): 1744–48. http://dx.doi.org/10.1139/e94-155.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Pseudotachylyte bodies were recently identified within and adjacent to the Early Proterozoic East Bull Lake and Shakespeare–Dunlop intrusions, located approximately 25–40 km west-southwest of the western margin of the Sudbury Igneous Complex. These breccia-like bodies locally form extensive vein networks and are preferentially developed along the contact between the intrusions and older Archean granitoid rocks. The pseudotachylyte veins comprise variable proportions of locally derived rock fragments and an aphanitic to fine-grained crystalline matrix that commonly displays flow textures. The veins appear to have formed by intense cataclasis and (or) frictional melting. These occurrences are very similar in appearance to Sudbury Breccia dykes that are observed at a radial distance of up to 80 km from the Sudbury Igneous Complex. Sudbury Breccia is widely believed to have formed as a result of the Sudbury event—a cataclysmic explosion that occurred at 1.85 Ga. The location of the pseudotachylyte veins described herein may coincide with one of the concentric bands of relatively intense Sudbury Breccia development observed to the north of the Sudbury Igneous Complex.

6

Boerner, D. E., B. Milkereit, and A. Davidson. "Geoscience impact: a synthesis of studies of the Sudbury Structure." Canadian Journal of Earth Sciences 37, no. 2-3 (April 2, 2000): 477–501. http://dx.doi.org/10.1139/e99-062.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Geophysical probing results are synthesized into a three-dimensional framework necessary for understanding the genesis of the Sudbury Structure, based primarily on seismic reflection results centred on the Sudbury Igneous Complex. Remnants of crustal melting from a catastrophic meteorite impact are superimposed on the juxtaposition of mid-crustal rocks exhumed during the Archean against deformed Paleoproterozoic sedimentary rocks. Sedimentation, metamorphism, deformation, and metasomatic overprints are all part of the post-impact history of Sudbury and tend to dominate the geophysical response of the structure. Pre-impact deformation, although certainly preserved in some aspects of Sudbury geology, is not clearly expressed in the geophysical data, nor are any elements of impact-induced deformation. Geophysical views of the Sudbury Igneous Complex are thus somewhat biased in representing mostly the post-impact, but pre-Grenvillian history of the region, with the exception of igneous events. Establishing the proper context for integrating these geophysical results in the genetic interpretation of the Sudbury Structure depends crucially upon timing constraints.

7

Hearst, R. B., and W. A. Morris. "Regional gravity setting of the Sudbury Structure." GEOPHYSICS 66, no. 6 (November 2001): 1680–90. http://dx.doi.org/10.1190/1.1487110.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

In the vicinity of Sudbury, Ontario, Canada, the boundary between the Southern and Superior tectonic provinces is overlain by the elliptical Sudbury Structure. On the basis of gravity modeling, genesis of the Sudbury Structure has been attributed to either a magmatic origin (having a dense hidden differentiate zone) or a meteorite impact origin (there being no dense hidden mass). The difference between the two gravity models centers on the problem of regional‐residual separation. As shown by numerous previous studies, any such separation of components is nonunique. This becomes especially problematic when, as in Sudbury, a portion of the near‐surface geology has a similar orientation and dimension to more deep‐seated source. In this paper, several numerical methods (upward continuation, downward continuation, wavelength filtering, trend‐surface analysis) for determining the regional component of the gravity field associated with the Sudbury Structure have been applied and evaluated. Of the numerical methods used, the upward and downward continuation operators provided the most insight into the deep structural controls of the Sudbury Basin. Our preferred interpretation of the regional gravity field invokes a two‐component structure. Underlying the southern half of the Sudbury Structure is a laterally continuous gravity anomaly that is probably associated with a zone of uplifted Huronian volcanics. The gravity anomaly under the northern portion of the Sudbury Structure has a more restricted spatial extent. The close association between the northern limit of the gravity anomaly and the surface outcrop of the Levack Gneiss suggests the source of this anomaly is probably a slab of dense Levack Gneiss. This interpretation favors a meteorite impact origin for the Sudbury Structure.

8

Archambault, Daniel J., and Keith Winterhalder. "Metal tolerance in Agrostis scabra from the Sudbury, Ontario, area." Canadian Journal of Botany 73, no. 5 (May 1, 1995): 766–75. http://dx.doi.org/10.1139/b95-084.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Acid, metal-contaminated soils are frequently colonized by plant species that have evolved tolerance to metals. Agrostis scabra (tickle grass) grows at several such sites in the Sudbury area. To test whether these populations were tolerant to metals, three experiments were performed. A hydroponic root growth experiment, in which clonal ramets from contaminated and uncontaminated sites were grown in metal-amended nutrient solutions, showed that plants from the Sudbury area had greater tolerance indices than those from outside Sudbury. A seed-based hydroponic experiment, where seeds were germinated in metal solutions, showed that metal-tolerance indices calculated from root growth were mostly greater for populations from Sudbury but that leaf growth was not a good indicator of metal tolerance. A seed-based soil-bioassay experiment, in which seeds were germinated on soils covered with filter paper, showed that seeds from contaminated sites performed better on contaminated soil and a 50:50 soil mixture (contaminated–uncontaminated) than those from uncontaminated sites. Populations of A. scabra growing on contaminated soils in the Sudbury area therefore appear to have been selected for metal tolerance. Ecological aspects of metal tolerance and the possible role of A. scabra in the revegetation of the Sudbury area are discussed. Key words: Agrostis scabra, tolerance, metals, acid soil, contamination.

9

Prevec, Stephen A., Duncan R. Cowan, and Gordon RJ Cooper. "Geophysical evidence for a pre-impact Sudbury dome, southern Superior Province, Canada." Canadian Journal of Earth Sciences 42, no. 1 (January 1, 2005): 1–9. http://dx.doi.org/10.1139/e04-097.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

New filtering of aeromagnetic images of the Sudbury area indicates the existence of a large, elliptical feature that appears to underlie the deformed Sudbury Structure in the region of the exposed Levack Gneiss Complex, such that the two features have long axes which are significantly orthogonal to one another. A northsouth-oriented ellipse appears to be crosscut by that of the Sudbury Structure and does not correspond to known local lithological or structural trends. The magnetic images, combined with existing tectonic, petrological, geothermometric and geobarometric, and geochronological data, are used to suggest the existence of a pre-impact crustal dome in the southernmost Abitibi subprovince, probably related to ca. 2450 Ma rifting and magmatism in the area. This is consistent with existing petrological and tectonic evidence from a variety of sources. Although the doming is itself unrelated to the ca. 1850 Ma Sudbury event, it may have affected the thermal regime existing at the time of impact, which would have profound implications for the subsequent evolution of the Sudbury Igneous Complex.

10

Matuszek, John E., Donna L. Wales, and John M. Gunn. "Estimated Impacts of SO2 Emissions from Sudbury Smelters on Ontario's Sportfish Populations." Canadian Journal of Fisheries and Aquatic Sciences 49, S1 (December 19, 1992): 87–94. http://dx.doi.org/10.1139/f92-303.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Impacts of acidification on the major sportfish species in Ontario (lake trout (Salvelinus namaycush), brook trout (S. fontinalis), smallmouth bass (Micropterus dolomieu), and walleye (Stizostedion vitreum)) were estimated from the results of extensive water quality surveys conducted during the period 1978–85. Local impacts, within the 17 000 km2 area most affected by emissions from Sudbury smelters, were also estimated and compared with the provincial values. The estimated numbers of acidic lakes in Ontario in which viable sportfish populations have disappeared were 119 lake trout lakes (5.1% of known lake trout lakes), 34 brook trout lakes (1.6%), 52 smallmouth bass lakes (2.2%), and 14 walleye lakes (0.3%). Most of these affected lakes were in the Sudbury zone, where fish populations, particularly those of lake trout, began declining more than 30 yr ago. The estimated numbers of critically acidic lakes in the Sudbury zone were 94 lake trout lakes, 14 brook trout lakes, 18 smallmouth bass lakes, and 7 walleye lakes. More recent sampling of a subset of Sudbury lakes indicated that substantial water quality improvements have occurred as a result of emission reductions from Sudbury smelters.

Більше джерел

Дисертації з теми "Sudburg":

1

Dennie, Donald Carleton University Dissertation History. "Sudbury 1883-1946: a social historical study of property and class." Ottawa, 1989.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Giroux, Laura Allison. "Magnetic subfabrics of the Whistle Offset dyke and embayment, Sudbury Impact Structure, Sudbury, Ontario." Thesis, University of Ottawa (Canada), 2005. http://hdl.handle.net/10393/26913.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

Quartz-diorite Offset dykes from the 1850 Ma Sudbury Impact Structure stem from the Sudbury Igneous Complex (SIC) and extend into the footwall rocks in radial and concentric patterns with respect to the SIC. The dykes formed by emplacement of magma derived from the impact melt body into radial and concentric fractures generated in the country rock by the hypervelocity meteorite impact. The NE-striking Whistle Offset dyke extends from the northeast corner of the SIC, and is connected to the SIC by the Whistle embayment structure. A suite of oriented specimens was collected from 20 sites in the Whistle Offset dyke and the embayment, in order to determine the emplacement flow pattern within the dyke, the embayment, and the hosted massive sulfide deposits. The emplacement flow pattern was studied by using magnetic anisotropy measurements in order to infer the petrofabrics, and the subfabrics, defined by different mineral populations. The magnetic anisotropy methods included the anisotropy of magnetic susceptibility (AMS), the anisotropy of anhysteretic remanence (AAR) and the anisotropy of partial anhysteretic remanence (ApAR). The complex magnetic mineralogy of the sample suite was examined using measurements of partial anhysteretic remanence (PAR) acquisition, alternating-field demagnetization and thermal demagnetization, in addition to petrographic and scanning electron microscope (SEM) studies. The subfabrics which are interpreted to record the flow pattern in the Whistle Offset dyke, are defined by low coercivity coarse-grained magnetite, interpreted to be of primary igneous origin. The fabrics are suggestive of lateral (horizontal) injection of the magma and subsequent sinking of molten massive sulfide bodies through the still unsolidified dyke. Sinking of the massive sulfides is recorded by moderately plunging to vertical magnetic lineations. Steeply plunging lineations elsewhere in the Offset dykes may also indicate the presence of sunken massive sulfides in the subsurface.

3

Jung, Thomas S. "Habitat use by a forest-dwelling bat community in the northern Great Lakes region." Thesis, McGill University, 2000. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=33008.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

To examine bat - habitat relationships, ultrasonic detectors were used to sample bat activity among: old-growth white pine (Pinus strobus ), mature white pine, boreal mixedwood, and selectively-cut white pine stands in central Ontario. Within the stands, bats were sampled in the canopy, the understory layer, and within canopy gaps. Forest structure was measured within each of the stands. The activity of bats was compared among forest stand types, within the stands, and in relation to forest structure. Also, maintaining forest wildlife populations requires data on the use of snags (i.e. dead trees). To provide further resolution of the habitat requirements of forest-dwelling bats, radio telemetry and exit counts were used to investigate the roosting ecology of mouse-eared bats (Myotis lucifugus and M. septentrionalis). Characteristics of snags used by mouse-eared bats were compared with randomly located snags and random geographic points, at three spatial scales (focal tree, surrounding forest, and landscape). (Abstract shortened by UMI.)

4

Lafrenière, Ginette. "Women's community organizing experiences in Sudbury, Ontario : an exploratory look." Thesis, McGill University, 2005. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=85928.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

This qualitative study examines sixteen women's understanding of their experiences in community organizing in a northern urban context. While most front-line community organizing is done by women, there is a paucity of research giving voice to their particular realities. Similarly, there is little information describing community organizing in a northern urban context. The study's conceptual frameworks draw on theory and research from rural and northern social work, activist mothering, feminist social policy, diversity and exclusion, and the social construction of identities. It follows a feminist research paradigm. The study illustrates women community organizers' sense of place and their perceptions of the politics of language, cultural and linguistic tensions, and the influences of northern economic and geographic realities. The research findings demonstrate the processes of community organizing in a northern setting, community organizers' demoralization because of increasingly less generous social policy environments, and the challenges of racial and linguistic divisions in community organizing. The study challenges the urban lens dominating social work education and highlights the legitimacy of community organizing within social work education. It discusses future research possibilities for cross-cultural community organizing involving minority francophone and ethnocultural populations as well as the relativity of notions of oppression within francophone spheres.

5

Farrell, Keith Paul John. "Mafic to ultramafic inclusions in the sublayer of the Sudbury Igneous Complex at Whistle Mine, Sudbury, Ontario, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ31427.pdf.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

6

MacQueen, Joyce Marion. "Public health nursing in Sudbury, 1920-1956." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ31451.pdf.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

7

Lyon, Matthew Jeremy. "Neutron transport in the Sudbury neutrino detector." Thesis, University of Oxford, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.337422.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

8

Raymond, Valérie. "L'emprunt lexical à l'anglais dans le français oral des locuteurs bilingues de Sudbury : contrainte ou enrichissement pour une langue minoritaire." Thesis, Université Laval, 2011. http://www.theses.ulaval.ca/2011/28052/28052.pdf.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

9

Nelles, Edward William. "Genesis of Cu-PGE-rich footwall-type mineralization in the Morrison deposit, Sudbury." Thesis, Laurentian University of Sudbury, 2014. https://zone.biblio.laurentian.ca/dspace/handle/10219/2205.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

The Morrison deposit, located at the Levack mine in the City of Greater Sudbury, is a footwall-type Cu-Ni-platinum-group-element (PGE) deposit hosted within a zone of Sudbury Breccia in the Archean Levack Gneiss Complex beneath the North Range of the Sudbury Igneous Complex. It consists of sharp-walled, sulfide-rich veins that are enriched in Cu-Pt-Pd-Au relative to contact-type mineralization and can be subdivided based on vein geochemistry, mineralogy, texture, and morphology into a pyrrhotite-rich upper domain, a chalcopyrite-rich lower domain, and a pyrrhotite equal to chalcopyrite middle domain. All domains contain steeply to vertically dipping first-order sulfide veins, irregular and discontinuous second-order sulfide veins, and disseminated sulfides in country rocks. First- and second-order veins can be further subdivided into inclusion-free veins typically within Sudbury breccia matrix or along clast-matrix boundaries, and very irregular and inclusion-rich veins associated with leucosomes in mafic gneiss clasts and granophyric-textured dikes. First-order veins consist of pyrrhotite > chalcopyrite = pentlandite > magnetite in the upper domain, pyrrhotite = chalcopyrite > pentlandite > cubanite > magnetite in the middle domain, and chalcopyrite >> pentlandite > pyrrhotite = cubanite > magnetite in the lower domain. Second-order veins consist of pyrrhotite = chalcopyrite > pentlandite > magnetite and chalcopyrite = millerite = pentlandite in the middle domain, and chalcopyrite >> millerite, millerite > chalcopyrite, bornite >> chalcopyrite, and millerite > bornite > chalcopyrite in the lower domain. Second order veins are adjacent to and in contact with epidote, amphibole, chlorite, carbonate, quartz, and magnetite alteration minerals. Sulfide mineralization in the Morrison deposit is similar to other footwall mineralization associated with the SIC. The veins appear to have been emplaced preferentially into zones of Sudbury Breccia that were within ~400m of the basal contact of the SIC, because that lithology is more permeable and because those zones are within the thermal aureole of the cooling SIC permitting penetration of sulfide melts. The mineralogical, textural, and geochemical zoning in the chalcopyrite-pentlandite-pyrrhotite-rich parts of the Morrison deposit are best explained by partial fractional and/or equilibrium crystallization of MSS and ISS. Bornite ± millerite-rich mineralization are interpreted to have formed by reaction of residual sulfide melts with wall rocks, consuming Fe and S to form actinolitemagnetite- epidote-chlorite-sulfide reaction zones and driving the sulfide melt across the thermal divide in that part of the Fe-Cu-Ni-S system to crystallize borniteSS ± milleriteSS. Gold-Pt-Pd appear to have been more mobile than other metals, forming localized zones of enrichment, although it is not clear yet whether they were mobile as Au-Pt-Pd-Bi-Te-Sb-rich melts or aqueous fluids.

10

Tsui, Tyron. "Through-going muons at the Sudbury Neutrino Observatory." Thesis, University of British Columbia, 2009. http://hdl.handle.net/2429/7317.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Анотація:

This thesis presents results from the through-going muon analysis at the Sudbury Neutrino Observatory. Over 1229.26 days, 77376 direct cosmic ray muons above cosθ > 0.4 and 514 neutrino-induced muons in the range -1 < cosθ < 0.4 were detected. A log-likelihood analysis was performed on the neutrino-induced muons to produce a flux measurement and constrain atmospheric neutrino mixing parameters. The best-fit oscillation values were Δm² = (2.6±2.0) × 10⁻³ eV², sin²2θ = 1.0±0.1. The observed muon flux was found to be (2.48±0.25) × 10⁻¹³ cm⁻²s⁻¹sr⁻¹ resulting in an overall flux normalization 1.22±0.09 times the theoretical estimates from the Bartol group. The quoted uncertainties are 1-D marginalized. The no-oscillation hypothesis was ruled out at 99.8% confidence level. The observed number of direct cosmic ray muons was converted into a vertical depth intensity. The resulting fits to the intensity as a function of depth were I₀ = (0.93±0.05) × 10⁻⁶ cm⁻²s⁻¹sr⁻¹, x = 2.33±0.31 km.w.e. and α = 5.62±0.40.

Більше джерел

Книги з теми "Sudburg":

1

Thoms, Ray. Sudbury. Erin, Ont: Boston Mills Press, 1994.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Star, The Sudbury. Sudbury: A century in review. Sudbury, Ont: Sudbury Star, 2000.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

3

Survey, Ontario Geological. Aggregate Resources Inventory West of Sudbury: Regional Municipality of Sudbury and District of Sudbury. S.l: s.n, 1987.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

4

Berry, Allan W. Eighteenth century Sudbury. Ipswich: Suffolk Books, 1992.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

5

Corporation, Sudbury Regional Development. Sudbury : special report. Sudbury, Ont: Sudbury Regional Development Corporation, 2000.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

6

O'Neill, Maury. Sudbury statistical summary. Sudbury, Ont: Laurentian University, Department of History, 1986.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

7

Dale, Wilson. Sudbury electrics & diesels. Sudbury, Ont: Nickel Belt Rails, 2001.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

8

Donegan, Rosemary. Le paysage industriel à Sudbury =: Sudbury, the industrial landscape. Sudbury, Ont: Art Gallery of Sudbury = Galerie d'art de Sudbury, 1998.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

9

Corporation, Sudbury Regional Development. Manufacturers directory : Sudbury Region. Sudbury, Ont: Sudbury Regional Development Corporation, 1992.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

10

Desbiens, Patrice. Sudbury: Poèmes 1979-1985. Sudbury, ON: Prise de parole, 2000.

Знайти повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Більше джерел

Частини книг з теми "Sudburg":

1

Flamini, Enrico, Alessandro Coletta, Maria Libera Battagliere, and Maria Virelli. "Sudbury, Canada." In Encyclopedic Atlas of Terrestrial Impact Craters, 621–24. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-05451-9_172.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Grieve, Richard A. F. "Sudbury Impact Structure." In Encyclopedia of Astrobiology, 1–4. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_5220-1.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

3

Grieve, Richard A. F. "Sudbury Impact Structure." In Encyclopedia of Astrobiology, 2404–7. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_5220.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

4

Leslie, J. R. "The Sudbury Neutrino Observatory." In Trends in Astroparticle-Physics, 48–57. Wiesbaden: Vieweg+Teubner Verlag, 1994. http://dx.doi.org/10.1007/978-3-663-01466-9_4.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

5

Sinclair, D. "The Sudbury Neutrino Observatory." In Neutrino Physics, 239–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73679-7_24.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

6

Earle, E. D., G. T. Ewan, H. W. Lee, H. B. Mak, B. C. Robertson, R. C. Allen, H. H. Chen, et al. "The Sudbury D2O Neutrino Detector." In Weak and Electromagnetic Interactions in Nuclei, 737–40. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-71689-8_143.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

7

Dressler, B. O., G. G. Morrison, W. V. Peredery, and B. V. Rao. "The Sudbury Structure, Ontario, Canada — A Review." In Research in Terrestrial Impact Structures, 39–68. Wiesbaden: Vieweg+Teubner Verlag, 1987. http://dx.doi.org/10.1007/978-3-663-01889-6_3.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

8

Foster, Eric. "Dearness Environmental Society and the Sudbury Schools." In Schooling for Sustainable Development in Canada and the United States, 137–49. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4273-4_10.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

9

Naldrett, Anthony J. "Deposits of the Sudbury Camp, Ontario, Canada." In Magmatic Sulfide Deposits, 405–80. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08444-1_8.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

10

Ewan, George. "Solar Neutrino Measurements at the SUDBURY Neutrino Observatory." In Beyond the Desert 2003, 279–91. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18534-2_19.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Тези доповідей конференцій з теми "Sudburg":

1

Klein, Joshua R. "Sudbury Neutrino Observatory." In NEUTRINOS, FLAVOR PHYSICS, AND PRECISION COSMOLOGY: Fourth Tropical Workshop on Particle Physics and Cosmology. AIP, 2003. http://dx.doi.org/10.1063/1.1627724.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Ewan, G. T. "Sudbury Neutrino Observatory." In AIP Conference Proceedings Volume 164. AIP, 1987. http://dx.doi.org/10.1063/1.36983.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

3

Cohen, E. "Recollections of Roger sudbury." In 2011 IEEE/MTT-S International Microwave Symposium - MTT 2011. IEEE, 2011. http://dx.doi.org/10.1109/mwsym.2011.5973462.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

4

SIMPSON, J. J. "THE SUDBURY NEUTRINO OBSERVATORY." In Proceedings of the Carolina Symposium on Neutrino Physics. WORLD SCIENTIFIC, 2001. http://dx.doi.org/10.1142/9789812811714_0007.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

5

Duncan, Fraser. "The Sudbury Neutrino Observatory." In The seventh conference on the intersection of particles and nuclear physics. AIP, 2000. http://dx.doi.org/10.1063/1.1345370.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

6

Heise, J. "The Sudbury Neutrino Observatory." In Next generation nucleon decay and neutrino detector. AIP, 2000. http://dx.doi.org/10.1063/1.1361732.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

7

McDonald, A. B. "Sudbury Neutrino Observatory Results." In Proceedings of Nobel Symposium 129. WORLD SCIENTIFIC, 2006. http://dx.doi.org/10.1142/9789812773906_0003.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

8

Sudbury, D., and A. Sudbury. "Family perspectives on Roger Sudbury." In 2011 IEEE/MTT-S International Microwave Symposium - MTT 2011. IEEE, 2011. http://dx.doi.org/10.1109/mwsym.2011.5973461.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

9

Cowen, D. F., T. Ekenberg, J. R. Klein, F. M. Newcomer, R. Van Berg, R. G. Van de Water, P. Wittich, A. Biman, and R. L. Stevenson. "The Sudbury Neutrino Observatory electronics chain." In Proceedings of 1994 IEEE Nuclear Science Symposium - NSS'94. IEEE, 1994. http://dx.doi.org/10.1109/nssmic.1994.474527.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

10

Gelnovatch, W., and D. McQuiddy. "Recalling professional interactions with Roger Sudbury." In 2011 IEEE/MTT-S International Microwave Symposium - MTT 2011. IEEE, 2011. http://dx.doi.org/10.1109/mwsym.2011.5973460.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

Звіти організацій з теми "Sudburg":

1

Beier, E. W. Sudbury Neutrino Observatory. Office of Scientific and Technical Information (OSTI), March 1992. http://dx.doi.org/10.2172/5608387.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

2

Ames, D. E., I. M. Kjarsgaard, and S. L. Douma. Sudbury Ni-Cu-PGE ore mineralogy compilation: Sudbury Targeted Geoscience Initiative (TGI). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214521.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

3

Ames, D. E., A. Davidson, J. L. Buckle, and K. D. Card. Geology, Sudbury bedrock compilation, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/221501.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

4

Card, K., P. Huppé, C. Bowie, and J. Harris. Bedrock geology/airborne radar, Sudbury. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194046.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

5

Pearson, W. N., R. E. Bretzlaff, and J. J. Carriere. Copper Deposits and Occurrences, Sudbury, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120317.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

6

Legault, D., B. Lafrance, and D. E. Ames. Structural study of Sudbury breccia and sulphide veins, Levack embayment, North Range of the Sudbury structure, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214183.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

7

Rose, D. G. Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/129999.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

8

Card, K. D., B. V. Sanford, and A. Davidson. Bedrock Geology, Lake Superior-Sudbury, Ontario-United States. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/195140.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

9

Card, K. D., B. V. Sanford, and A. Davidson. Airborne Synthetic Aperture Radar (SAR)/geology, Sudbury, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/193704.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.

10

Davidson, A., and J. W. F. Ketchum. Grenville front studies in the Sudbury Region, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134254.

Повний текст джерела

Стилі APA, Harvard, Vancouver, ISO та ін.