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Letteratura scientifica selezionata sul tema "Kalgoorlie"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 20 febbraio 2023

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Articoli di riviste sul tema "Kalgoorlie"

1

Kerr, B. "A Metaplan Approach to Needs Assessment." Aboriginal Child at School 16, no. 3 (July 1988): 37–44. http://dx.doi.org/10.1017/s0310582200015418.

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This paper outlines an approach used by the Aboriginal Education Unit - Kalgoorlie Education Centre, W.A., to determine the educational needs of Aboriginal Communities. The team that carried out this program were: Mr Billy Kerr, Aboriginal Education Officer, Kalgoorlie D.E.C.; Mr Billy Vincent, Aboriginal Liaison Officer, Kalgoorlie D.E.C.; Mr Neil Darby, Priority Country Areas Program Field Officer, Kalgoorlie D.E.C.; Mr Ted Penny, Community/Schools Liaison Unit, Ministry of Education; Mr Lex Leslie, Principal, Yintarri School, Coonana.

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2

Vielreicher, Noreen Mary, David Ian Groves, and Neal Jesse McNaughton. "The giant Kalgoorlie Gold Field revisited." Geoscience Frontiers 7, no. 3 (May 2016): 359–74. http://dx.doi.org/10.1016/j.gsf.2015.07.006.

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3

Zhang, Xihong, Yu-Wen Chiu, Hong Hao, Ariel Hsieh, Phil Dight, and Kewei Liu. "Dynamic compressive properties of Kalgoorlie basalt rock." International Journal of Rock Mechanics and Mining Sciences 135 (November 2020): 104512. http://dx.doi.org/10.1016/j.ijrmms.2020.104512.

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4

Phillips, G. Neil. "Geology and alteration in the Golden Mile, Kalgoorlie." Economic Geology 81, no. 4 (July 1, 1986): 779–808. http://dx.doi.org/10.2113/gsecongeo.81.4.779.

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5

McMickan, Peter J., Paul C. C. Sauter, and Kim F. Frankcombe. "Geophysical Investigations of the Kalgoorlie Goldfield, Western Australia." Exploration Geophysics 25, no. 3 (September 1994): 167. http://dx.doi.org/10.1071/eg994167a.

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6

Hastie, C. W., J. M. Limerick, R. A. Campain, and N. J. Horner. "A Review of Automation at Kalgoorlie Nickel Smelter." IFAC Proceedings Volumes 18, no. 6 (July 1985): 199–205. http://dx.doi.org/10.1016/s1474-6670(17)60510-x.

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7

Smith, Leslie. "Flexible Delivery of Education in Kalgoorlie: Planning and Opening a Flexible Delivery Centre of Education at Curtin University Kalgoorlie Campus." Australian and International Journal of Rural Education 10, no. 1 (March 1, 2000): 40–45. http://dx.doi.org/10.47381/aijre.v10i1.450.

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Many learning institutions have been restructuring to meet the demands of clients and staff (Nicholls 1996). Over the last two years the Kalgoorlie campus has been re-engineering its structure, including its management practices and teaching and learning strategies. Just as the administration has to be lean and mean in these economic times, so the teaching and learning has to be cost effective, however our main reason for bringing in flexible learning is to improve customer service' and increase the number of student enrolments. In other campuses offering flexible learning it has been found th

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8

Phillips, G. Neil, David I. Groves, F. B. Neall, T. H. Donnelly, and I. B. Lambert. "Anomalous sulfur isotope compositions in the Golden Mile, Kalgoorlie." Economic Geology 81, no. 8 (December 1, 1986): 2008–15. http://dx.doi.org/10.2113/gsecongeo.81.8.2008.

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9

Yan, D. "Dewatering of fine slurries by the Kalgoorlie Filter Pipe." Minerals Engineering 16, no. 3 (March 2003): 283–89. http://dx.doi.org/10.1016/s0892-6875(03)00005-0.

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10

MacRae, Colin M., Nicholas C. Wilson, and Joel Brugger. "Quantitative Cathodoluminescence Mapping with Application to a Kalgoorlie Scheelite." Microscopy and Microanalysis 15, no. 3 (May 22, 2009): 222–30. http://dx.doi.org/10.1017/s1431927609090308.

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AbstractA method for the analysis of cathodoluminescence spectra is described that enables quantitative trace-element-level distributions to be mapped within minerals and materials. Cathodoluminescence intensities for a number of rare earth elements are determined by Gaussian peak fitting, and these intensities show positive correlation with independently measured concentrations down to parts per million levels. The ability to quantify cathodoluminescence spectra provides a powerful tool to determine both trace element abundances and charge state, while major elemental levels can be determined

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Tesi sul tema "Kalgoorlie"

1

Steinert, Aaron. "Development of hardpans on Hypersaline Tailings Kalgoorlie, W.A. /." Adelaide, 1998. http://web4.library.adelaide.edu.au/theses/09SB/09sbs822.pdf.

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2

Hartley, Richard G. "A history of technological change in Kalgoorlie gold metallurgy 1895-1915." Thesis, Hartley, Richard G. (1998) A history of technological change in Kalgoorlie gold metallurgy 1895-1915. PhD thesis, Murdoch University, 1998. https://researchrepository.murdoch.edu.au/id/eprint/51199/.

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Because of the peculiar characteristics of the Kalgoorlie goldfield's environment and geology, its metallurgy developed largely independently of other major gold mining centres. Its engineers and metallurgists borrowed ideas from a variety of sources to develop new equipment such as the filter press and the tube mill and new procedures such as the 'Australian method' of treating ores by fine crushing, sliming and filtration. By 1905 Kalgoorlie was the leading centre for gold metallurgical development in the world, and equipment and techniques developed there were adopted with remarkable rapidi

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3

Harris, Kira Jada. "One percent motorcycle clubs: Has the media constructed a moral panic in Kalgoorlie-Boulder, Western Australia?" Thesis, Edith Cowan University, Research Online, Perth, Western Australia, 2009. https://ro.ecu.edu.au/theses/1881.

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The purpose of this study was to evaluate an instrument designed to assess the influence of the media on opinions regarding the one percent motorcycle clubs in Kalgoorlie-Boulder, establishing whether the media had incited a moral panic towards the clubs. The concept of the moral panic, developed by Stanley Cohen iii ( 1972), is the widespread fear towards a social group by events that are overrepresented and exaggerated. Exploring the concept of a moral panic towards the one percent sub-culture, this study compares the perceptions from two groups of non-members in Kalgoorlie-Boulder. One grou

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4

Gregson, Sarah School of Industrial Relations &amp Organisational Behaviour UNSW. "Foot soldiers for capital: the influence of RSL racism on interwar industrial relations in Kalgoorlie and Broken Hill." Awarded by:University of New South Wales. School of Industrial Relations and Organisational Behaviour, 2003. http://handle.unsw.edu.au/1959.4/19331.

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The historiography of Australian racism has principally "blamed" the labour movement for the existence of the White Australia policy and racist responses to the presence of migrant workers. This study argues that the motivations behind ruling class agitation for the White Australia policy have never been satisfactorily analysed. To address this omission, the role of the Returned and Services League of Australia (RSL) in race relations is examined. As an elite-dominated, cross-class organisation with links to every section of society, it is argued that the RSL was a significant agitator for mig

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5

Rule, Matt. "Feasibility of a grid connected solar power tower with molten salt storage plant for Kalgoorlie-Boulder, Western Australia." Thesis, Rule, Matt (2016) Feasibility of a grid connected solar power tower with molten salt storage plant for Kalgoorlie-Boulder, Western Australia. Masters by Coursework thesis, Murdoch University, 2016. https://researchrepository.murdoch.edu.au/id/eprint/35884/.

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Solar power tower (SPT) plants with thermal energy storage (TES) provide great opportunities on the utility-scale; becoming a viable option for areas with moderate to high direct solar availability. The absence of commercial SPTs in Australia, together with the need to increase renewable energy capacity, raises the importance of proving it viable and beneficial. There is an apparent research gap, specifically, into the feasibility of a grid connected SPT with molten salt storage system for the Goldfields city, which this research explores. In this dissertation, solar power tower with storage s

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Mamuse, Antony. "Spatial statistical estimation of undiscovered mineral endowment: case of komatiite-associated nickel sulphide resources, Kalgoorlie Terrane, Western Australia." Thesis, Curtin University, 2010. http://hdl.handle.net/20.500.11937/449.

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The Kalgoorlie Terrane of the Yilgarn Craton, Western Australia, containing about 60% (~11 Mt) of the world’s known komatiite-hosted nickel sulphide resources, is the world’s best studied and economically most important province for this mineral deposit type. Although increasingly mature in terms of nickel exploration, the Kalgoorlie Terrane is believed to contain significant additional undiscovered nickel endowment. Using the data-rich Kalgoorlie Terrane, this thesis develops a benchmark methodology that combines geological knowledge with spatial analysis and mathematical-statistical methods

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7

Kyaw-Myint, Su Mon, and N/A. "Salivary IgA responses during the first two years of life: a study of aboriginal and non-aboriginal children." University of Canberra. Applied Science, 2003. http://erl.canberra.edu.au./public/adt-AUC20050523.095413.

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Nontypeable Haemophilus influenzae (NTHi), Streptococcus pneumoniae and Moraxella catarrhalis are common bacterial agents of otitis media which is a major cause of morbidity in young children. Mucosal immune responses are an integral part of the immune defense against middle ear infection and it is known that certain populations, including Australian Aboriginal children, are highly susceptible to disease. The current study focussed on the development of the mucosal immunity to the three bacterial pathogens in Aboriginal and non-Aboriginal children from birth to two years of age, living in the

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Said, Nuru. "Geochemistry of the Neoarchean mafic volcanic and intrusive rocks in the Kalgoorlie Terrane, eastern Yilgarn, Western Australia : implications for geodynamic setting." University of Western Australia. School of Earth and Environment, 2009. http://theses.library.uwa.edu.au/adt-WU2009.0156.

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[Truncated abstract] The Neoarchean (2800 to 2600 Ma) Eastern Goldfields Superterrane (EGST) comprises elongated belts of deformed and metamorphosed volcanic and sedimentary rocks intruded by granitoids. The Superterrane is made up of five distinct tectonostratigraphic terranes. From west to east these are the Kalgoorlie, Gindalbie, Kurnalpi, Laverton and Duketon Terranes. The Kalgoorlie Terrane is characterised by 2720 to 2680 Ma marine mafic-ultramafic volcanic successions interlayered with, and overlain by, 2710 to 2660 Ma dominantly trondhjemite-tonalite-dacite (TTD) dacititic volcaniclast

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9

Pick, David. "Making sense of a merger: A study of frame shifts in the merger between the Western Australian School of Mines and Kalgoorlie College." Thesis, Pick, David (2002) Making sense of a merger: A study of frame shifts in the merger between the Western Australian School of Mines and Kalgoorlie College. PhD thesis, Murdoch University, 2002. https://researchrepository.murdoch.edu.au/id/eprint/51213/.

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Late in 1996, Kalgoorlie College and the Western Australian School of Mines in Western Australia were merged to form an expanded campus of Curtin University, based in the state capital City of Perth. This event is examined as an episode of organisation change, with a particular focus on the micro-level experience of the various actors and groups involved in the change episode. The merger took place against a background of multi-level social and institutional change: for the Kalgoorlie-Boulder regional economy, in Australian higher educational policy and in national economic and social policy i

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Latchford, Norma. "A Study of the Relationship between Mining and the Performing Arts in Australia 1850 – 1914: case studies of the Ballarat and Kalgoorlie-Boulder goldfields." Thesis, Curtin University, 2020. http://hdl.handle.net/20.500.11937/78567.

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In describing the historical development of these two settlements based on mining, this thesis outlines the ways in which the performing arts played a significant role in the evolving social and cultural development of both centres and that mining, especially in the form of the these two goldrushes, was highly influential in the distinctive development of the performing arts in Australia in the second half of the nineteenth century and beyond.

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Libri sul tema "Kalgoorlie"

1

Dwyer, Jack. In old Kalgoorlie. Perth, WA: Western Australian Museum, 1989.

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2

Phillips, G. Neil. A century of gold mining at Kalgoorlie. Townsville, Australia: Economic Geology Research Unit, Key Centre in Economic Geology, James Cook University of North Queensland, 1993.

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3

Rycroft, Alan. Kalgoorlie-Leonora, timber bridges: Strength evaluation by testing. [Australia]: Westrail, 1992.

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4

Kern, A. M. Hydrogeology of the Kalgoorlie 1:250 000 sheet. Perth: Geological Survey of Western Australia, Dept. of Minerals and Energy, 1995.

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5

Keats, W. Regional geology of the Kalgoorlie-Boulder gold-mining district. Perth: Geological Survey of Western Australia, 1987.

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6

Regional geology of the Kalgoorlie-Boulder gold-mining district. Perth: State Print. Division, 1987.

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EXPLO '99 (Conference) (1999 Kalgoorlie, Western Australia). EXPLO '99 7 - 11 November 1999 Kalgoorlie, Western Australia. Edited by Workman-Davies Clive, Australasian Institute of Mining and Metallurgy., and Western Australian School of Mines. Carlton, Vic: Australasian Institute of Mining and Metallurgy, 1999.

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8

1962-, McDonald Bernadette, ed. The fields: The Kalgoorlie and Coolgardie Goldfields, 1892-1912. Fremantle, W.A: Fremantle Arts Centre Press, 1988.

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9

King, Norma. The voice of the goldfields: 100 years of the Kalgoorlie miner. Kalgoorlie: Hocking, 1995.

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10

Contract Operators' Conference (1996 Kalgoorlie, W.A.). Contract Operators' Conference: 28-29 October 1996, Kalgoorlie, Western Australia. Carlton, Vic: Australasian Institute of Mining and Metallurgy, 1996.

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Capitoli di libri sul tema "Kalgoorlie"

1

Grimsey, David, Eric Grimsey, and Peter Bjorklund. "Fluxing Optimisation and Control Improvements at the Kalgoorlie Nickel Smelter." In The Minerals, Metals & Materials Series, 271–81. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65647-8_23.

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Phillips, Neil. "Case Study: The Formation of a Giant Goldfield: Kalgoorlie, Western Australia." In Modern Approaches in Solid Earth Sciences, 131–43. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-3081-1_13.

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3

"Interview of Magistrate Gregory Andrew Benn, Regional Magistrate, Kalgoorlie– Boulder." In Trends in the Judiciary, 41–50. Routledge, 2013. http://dx.doi.org/10.1201/b16316-9.

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4

McDivitt, Jordan A., Steffen G. Hagemann, Matthew S. Baggott, and Stuart Perazzo. "Chapter 12: Geologic Setting and Gold Mineralization of the Kalgoorlie Gold Camp, Yilgarn Craton, Western Australia." In Geology of the World’s Major Gold Deposits and Provinces, 251–74. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.12.

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Abstract The Kalgoorlie gold camp in the Yilgarn craton of Western Australia comprises the supergiant Golden Mile and the smaller Mt. Charlotte, Mt. Percy, and Hidden Secret deposits. Since the camp’s discovery in 1893, ~1,950 metric tons (t) of Au have been produced from a total estimated endowment of ~2,300 t. The camp is located within Neoarchean rocks of the Kalgoorlie terrane, within the Eastern Goldfields superterrane of the eastern Yilgarn craton. Gold mineralization is distributed along an 8- × 2-km, NNW-trending corridor, which corresponds to the Boulder Lefroy-Golden Mile fault system. The host stratigraphic sequence, dated at ca. 2710 to 2660 Ma, comprises lower ultramafic and mafic lava flow rocks, and upper felsic to intermediate volcaniclastic, epiclastic, and lava flow rocks intruded by highly differentiated dolerite sills such as the ca. 2685 Ma Golden Mile Dolerite. Multiple sets of NNW-trending, steeply dipping porphyry dikes intruded this sequence from ca. 2675 to 2640 Ma. From ca. 2685 to 2640 Ma, rocks of the Kalgoorlie gold camp were subjected to multiple deformation increments and metamorphism. Early D1 deformation from ca. 2685 to 2675 Ma generated the Golden Mile fault and F1 folds. Prolonged sinistral transpression from ca. 2675 to 2655 Ma produced overprinting, NNW-trending sets of D2-D3 folds and faults. The last deformation stage (D4; &lt; ca. 2650 Ma) is recorded by N- to NNE-trending, dextral faults which offset earlier structures. The main mineralization type in the Golden Mile comprises Fimiston lodes: steeply dipping, WNW- to NNW-striking, gold- and telluride-bearing carbonate-quartz veins with banded, colloform, and crustiform textures surrounded by sericite-carbonate-quartz-pyrite-telluride alteration zones. These lodes were emplaced during the earlier stages of regional sinistral transpression (D2) as Riedel shear-type structures. During a later stage of regional sinistral transpression (D3), exceptionally high grade Oroya-type mineralization developed as shallowly plunging ore shoots with “Green Leader” quartz-sericite-carbonate-pyrite-telluride alteration typified by vanadium-bearing muscovite. In the Hidden Secret orebody, ~3 km north-northwest of the Golden Mile, lode mineralization is a silver-rich variety characterized by increased abundance of hessite and petzite and decreased abundance of calaverite. At the adjacent Mt. Charlotte deposit, the gold-, silver-, and telluride-bearing lodes become subordinate to the Mt. Charlotte-type stockwork veins. The stockwork veins occur as planar, 2- to 50-cm thick, auriferous quartz-carbonate-sulfide veins that define steeply NW- to SE-dipping and shallowly N-dipping sets broadly coeval with D4 deformation. Despite extensive research, there is no consensus on critical features of ore formation in the camp. Models suggest either (1) distinct periods of mineralization over a protracted, ca. 2.68 to 2.64 Ga orogenic history; or (2) broadly synchronous formation of the different types of mineralization at ca. 2.64 Ga. The nature of fluids, metal sources, and mineralizing processes remain debated, with both metamorphic and magmatic models proposed. There is strong evidence for multiple gold mineralization events over the course of the ca. 2.68 to 2.64 orogenic window, differing in genesis and contributions from either magmatic or metamorphic ore-forming processes. However, reconciling these models with field relationships and available geochemical and geochronological constraints remains difficult and is the subject of ongoing research.

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"The Contribution of High Resolution Aeromagnetics to Archean Gold Exploration in the Kalgoorlie Region, Western Australia." In The Geology of Gold Deposits, 389–97. Society of Economic Geologists, 1989. http://dx.doi.org/10.5382/mono.06.30.

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Tripp, Gerard I., Richard M. Tosdal, Thomas Blenkinsop, Jamie R. Rogers, and Scott Halley. "Chapter 33: Neoarchean Eastern Goldfields of Western Australia." In Geology of the World’s Major Gold Deposits and Provinces, 709–34. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.33.

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Abstract Neoarchean greenstone-hosted gold deposits in the Eastern Goldfields Superterrane of the Yilgarn craton of Western Australia are diverse in style, timing with respect to magmatic activity, structural environment, host rocks, and geochemical character. Geologic constraints for the range of gold deposits indicate deposit formation synchronous with volcanism, synchronous with syn- and postvolcanic intrusion, synchronous with postvolcanic deformation in faults and shear zones, or some combination of superposed events over time. The gold deposits are distributed as clusters along linear belt-parallel fault zones internal to greenstone belts but show no association with major terrane boundary faults. World-class gold districts are associated with the thickest, internal parts of the greenstone belts identified by stratigraphic preservation and low metamorphic grades. Ore-proximal faults in those regions are more commonly associated with syn- and postvolcanic structures related to greenstone construction and deformation rather than major terrane amalgamation. Using the Kalgoorlie district as a template, the gold deposits show a predictable regional association with thicker greenstone rocks overlain unconformably by coarse clastic rock sequences in the uppermost units of the greenstone stratigraphy. At a camp scale, major gold deposits show a spatial association with unconformable epiclastic and volcaniclastic rocks located above an unconformity internal to the Black Flag Group. Distinct episodes of gold deposition in coincident locations suggest fundamental crustal structural controls provided by the fault architecture. Late penetrative deformation and metamorphism overprinted the greenstone rocks and the older components of many gold deposits and were accompanied by major gold deposition in late quartz-carbonate veins localized in crustal shear zones or their higher order fault splays.

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Turner, Stephen J., Graeme Reynolds, and Steffen G. Hagemann. "Chapter 13: Boddington: An Enigmatic Giant Archean Gold-Copper (Molybdenum-Silver) Deposit in the Southwest Yilgarn Craton, Western Australia." In Geology of the World’s Major Gold Deposits and Provinces, 275–88. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.13.

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Abstract Boddington is a giant, enigmatic, and atypical Archean Au-Cu deposit hosted in a small, remnant greenstone belt within granite-gneiss and migmatite of the Southwest terrane of the Yilgarn craton, Western Australia. Primary Au and Cu (and Mo) mineralization consists of a network of thin fractures and veins, controlled by shear zones, and dominantly hosted by early dioritic intrusions and their immediate wall rocks, which comprise felsic to intermediate-composition volcanic and volcaniclastic rocks. The pre-~2714 Ma host rocks are typically steeply dipping and strongly deformed, with early ductile and overprinting brittle-ductile fabrics, and have been metamorphosed at mid- to upper greenschist facies. Features consistent with porphyry-style mineralization, classic orogenic shear zones, and intrusion-related Au-Cu-Bi mineralization are all recognized, giving rise to a variety of genetic interpretations. It is clear that Boddington does not fit any classic Archean orogenic gold deposit model, having a general lack of quartz veins and iron carbonate alteration, a Cu (Mo and Bi) association, zoned geochemical anomalism, and evidence of high-temperature, saline ore-forming fluids. Detailed petrographic, geochemical, and melt inclusion studies suggest a late-stage ~2612 Ma, monzogranite intrusion as one of the principal sources of the mineralizing fluids. However, there is also local evidence for older, perhaps protore, porphyry-style Cu (±Au) in the dioritic intrusions and patchy, locally high-grade, orogenic-style gold mineralization associated with enclosing shear zones and brittle-style deformation, which was focused on the relatively competent dioritic intrusions. The relative contributions of metals from these components to the system may not be resolvable. It appears that the Boddington deposit has been a locus for multiple episodes of intrusion, alteration, and mineralization over an extended period of time, as has been demonstrated in a number of other large Canadian and Australian gold deposits, including the Golden Mile near Kalgoorlie.

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Atti di convegni sul tema "Kalgoorlie"

1

Beer, Adam, and Michael Morrongiello. "Wall Optimisation - A Case Study From the Fimiston Open Pit, Kalgoorlie Consolidated Gold Mines." In 2007 International Symposium on Rock Slope Stability in Open Pit Mining and Civil Engineering. Australian Centre for Geomechanics, Perth, 2007. http://dx.doi.org/10.36487/acg_repo/708_26.

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2

Watton, James, and Mark Fowler. "Slope performance monitoring and management of a pit wall experiencing large-scale deformations near Kalgoorlie, Western Australia." In 2020 International Symposium on Slope Stability in Open Pit Mining and Civil Engineering. Australian Centre for Geomechanics, Perth, 2020. http://dx.doi.org/10.36487/acg_repo/2025_58.

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Rapporti di organizzazioni sul tema "Kalgoorlie"

1

Kalgoorlie - Premises Post Office Building 1916 (plate 88). Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_pn-000237.

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2

Commonwealth Bank - Branches - Kalgoorlie - Exterior - November 1922 (plate 285). Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_pn-000241.

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3

Commonwealth Bank - Branches - Kalgoorlie - Interior of premises - c.1922 (plate 284). Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_pn-000242.

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