Bibliographies thématiques / Geology - Ontario - Bonheur area

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Littérature scientifique sur le sujet « Geology - Ontario - Bonheur area »

Auteur : Grafiati
Publié le 4 juin 2021
Mis à jour le 29 juillet 2025

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Articles de revues sur le sujet "Geology - Ontario - Bonheur area"

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McDougall, Raymond. "Mineral Highlights from the Bancroft Area, Ontario, Canada." Rocks & Minerals 94, no. 5 (2019): 408–19. http://dx.doi.org/10.1080/00357529.2019.1619134.

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Lykova, Inna, John Montgomery, and John Biczok. "Strange Scepter Quartz from the Lyndhurst Area, Ontario, Canada." Rocks & Minerals 97, no. 3 (2022): 254–59. http://dx.doi.org/10.1080/00357529.2022.2028100.

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Lykova, Inna, John Montgomery, and John Biczok. "Strange Scepter Quartz from the Lyndhurst Area, Ontario, Canada." Rocks & Minerals 97, no. 3 (2022): 254–59. http://dx.doi.org/10.1080/00357529.2022.2028100.

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Kile, Daniel E. "Mineralogy of the Amethyst Mines in the Thunder Bay Area, Thunder Bay, Ontario, Canada." Rocks & Minerals 94, no. 4 (2019): 306–43. http://dx.doi.org/10.1080/00357529.2019.1595939.

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Fralick, Philip W., and Andrew D. Miall. "Sedimentology of the lower huronian supergroup (early proterozoic), Elliot lake area, Ontario, Canada." Sedimentary Geology 63, no. 1-2 (1989): 127–53. http://dx.doi.org/10.1016/0037-0738(89)90075-4.

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Sharpe, David R., and Peter J. Barnett. "Significance of Sedimentological Studies on the Wisconsinan Stratigraphy of Southern Ontario." Géographie physique et Quaternaire 39, no. 3 (2007): 255–73. http://dx.doi.org/10.7202/032607ar.

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ABSTRACTDetailed facies mapping along Lake Erie and Lake Ontario Bluffs, plus other studies illustrate that sedimentological studies, especially those with geomorphic or landform control, have had three main effects on the Wisconsinan stratigraphy of Ontario: (1) improved understanding of depositional processes and environments of several major rock stratigraphic units, without altering the stratigraphic framework, (2) aided correlation of drift sequences, and (3) questioned previous interpretations and stratigraphic correlations of drift sequences. Thus sedimentological analysis can not be se
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Cooper, A. J. "Waste disposal site selection techniques in Quaternary terraine Ontario, Canada." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 211–17. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.19.

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AbstractThick and predictable deposits of fine grained Quaternary materials have been used for the siting of waste management facilities in Ontario. The search for such sites is founded on the application of techniques in Quaternary geology and hydrogeology. Two examples are presented. Oxford County is located southwest of Toronto in an area of parallel morainic ridges separated by flat till plains. Conventional wisdom would focus on the till plains for thick, consistent fine grained Quaternary Sediments. However, the careful analysis of the Quaternary stratigraphy and glacial history revealed
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Fee, E. J., and R. E. Hecky. "Introduction to the Northwest Ontario Lake Size Series (NOLSS)." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 12 (1992): 2434–44. http://dx.doi.org/10.1139/f92-269.

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The rationale, design, and limitations of the Northwest Ontario Lake Size Series (NOLSS) research program are described. The primary purpose of NOLSS is to discover how lake size per se influences limnological and fisheries phenomena, so that conclusions drawn from studies of particular lakes can be rigorously scaled and applied to lakes of other sizes. NOLSS consists of six lakes located in a remote wilderness region of Northwest Ontario. These lakes were chosen for their geological, hydrological, and morphological similarity (Canadian Shield geology; water renewal time> 5 yr; fully strati
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Motazedian, Dariush, and James Hunter. "Development of an NEHRP map for the Orleans suburb of Ottawa, Ontario." Canadian Geotechnical Journal 45, no. 8 (2008): 1180–88. http://dx.doi.org/10.1139/t08-051.

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The average shear-wave velocity to a depth of 30 m (Vs30) has been obtained for 73 sites in the Orleans area in the northeast part of the City of Ottawa. Measurements of Vs30 were made using both ground surface reflection and refraction methods. In addition, borehole data was used to estimate Vs versus depth profiles using average Vs values assigned to distinct geological units. High values of Vs (>1500 m/s) were obtained in areas of thin surficial sediments overlying Paleozoic bedrock, and low Vs values (<180 m/s) were calculated in areas of thick late–post-glacial clay. The Vs30 values
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Mohajer, Arsalan A. "Seismicity and Seismotectonics of the Western Lake Ontario Region." Géographie physique et Quaternaire 47, no. 3 (2007): 353–62. http://dx.doi.org/10.7202/032963ar.

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ABSTRACTThe western Lake Ontario region, a traditionally perceived area of low seismic risk, is densely populated and is home to, among other critical facilities, the nuclear reactors of Pickering and Darlington. These and other characteristics of the region call for improved estimates of seismic hazard. Due to a lack of understanding of the causative geological sources and recurrence characteristics of the reported seismic activity, there is considerable uncertainty regarding estimated ground motion parameters, a fundamental component of seismic hazard assessments. To attempt to improve the d
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Thèses sur le sujet "Geology - Ontario - Bonheur area"

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Brown, Julie Louise. "Neoarchean evolution of the western-central Wabigoon boundary zone, Brightsand Forest Area, Ontario." Thesis, University of Ottawa (Canada), 2002. http://hdl.handle.net/10393/6451.

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The boundary between the western and central domains of the Wabigoon subprovince has been considered to represent a ca. 2.7 Ga suture between juvenile Neoarchean volcanic rocks in the west and granitoid rocks with Mesoarchean ancestry in the central Wabigoon. The nature and timing of interaction between these two terranes was examined southeast of the Sturgeon Lake greenstone belt within the central Wabigoon, where amphibolite-facies supracrustal remnants are dismembered by Neoarchean plutonic rocks and shear zones. Of the 4 preserved ductile deformation fabrics, D1 and D2 are bracketed by a 2
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Leblanc, Genevieve. "Geology and mineralization in the Big Four Lake area, Shining Tree, Abitibi greenstone belt, Ontario." Thesis, University of Ottawa (Canada), 2008. http://hdl.handle.net/10393/27699.

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The purpose of the research work (in partnership with the Ontario Geological Survey (OGS) and International KRL Resources Corp. (KRL)) was to better define the geology and mineralization of the Big Four Lake area, close to Shining Tree in Ontario, part of the southwesthern Abitibi greenstone belt. Rocks of the area belong to the Deloro assemblage a suite of calc-alkaline mafic to felsic metavolcanic rocks, tholeiitic mafic to intermediate metavolcanic rocks, iron formation plus komatiites of the Kidd-Munro and Pacaud assemblages, all cut by later intrusions. The rocks are metamorphosed to the
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Chow, Andre M. C. (Andre Mu-Chin). "Sedimentology and paleontology of the Attawapiskat Formation (Silurian) in the type area, northern Ontario." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65494.

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Smyk, Mark Cory 1961 Carleton University Dissertation Geology. "Geology of Archean interflow sedimentary rocks and their relationship to Ag-Bi-Co-Ni-As veins, Cobalt area, Ontario." Ottawa.:, 1987.

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McMullen, Sarah Margaret. "Tectonic evolution of the Bark Lake area, eastern Central Gneiss Belt, Ontario Grenville, constraints from geology, geochemistry and U-Pb geochronology." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0010/MQ48503.pdf.

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McMullen, Sarah Margaret Carleton University Dissertation Earth Sciences. "Tectonic evolution of the Bark Lake area, Eastern Central Gneiss Belt, Ontario Grenville; constraints from geology, geochemistry and U-Pb geochronology." Ottawa, 1999.

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Murphy, Elena I. "Geology, metamorphism, and geochemistry of Southern and Grenville Province rocks in the vicinity of the Grenville Front, Timmins Creek area, near Sudbury, Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0018/MQ46496.pdf.

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Livres sur le sujet "Geology - Ontario - Bonheur area"

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McKenzie, D. Ian. Quaternary geology of the Waterloo area, Ontario. Geological Association of Canada/Mineralogical Association of Canada, 1994.

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Stone, Denver. Geology of the northern Superior area, Ontario. Ontario Geological Survey, 2005.

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Stone, Denver. Precambrian geology of the Atikokan area, northwestern Ontario. Geological Survey of Canada, 1992.

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C, Kamineni D., Jackson M. C, and Geological Survey of Canada, eds. Precambrian geology of the Atikokan area, northwestern Ontario. Energy, Mines and Resources Canada, 1992.

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Stone, Denver. Precambrian geology of the Berens River Area, Northwest Ontario. Mines and Minerals Information Centre, 1998.

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Karrow, P. F. Quaternary geology of the Hamilton - Cambridge area: Southern Ontario. Ontario Ministry of Northern Development and Mines, 1987.

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A, Davidson. Grenville front relationships in the Sudbury area, Ontario. Geological Association of Canada/Mineralogical Association of Canada, 1994.

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Barnett, P. J. Quaternary geology of the Bancroft area: Southern Ontario. Ontario Ministry of Northern Development and Mines, 1989.

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Thorleifson, L. Harvey. Quaternary geology and drift prospecting, Beardmore-Geraldton area, Ontario. Geological Survey of Canada, 1993.

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J, Frarey M. Proterozoic geology of the Lake Panache-Collins Inlet area, Ontario. Geological Survey of Canada, 1985.

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Chapitres de livres sur le sujet "Geology - Ontario - Bonheur area"

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Sharpe, David R. "Quaternary geology of Toronto area, Ontario." In Centennial Field Guide Volume 5: Northeastern Section of the Geological Society of America. Geological Society of America, 1987. http://dx.doi.org/10.1130/0-8137-5405-4.339.

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Cater, D. F. "Macassa Mine Geology." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch04.

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Abstract The Macassa Mine, a division of LAC Minerals Ltd. is situated immediately west of the town of Kirkland Lake, Ontario. It is the only active producer of seven (7) mines located along the famed Mile of Gold in the Kirkland Lake Gold Camp. Production from all seven mines in the camp from inception to the end of 1989 amounted to 52.6 million tons generating 23.4 million ounces at an average grade of 0. 446 ounce/ton (source: MNDM resident geologists office pers. comm. ). Production at the Macassa Mine commenced in late 1933 at a rate of 200 tons per day. The mine has produced gold continu
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Powell, W. G., M. W. Kilbourne, and C. J. Hodgson. "Gold-Related Geology of the Matachewan Camp." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch07.

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Abstract The Matachewan camp is located in the southwestern Abitibi Greenstone Belt of the Superior Province, 55 kilometres west of Kirkland Lake, northeastern Ontario. Gold production from the camp has come entirely from two contiguous mines, the Young-Davidson mine (YDM) and the Matachewan Consolidated mine (MCM). Between 1933 and 1957, a total of 9. 6 million tonnes of ore with an average grade of 3. 1 g/t Au and 0. 93 g/t Ag was produced from these mines. In 1979-80 Pamour Porcupine Mines Limited removed an additional 18,000 tonnes of ore at >3.4 g/t from open pit operations on the
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"Archean Au Quartz Vein Mineralization Hosted in a Tonalite-Trondhjemite Terrane, Renabie Mine Area, Wawa, North Ontario, Canada." In The Geology of Gold Deposits. Society of Economic Geologists, 1989. http://dx.doi.org/10.5382/mono.06.01.

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Motel, Bon Air, and Kirkland Lake. "Underground Tour of Macassa Mine." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch02.

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Abstract 1991 MAY 31 FRIDAY MORNING tour underground at Macassa. From the Bon Air Motel, proceed 5.85 km west along Highway 66 (Government Road) then turn right; at 6.85 km park near Macassa No.3 shaft headframe. For a description see paper entitled “Macassa Mine Geology” in this guidebook.
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Cater, D. F. "Underground Tour of Holt-Mcdermott Mine; Freewest Resources Teddy Bear Valley and Pyke Hill." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch09.

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Abstract The trip begins in Toronto (1991 May 30 Thursday) and proceeds to Kirkland Lake by motor coach. The evening includes a Kirkland Lake branch CIM meeting (speaker Wayne Benham on a recent Kirkland Lake gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater.
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Cater, D. F. "Return Trip to Toronto." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch10.

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Abstract The trip begins in Toronto (1991 May 30 Thursday) and proceeds to Kirkland Lake by motor coach. The evening includes a Kirkland Lake branch CIM meeting (speaker Wayne Benham on a recent Kirkland Lake gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater.
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Cater, D. F. "Travel from Toronto to Kirkland Lake." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch01.

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Abstract The trip begins in Toronto (1991 May 30 Thursday) and proceeds to Kirkland Lake by motor coach. The evening includes a Kirkland Lake branch CIM meeting (speaker Wayne Benham on a recent Kirkland Lake gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater.
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Robbins, Eleanora I., and Michalann Harthill. "Life in a Copper Province." In Geology and Health. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195162042.003.0024.

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The North American Lake Superior region contains a world-class copper province nearly 300,000 km² in area. A dozen major copper deposits and hundreds of smaller mineral accumulations are located in Michigan, Minnesota, and Ontario (Morey and Sims 1996), many of which include As, nickel (Ni), platinum (Pt), palladium (Pd), Co, Mo, and Fe, as well as Cu (Nicholson et al. 1992). Historically, the province has hosted a variety of life forms; fossil biota have been traced as far back as 2.6-2.75 Ga. Palynological and microbial research (Robbins 1985, Robbins et al. 1994) prompts speculation about p
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Cater, D. F. "Larder Lake Gold Field Trip." In Archean Gold Deposits of the Matachewan-Kirkland Lake-Larder Lake Area, Ontario, Canada. Society of Economic Geologists, 1991. http://dx.doi.org/10.5382/gb.11.ch08.

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Abstract 1991 JUNE 02 SUNDAY MORNING AND AFTERNOON TOUR will be by bus, which will carry the lunches so we can eat wherever we happen to be around noon time. The two longest walks from the bus should total less than 4 km “round trip”. If time becomes too short to visit to-day’s 10 tour stops (No. 6 to 15), one or more might have to be left out. This will ensure that we arrive back at the motel in time to prepare for the evening meal followed by the talk on American Barrick’s Holt-McDermott gold mine, where you will go underground to-morrow and receive a mine description handout. For a descript
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Rapports d'organisations sur le sujet "Geology - Ontario - Bonheur area"

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Stone, D., and D. C. Kamineni. Geology, Atikokan area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127620.

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Morton, R. L., G. Hudak, and J. M. Franklin. Geology, south Sturgeon Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210728.

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Stone, D., C. Kamineni, M. Jackson, and W. Shanks. Geology of the Atikokan area, Northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130128.

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Sanborn-Barrie, M., and T. Skulski. Structural geology, central Sturgeon Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209936.

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Percival, J. A., S. Castonguay, J. B. Whalen, J. L. Brown, V. McNicoll, and J. R. Harris. Geology, Sturgeon Lake-Obonga Lake area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210472.

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St-Onge, D. A. Quaternary geology of the Cornwall area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/223019.

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Brennand, T. A. Preliminary surficial geology site attributes, Oshawa area, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194144.

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Matile, G. L. D., and L. H. Thorleifson. Surficial geology, Falcon Lake area, Manitoba and Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207499.

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Stone, D., D. C. Kamineni, and M. C. Jackson. Precambrian geology of the Atikokan area, northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/134053.

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Matile, G. L. D., and L. H. Thorleifson. Surficial geology - Whitemouth Lake area, Manitoba, Ontario, and Minnesota. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/203614.

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