Relevant bibliographies by topics / Geology – Ontario – Batchawana Area

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  2. Dissertations / Theses
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Academic literature on the topic 'Geology – Ontario – Batchawana Area'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Geology – Ontario – Batchawana Area"

1

Kelso, J. R. M. "Fish Community Structure, Biomass, and Production in the Turkey Lakes Watershed, Ontario." Canadian Journal of Fisheries and Aquatic Sciences 45, S1 (1988): s115—s120. http://dx.doi.org/10.1139/f88-275.

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The Turkey Lakes Watershed contains four lakes, and the headwater lake (Batchawana Lake) consists of two distinct basins, neither of which supports a native, reproducing fish stock. Fish biomass varied by a factor of 3.3 among the other three lakes in the watershed. Fish flesh production varied by a factor of only 1.5 in the system. Salmonid and small cyprinid contribution to biomass and production increased with progression downstream. Both fish biomass and production per unit surface area decreased with increasing lake depth. The fish biomass and production in the watershed was strongly infl
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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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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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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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7

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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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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MIALL, ANDREW D. "Sedimentation on an early Proterozoic continental margin under glacial influence: the Gowganda Formation (Huronian), Elliot Lake area, Ontario, Canada." Sedimentology 32, no. 6 (1985): 763–88. http://dx.doi.org/10.1111/j.1365-3091.1985.tb00733.x.

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Eyles, N., and K. W. F. Howard. "A hydrochemical study of urban landslides caused by heavy rain: Scarborough Bluffs, Ontario, Canada." Canadian Geotechnical Journal 25, no. 3 (1988): 455–66. http://dx.doi.org/10.1139/t88-051.

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Scarborough Bluffs is a 15 km long stretch of the Lake Ontario shoreline east of downtown Toronto. This heavily urbanized area currently represents Canada's most serious erosion problem. The worst affected zone is 1.5 km long and lies along South Marine Drive where 50 m high bluffs are failing by shallow retrogressive failures of jointed glacial clays over underlying deltaic sands and clays. The erosion rate is about four times that for the coastline as a whole.Heavy rains in the Toronto area in August and September 1986 produced a spate of slope failures and mud flows. Particularly heavy stor
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Dissertations / Theses on the topic "Geology – Ontario – Batchawana Area"

1

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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7

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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Books on the topic "Geology – Ontario – Batchawana 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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2

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

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3

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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5

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

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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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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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9

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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Book chapters on the topic "Geology – Ontario – Batchawana Area"

1

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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"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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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 possible correlations between copper and the biota that evolved there. Because the region has been subjected to continental collisions, volcanism, glaciation, rifting, weathering, sea level rise and fall, waxing and waning of lakes, soil formation, and now to human settlement and development including mining, the fossil record is discontinuous. This review of the geologic formations in the Lake Superior region from the Precambrian to the present, and their copper and biotic occurrences and associations, attempts to illuminate some of those geologic/ biologic correlations, and includes mention of modern environmental concerns. Copper is one of nearly 75 chemical elements contributing to metabolic or structural functions of organisms (Dexter-Dyer et al. 1984). Bioassimilation varies and depends not only on availability from the environment, but also on the species, gender, and age of organism with specific concentrations also depending on diet, health, tissue assayed, and various synergisms with other trace elements such as Fe and Zn. Indeed, copper is an essential element and co-factor contributing to copper-associated polypeptides that provide catalytic and electron transfer functions in almost every known group of organisms alive today, from bacteria to humans. Copper proteins contribute to skin pigmentation, nerve coverings, and in mechanisms of development, maintenance, and repair of connective tissues important for well-functioning cardiovascular systems (Eisler 2000). Presently, over two dozen essential copper proteins, some with porphyrin-copper functional groups (similar to the porphyrin-iron association in hemoglobin), have been identified, each with its specific developmental or physiological function (Cowan 1998).
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"Landscape Influences on Stream Habitats and Biological Assemblages." In Landscape Influences on Stream Habitats and Biological Assemblages, edited by Les W. Stanfield and Bruce W. Kilgour. American Fisheries Society, 2006. http://dx.doi.org/10.47886/9781888569766.ch28.

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<em>Abstract.</em>—–We demonstrate the effects of percent impervious cover (PIC) on biophysical properties of Lake Ontario tributary streams. Biophysical data (fish assemblages, benthic invertebrate assemblages (benthos), instream physical habitat, and temperature) were collected from more than 575 wadeable stream sites. A geographic information system application was developed to characterize the landscape upstream of each site (i.e., drainage area, surficial geology, land use/land cover, slope, stream length, and climate). Total PIC of catchments was estimated from land use/land cover, and a base flow index was derived from the surficial geology. The relationship between PIC and biophysical responses was determined after statistically removing the effects of natural landscape features (i.e., catchment area, slope, base flow index) on those responses. Contrasts in PIC from natural conditions (<3% to 10%) were related to variations in fish and benthos assemblages. Both coldwater sensitive and warmwater tolerant fish and diverse benthos assemblages were found in catchments with low PIC. At more than 10 PIC (i.e., about 50% urban), both fish and benthos consisted of mainly warmwater or tolerant assemblages. For example, trout were absent and minnows were dominant. While some of the apparent PIC effect may have been confounded by land use/land cover and surficial geology, the consistency of the findings even after natural catchment conditions were considered suggests that the threshold response is valid. Percent impervious cover had a weaker effect on instream geomorphic variables than on biological variables. The models derived from this study can be used to predict stream biophysical conditions for catchments with varying levels of development.
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"Landscape Influences on Stream Habitats and Biological Assemblages." In Landscape Influences on Stream Habitats and Biological Assemblages, edited by Bruce W. Kilgour and Les W. Stanfield. American Fisheries Society, 2006. http://dx.doi.org/10.47886/9781888569766.ch30.

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<em>Abstract.</em>—Assessments of stream fish or benthos assemblages normally involve a contrast of conditions at test sites to conditions represented by regional reference sites that are either minimally or least disturbed. Identification of reference sites is difficult and normally involves a variety of subjective criteria. The development of reference models for stream fish and benthos in the Canadian tributaries of Lake Ontario is particularly challenging because there are few undeveloped areas and there is no consensus on criteria for a least-disturbed condition. Rather than identify sites as representing a least-disturbed condition, we developed a series of models that relate the existing biophysical condition of streams (i.e., the fish, benthos, and instream habitat) to landscape (i.e., slope, geology, catchment area) and land use/land cover (percent impervious cover [PIC]). Relationships between indices of biophysical condition and PIC can be used to hindcast or estimate the expected biophysical condition at a variety of land cover scenarios. The models cannot be used to predict conditions outside the calibration data range, but this approach does allow us to make use of a disturbance gradient and make predictions with a minimal number of least-disturbed sites. The difference between the hindcast reference and present day conditions is an estimate of present-day impacts. Results from this exercise provided an estimate of the magnitude of impairment of streams in the Canadian portion of the Lake Ontario region.
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Reports on the topic "Geology – Ontario – Batchawana Area"

1

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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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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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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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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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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