Дисертації з теми "South Australia Fleurieu Peninsula"
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1
West, Andrew S. "The shore platforms of the Fleurieu Peninsula, South Australia /." Title page, abstract and table of contents only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbw516.pdf.
Повний текст джерела
2
Bickford, Sophia Anastasia. "A historical perspective on recent landscape transformation: integrating palaeoecological, documentary and contemporary evidence for former vegetation patterns and dynamics in the Fleurieu Peninsula, South Australia." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09PH/09phb583.pdf.
Повний текст джерелаАнотація:
Includes bibliographical references (p. 301-319). Palaeoecological records, documented historical records and remnant vegetation were investigated in order to construct a multi-scaled history of vegetation pattern and change in the Fleurieu Peninsula, South Australia over the last c. 8000 years. Aims to better understand post-European landscape transformation and address the inherently historical components of the problems of regional biodiversity loss, land sustainability and the cumulative contribution to global climatic change.
3
Collings, Greg. "Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia /." Title page, table of contents and summary only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09phc711.pdf.
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4
Boord, R. A. "Sedimentology of the Cambrian, Upper Kanmantoo Group, Southern Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09AR/09arb724.pdf.
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5
Stolz, Ned. "A magnetics study of the Brachina Formation on southern Fleurieu Peninsula, South Australia /." Adelaide, 1985. http://web4.library.adelaide.edu.au/theses/09SB/09sbs876.pdf.
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6
Szmidel, Rebekah. "The structural geology of Sellick Hill to Myponga Beach, Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbs998.pdf.
Повний текст джерелаАнотація:
Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1996.National Grid reference (SI-54)6527 - II, (SI-54) 6627 - III 1:10 000 sheet. Includes bibliographical references (leaves 32-39).
7
Crowhurst, Peter V. "The geology, petrology and geochemistry of the Proterozoic Inlier, south of Myponga, Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09SB/09sbc953.pdf.
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8
Barrett, Lyon. "The structural geology of the Rapid Bay-Second Valley area, Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbb274.pdf.
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9
Macdonald, Andrew. "The structural geology of the Yohoe Creek to Cape Jervis area, Fleurieu Peninsula, South Australia /." Title page, contents and introduction only, 1995. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bm1348.pdf.
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10
Kapetas, John. "The structure of the Clarendon - Mt. Bold region : southern Adelaide fold belt, Fleurieu Peninsula, South Australia /." Title page, abstract and contents only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbk17.pdf.
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11
Buhrer, Daniel Anton. "The structure of Myponga River-Carrickalinga Creek area, Southern Adelaide Fold Belt, Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbb931.pdf.
Повний текст джерелаАнотація:
Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1996.National Grid reference (SI 54) 6527-36 ; 44, 45, 36, 37 1:10 000 sheets. Includes bibliographical references.
12
Harvey, Leslie M. "Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09SB/09sbh342.pdf.
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13
Tiver, Fleur. "The vegetation patterns of north-western Eyre Peninsula, South Australia /." Title page, contents and summary only, 1987. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bt623.pdf.
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14
Burn, Nicholas R. "Thermoluminescence studies of a uraniferous tertiary Palaeochannel, Eyre Peninsula, South Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09SB/09sbb963.pdf.
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15
Schaefer, Bruce F. "Insights into protenozoic tectonics from the southern Eyre Peninsula, South Australia /." Title page, contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phs2938.pdf.
Повний текст джерела
16
Hawke, Bruce. "Vegetation analysis with biogeographic implications in North-East Eyre Peninsula, South Australia /." Title page, summary and contents only, 1986. http://web4.library.adelaide.edu.au/theses/09SB/09sbh392.pdf.
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17
Nguyen, Cao Nam. "Farming risks in the Upper Eyre Peninsula : AGRIC 7010 Project C (ANR) (one semester)." Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09AGM/09agmn5764.pdf.
Повний текст джерелаАнотація:
"November 2002." Bibliography: leaves 73-80. Identifies main sources of farming risk in the Upper Eyre Peninsula as climate variability and financial risk. Finds that farmers manage risk by having high equity and off-farm investment, using gross margin analysis, having farm management deposits, diversifying varieties, minimizing tillage, relying on experts for grain marketing and keeping stock for high price periods.
18
Forrest, Catherine A. "Sandstone morphology in the coastal context Talia area, West Coast, Eyre Peninsula, South Australia /." Title page, abstract and contents only, 1993. http://web4.library.adelaide.edu.au/theses/09AR/09arf728.pdf.
Повний текст джерелаАнотація:
Thesis (B.A.(Hons.))--University of Adelaide, Dept. of Geography & Dept. of Geology & Geophysics, 1994.Elliston topographic map, 1982:1:250,000, sheet S1 53-6 Parker, A.J., 1989; Elliston geological map, 1:250,000, sheet S1 53-6 Talia topographic map, 1984, 1:50,000 sheet 5831-2 & PT3. Includes bibliographical references (leaves 36-44).
19
Holloway, Robert E. "Factors affecting the growth of wheat roots in the subsoils of upper Eyre Peninsula, South Australia /." Adelaide : University of Adelaide, 1991. http://web4.library.adelaide.edu.au/theses/09A/09ah745.pdf.
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20
Alexander, Felicity Anne. "Public participation in the marina developments at Port Vincent and Wallaroo on the Yorke Peninsula, South Australia." Title page, table of contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09ENV/09enva375.pdf.
Повний текст джерелаАнотація:
Bibliography: leaves 98-103. Examines the role of public participation in coastal protection and coastal management in two marina developments proposed for Yorke Peninsula. The study concluded that there was potential for the South Australian Planning System to incorporate sustainable development and involve the public to a greater extent. The Environmental Impact Assessment process has been perceived as a means of incorporating the principles of ecologically sustainable development at a community level, but the extent to which this has occured for the marina developments at Port Vincent and Wallaroo is limited.
21
Kerin, Paul D. "A spatial economic analysis of the Eyre Peninsula grain handling and transportation system." Title page, abstract and contents only, 1985. http://web4.library.adelaide.edu.au/theses/09ECM/09ecmk39.pdf.
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22
Menpes, Robert. "Structural evolution of a tanspression zone in the southern Adelaide fold belt, north-east Dudley Peninsula, Kangaroo Island, South Australia /." Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbm547.pdf.
Повний текст джерелаАнотація:
Thesis (B. Sc. (Hons))--University of Adelaide, Dept. of Geology and Geophysics, 1993.On title page: "National Grid reference (51-54) 6526 - III & IV (1:50000). Includes bibliographical references (leaves 39-44).
23
Thiel, Stephan. "Electromagnetic induction studies of the Eyre Peninsula anomaly and their relationship to the tectonics of the Southern Gawler Craton, South Australia /." Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SB/09sbt399.pdf.
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24
Pembshaw, John Michael Heynes. "Aboriginal morbidity, Yorke Peninsula : a study of Aboriginal morbidity for the period 1 July 1976 to 30 June 1986 based on the patient registers of the Maitland Hospital, South Australia /." Title page, contents and abstract only, 1986. http://web4.library.adelaide.edu.au/theses/09AR/09arp394.pdf.
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25
Bickford, Sophia Anastasia. "A historical perspective on recent landscape transformation: integrating palaeoecological, documentary and contemporary evidence for former vegetation patterns and dynamics in the Fleurieu Peninsula, South Australia / Sophia Anastasia Bickford." Thesis, 2001. http://hdl.handle.net/2440/21741.
Повний текст джерелаАнотація:
Includes bibliographical references (p. 301-319).xx, 319, [30] leaves : ill. (some col.), maps ; 30 cm.
Palaeoecological records, documented historical records and remnant vegetation were investigated in order to construct a multi-scaled history of vegetation pattern and change in the Fleurieu Peninsula, South Australia over the last c. 8000 years. Aims to better understand post-European landscape transformation and address the inherently historical components of the problems of regional biodiversity loss, land sustainability and the cumulative contribution to global climatic change.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geographical and Environmental Studies, 2001
26
Collings, Gregory James. "Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia / by Gregory James Collings." Thesis, 1996. http://hdl.handle.net/2440/18910.
Повний текст джерелаАнотація:
Bibliography: leaves 191-225.2 v. : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
The temporal dynamics of eight subtidal mixed macroalgal communities were quantified. The results were discussed in terms of the implications for sampling programs in the future and the reliability of previous work.
Thesis (Ph.D.)--University of Adelaide, Dept. of Botany, 1997?
27
Collings, Gregory James. "Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia / by Gregory James Collings." 1996. http://hdl.handle.net/2440/18910.
Повний текст джерелаАнотація:
Bibliography: leaves 191-225.2 v. : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
The temporal dynamics of eight subtidal mixed macroalgal communities were quantified. The results were discussed in terms of the implications for sampling programs in the future and the reliability of previous work.
Thesis (Ph.D.)--University of Adelaide, Dept. of Botany, 1997?
28
Barrett, L. "The structural geology of the Rapid BaySecond Valley area, Fleurieu Peninsula, South Australia." Thesis, 1995. http://hdl.handle.net/2440/128629.
Повний текст джерелаАнотація:
This item is only available electronically.Whilst the geology of the Rapid Bay-Second Valley area is known to be both structurally and stratigraphically complex, previous workers (Daily, 1963; Evans 1987; Drayton, 1963; Campana and Wilson, 1955) have been unable to agree on many aspects of the area. Neoproterozoic and Cambrian aged sediments were first deposited in an extensional basin, which was formed due to lithospheric thinning, and associated subsidence (Jenkins, 1986, 1990). These rocks have then been subjected to at least one phase of deformation, the Cambro-Ordovician Delamerian Orogeny (Offler & Fleming, 1968; Thompson, 1970). Listric extensional faults were formed both before and during sedimentation of the rocks, which has created narrow zones of weakness that the subsequent compressional event has exploited, creating thrust faults (Flottman et al., 1994). Structural mapping of the area has revealed that it is transected by two thrust faults and is intensely folded in places. Structural data has been collected during eight weeks of field work and has been compiled into a 1:10 000-scale geological map which accurately represents the area. A computer-generated three-dimensional model has been created for the area, based on this map, and cross and profile sections constructed from the data collected. The model was constructed using Vulcan™ software. Strain analysis has also been conducted on many of the folds in the area.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1995
29
Crowhurst, P. V. "The geology, petrology and geochemistry of the Proterozoic inlier, south of Myponga, Fleurieu Peninsula, South Australia." Thesis, 1988. http://hdl.handle.net/2440/119710.
Повний текст джерелаАнотація:
This item is only available electronically.The study area is located within the Yankalilla-Myponga Proterozoic lnlier, approximately 60km south of Adelaide. The basement rocks are comprised of a mixture of metasediments and intrusives. The metasediments predominantly comprise of quartz-biotite gneisses and schists. They are intruded by basic dykes, pegmatites and an aplite/microgranite. The basic dykes have oceanic basalt affinities and could originally have been formed during an 'aborted rifting' event, but the more felsic rocks are more likely to lie within plate granites. The origin of the 'Houghton' granulite is difficult to ascertain, because it has a varied internal composition and is closely comparable to a diorite and a shale. The basement inlier rocks are found within the overlying unconformable upper Proterozoic Adelaidean System. They have undergone at least four phases of deformation and metamorphism. Mineral assemblages found in the rocks indicate metamorphism reached at least upper amphibolite facies. The maximum pressure and temperature conditions were calculated from microprobe data. They range from 8-10 kb at 550 -650 C. U-Pb isochron dating was performed on the aplite/microgranite of the area and was found to be 1578+\-22Ma ,which places a minimum age on the inlier rocks. This date obtained and the deformation processes recognized are comparable to other basement rocks in South Australia; noticeably the Gaw1er Craton and the Olary Province. This may indicate a homogeneous terrain once spanned most of South Australia during the lower Proterozoic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1988
30
Harvey, L. M. "Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia." Thesis, 1989. http://hdl.handle.net/2440/119293.
Повний текст джерелаАнотація:
This item is only available electronically.A N-E striking elongate aeromagnetic anomaly is observed over the Talisker Mine area, on the southern Fleurieu Peninsula, which has character and amplitude similar to an anomaly observed at Delamere (several kilometres to the north) found to be caused by magnetic Brachina Formation. Geological and geophysical techniques have been used to determine if the rock type at Talisker is also magnetic Brachina Formation, why there is a gap between the two anomalies, and why the anomaly at Talisker ends near the south coast. Geological mapping, microscopy and petrologic studies have been used in conjunction with local ground magnetic surveys and modelling procedures, to reveal magnetic Brachina Formation as the cause of the anomaly at Talisker. Mapping has shown the anomaly to be the result of a sliver of magnetic Brachina Formation caught up within a local zone of intense deformation that extends for at least 1500m across strike, and which outcrops on the coast. The Brachina Formation is sheared out against Cambrian Backstairs Passage Formation to the south, forming the southern end to the anomaly. To the north, the Brachina Formation suffered deeper erosion during Permian times, and is covered by a greater thickness of non-magnetic cover which causes the apparent gap in the aeromagnetic anomaly.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1989
31
Loader, L. "The Eyre Peninsula conductivity anomaly, South Australia." Thesis, 2018. http://hdl.handle.net/2440/130629.
Повний текст джерелаАнотація:
This item is only available electronically.A major electrically conducting structure has been spatially located in the southern Eyre Peninsula, South Australia. The structure extends from the continental margin inland along the eastern margin of the Eyre Peninsula, trending north-northeast for approximately 150 km. In order to provide a two-dimensional image of the crust orthogonal to the conductor’s strike, 39 broadband (1000 to 0.01 Hz) magnetotelluric sites were collected with approximately 2 km separation across the peninsula. A smoothed 2-D inversion model demonstrated that the conductor appears centred beneath a topographic high, structurally bound at the east by the transpressional Kalinjala Shear Zone and resistive Donington Suite granitoids, and the Sleaford Complex to the west. The main features from modelling are: (i) east of the Kalinjala Shear Zone, a region of high resistivity (> 1000 ohm/m) relates to the Donington Suite granitoids; (ii) the late Archaean Sleaford Complex (2480–2420 Ma) bordering the Donington Suite granitoids features a lower, wider resistivity range between 5 to < 600 ohm/m, and is near-vertical in the top 12 km; (iii) the lowest resistivity structure of < 0.1 ohm/m occurs at a depth of 5-10 km, and appears to terminate at a depth of ~15 km; (iv) the low resistivity structure correlates with banded iron formations and is credibly the result of biogenically deposited graphite in marine sediments, which migrated to become concentrated in fold hinges during the Kimban Orogeny; and (iv) the conductor is co-located with a ridge of high gravity (+ 200 to 500 mGals). The origin of this high gravity may be due to a mafic intrusive block of oceanic crust, compressed during the continental collision of the Kimban Orogeny. Utilising the constraints of the 2-D model, a regional 3-D forward model was developed which shows agreement with compiled legacy data sets.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
32
Carne, Vanessa Lynne. "Ecology of Mediterranean snails in Southern Australian agriculture : a study of Cernuella virgata and Cochlicella acuta on the Yorke Peninsula / Vanessa L. Carne." 2003. http://hdl.handle.net/2440/22109.
Повний текст джерелаАнотація:
"August 2003."Includes bibliographical references (leaves 294-333)
2 v. (xxxi, 333 leaves) ; ill. (some col.) ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, School of Agriculture and Wine, Discipline of Plant and Pest Science, 2005
33
Clough, Angela. "Nitrogen and carbon mineralisation in agricultural soils of South Australia / by Angela Clough." 2001. http://hdl.handle.net/2440/22426.
Повний текст джерелаАнотація:
"September 2001"Bibliography: leaves 144-159.
xix, 159 leaves : ill. ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
The two main aims of this study were: 1) to determine if the presence of Calcium carbonate in soil was the reason behind soils from Yorke Peninsula having relatively high OC (organic carbon) contents, given local farming practices, and 2) to determine the effect that the composition of the soils' OC has on the mineralisation rates.
Thesis (Ph.D.)--University of Adelaide, Dept. of Agronomy and Farming Systems, 2002
34
Schaefer, Bruce F. "Insights into proterozoic tectonics from the southern Eyre Peninsula, South Australia / Bruce F. Schaefer." Thesis, 1998. http://hdl.handle.net/2440/19291.
Повний текст джерелаАнотація:
Copies of author's previously published articles inserted.Includes bibliographical references (6 leaves)
xi, 131, [71] leaves : ill., maps ; 30 cm.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1999
35
Wolff, Keryn Dianne. "Regional Carbonate Geochemistry and Biogeochemistry for Cu Exploration on the Yorke Peninsula, South Australia." Thesis, 2018. http://hdl.handle.net/2440/120233.
Повний текст джерелаАнотація:
This thesis describes the geochemistry from carbonate rocks and biogeochemistry from mallee across the Yorke Peninsula to better characterise and define mineral systems that may occur in IOCG prospective basement rocks masked by various overlying cover sequences. Presented here is geochemical data from three cliff escarpments (vertical geochemical profiles) which preserve cover sequences overlying basement rocks. Ca/Sr ratios were found to be a defining discriminator between marine and pedogenic carbonate rocks within the profiles; pedogenic carbonates have Ca/Sr ratios less than 650 and marine carbonates have Ca/Sr ratios greater than 1260. This simple discriminant can also be used to identify samples appropriate for carbonate sampling in mineral exploration, particularly in drill cuttings, as well as retrospective filtering of multi-element geochemical exploration data sets. A regional sampling program was undertaken in the context of the regolith landform setting from a newly constructed map of Yorke Peninsula. The majority of carbonate material occurring at the surface across the Yorke Peninsula has Ca/Sr <650, with lesser occurrences of carbonate preserving Ca/Sr ratios between 650 and 1260 and one preserving marine Ca/Sr >1260. The majority of surface carbonates have Ca/Sr consistent with a mixture of rainfall sources and marine carbonate sources. With the dominant contributor of Ca and Sr from rainwater. Surface carbonates with Ca/Sr ratios >650 have a greater proportion of Ca and Sr sourced from marine carbonates, incorporated either from wind-blown dust or from in-situ marine carbonates. The systematically lower Ca/Sr of rainwater, compared to marine carbonates, translates into systematically lower Ca/Sr in pedogenic compared to marine carbonates. This is an effective discriminator of carbonates formed by pedogenic processes and weathered marine carbonates. The dominantly pedogenic nature of the carbonate rocks sampled across the Yorke Peninsula means that they are appropriate for use in mineral exploration geochemistry for underlying iron oxide-copper-gold deposits. The range of the Cu values in the carbonate rocks is 1.4–36ppm. Elevated Cu concentrations (1.4–36ppm) occur more commonly within carbonate rocks within 3km of known Cu occurrences. . Eucalyptus foliage was collected at a suitable time of year to maximise root absorption and minimise contamination from farming practices. The range of Cu concentrations within Eucalyptus with mallee-form was 1.6–10ppm. Mallee within 3km of known mineralisation has a concentration of 2–10ppm Cu. There was little statistical difference between the four mallee species sampled so that it is reasonable to use all data as a collective dataset. As mallee occur across a large portion of southern Australia, this method of sampling could prove to be a useful tool for frontiers in exploration where tenure occurs typically over large areas, with widespread cover and restricted access due to environmental and cultural sensitivities.Thesis (Ph.D.) -- University of Adelaide, School of Physical Sciences, 2019
36
Mills, David (Peter David Duncombe). "The role of goal setting in the diabetes case management of Aboriginal and non-Aboriginal populations in rural South Australia / David Mills." Thesis, 2005. http://hdl.handle.net/2440/38374.
Повний текст джерелаАнотація:
Includes publications published as a result of ideas developed in this thesis, inserted at end.Includes bibliographical references (leaves 210-242)
242 leaves
Examines goal setting in people with diabetes as part of chronic disease management in a rural setting. The studies were performed in Eyre Peninsula with a significant (10-20%) Aboriginal population.
Thesis (M.D.) -- University of Adelaide, Dept. of General Practice, 2005
37
Mills, David (Peter David Duncombe). "The role of goal setting in the diabetes case management of aboriginal and non-aboriginal populations in rural South Australia / David Mills." 2005. http://hdl.handle.net/2440/38374.
Повний текст джерелаАнотація:
Includes publications published as a result of ideas developed in this thesis, inserted at end."April 2005"
Includes bibliographical references (leaves 210-242)
242 leaves :
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Examines goal setting in people with diabetes as part of chronic disease management in a rural setting. The studies were performed in Eyre Peninsula with a significant (10-20%) Aboriginal population.
Thesis (M.D.)--University of Adelaide, Dept. of General Practice, 2005
38
Adcock, Damien Paul. "Soil water and nitrogen dynamics of farming systems on the upper Eyre Peninsula, South Australia." Thesis, 2005. http://hdl.handle.net/2440/37810.
Повний текст джерелаАнотація:
In the semi - arid Mediterranean - type environments of southern Australia, soil
and water resources largely determine crop productivity and ultimately the sustainability of farming systems within the region. The development of sustainable farming systems is a constantly evolving process, of which cropping
sequences ( rotations ) are an essential component. This thesis focused on two important soil resources, soil water and nitrogen, and studied the effects of different crop sequences on the dynamic of these resources within current farming systems practiced on the upper Eyre Peninsula of South Australia.
The hypothesis tested was that : continuous cropping may alter N dynamics but will not necessarily alter water use efficiency in semi - arid Mediterranean - type environments. Continuous cropping altered N - dynamics ; increases in inorganic N were dependent on the inclusion of a legume in the cropping sequence.
Associated with the increase in inorganic N supply was a decrease in WUE by the subsequent wheat crop. Overall, estimates of water use efficiency, a common index of the sustainability of farming systems, in this study concur with reported values for the semi - arid Murray - Mallee region of southern Australia and other
semi - arid environments worldwide.
Soil water balance and determination of WUE for a series of crop sequences in this thesis suggests that the adoption of continuous cropping may increase WUE and confer a yield benefit compared to crop sequences including a legume component in this environment. No differences in total water use ( ET ) at anthesis or maturity were measured for wheat regardless of the previous crop. Soil evaporation ( E [subscript s] ) was significantly affected by crop canopy development, measured as LAI from tillering until anthesis in 2002, however total seasonal E [subscript s] did not differ between crop sequences. Indeed in environments with infrequent
rainfall, such as the upper Eyre Peninsula, soil evaporation may be water - limited rather than energy limited and the potential benefits from greater LAI and reduced E [subscript s] are less.
Greater shoot dry matter production and LAI due to an enhanced inorganic N supply for wheat after legumes, and to a lesser degree wheat after canola, relative to continuous cereal crop sequences resulted in increases in WUE calculated at anthesis, as reported by others. Nonetheless the increase in WUE was not sustained due to limitations on available soil water capacity caused by soil physical and chemical constraints. Access to more soil water at depth ( > 0.8m ) through additional root growth was unavailable due to soil chemical limitations. More importantly, the amount of plant available water within the ' effective rooting depth ' ( 0 - 0.8m ) was significantly reduced when soil physical factors were accounted for using the integral water capacity ( IWC ) concept. The difference between the magnitude of the plant available water capacity and the integral water capacity was approximately 90mm within the ' effective rooting depth ' when measured at field capacity, suggesting that the ability of the soil to store water and buffer against periodic water deficit was severely limited. The IWC concept offers a method of evaluating the physical quality of soils and the limitations that these physical properties, viz. aeration, soil strength and hydraulic conductivity, impose on the water supply capacity of the soil.
The inability of the soil to maintain a constant supply of water to satisfy maximal transpiration efficiency combined with large amounts of N resulted in ' haying off ', and reduced grain yields. A strong negative linear relationship was established between WUE of grain production by wheat and increasing soil NO₃ - N at sowing in 2000 and 2002, which conflicts with results from experiments in
semi - arid Mediterranean climates in other regions of the world where applications of N increased water use efficiency of grain.
Estimates of proportional dependence on N₂ fixation ( % N [subscript dfa] ) for annual medics and vetch from this study ( 43 - 80 % ) are comparable to others for environments in southern Australia ( < 450mm average annual rainfall ). Such
estimates of fixation are considered low ( < 65 % ) to adequate ( 65 - 80 % ). Nevertheless, the amount of plant available N present at sowing for subsequent
wheat crops, and the occurrence of ' haying off ', suggests that WUE is not N - limited
per se, as implied by some reports, but constrained by the capacity of a soil to balance the co - limiting factors of water and nitrogen.Thesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2005.
39
Adcock, Damien Paul. "Soil water and nitrogen dynamics of farming systems on the upper Eyre Peninsula, South Australia." 2005. http://hdl.handle.net/2440/37810.
Повний текст джерелаАнотація:
In the semi - arid Mediterranean - type environments of southern Australia, soil and water resources largely determine crop productivity and ultimately the sustainability of farming systems within the region. The development of sustainable farming systems is a constantly evolving process, of which cropping sequences ( rotations ) are an essential component. This thesis focused on two important soil resources, soil water and nitrogen, and studied the effects of different crop sequences on the dynamic of these resources within current farming systems practiced on the upper Eyre Peninsula of South Australia. The hypothesis tested was that : continuous cropping may alter N dynamics but will not necessarily alter water use efficiency in semi - arid Mediterranean - type environments. Continuous cropping altered N - dynamics ; increases in inorganic N were dependent on the inclusion of a legume in the cropping sequence. Associated with the increase in inorganic N supply was a decrease in WUE by the subsequent wheat crop. Overall, estimates of water use efficiency, a common index of the sustainability of farming systems, in this study concur with reported values for the semi - arid Murray - Mallee region of southern Australia and other semi - arid environments worldwide. Soil water balance and determination of WUE for a series of crop sequences in this thesis suggests that the adoption of continuous cropping may increase WUE and confer a yield benefit compared to crop sequences including a legume component in this environment. No differences in total water use ( ET ) at anthesis or maturity were measured for wheat regardless of the previous crop. Soil evaporation ( E [subscript s] ) was significantly affected by crop canopy development, measured as LAI from tillering until anthesis in 2002, however total seasonal E [subscript s] did not differ between crop sequences. Indeed in environments with infrequent rainfall, such as the upper Eyre Peninsula, soil evaporation may be water - limited rather than energy limited and the potential benefits from greater LAI and reduced E [subscript s] are less. Greater shoot dry matter production and LAI due to an enhanced inorganic N supply for wheat after legumes, and to a lesser degree wheat after canola, relative to continuous cereal crop sequences resulted in increases in WUE calculated at anthesis, as reported by others. Nonetheless the increase in WUE was not sustained due to limitations on available soil water capacity caused by soil physical and chemical constraints. Access to more soil water at depth ( > 0.8m ) through additional root growth was unavailable due to soil chemical limitations. More importantly, the amount of plant available water within the ' effective rooting depth ' ( 0 - 0.8m ) was significantly reduced when soil physical factors were accounted for using the integral water capacity ( IWC ) concept. The difference between the magnitude of the plant available water capacity and the integral water capacity was approximately 90mm within the ' effective rooting depth ' when measured at field capacity, suggesting that the ability of the soil to store water and buffer against periodic water deficit was severely limited. The IWC concept offers a method of evaluating the physical quality of soils and the limitations that these physical properties, viz. aeration, soil strength and hydraulic conductivity, impose on the water supply capacity of the soil. The inability of the soil to maintain a constant supply of water to satisfy maximal transpiration efficiency combined with large amounts of N resulted in ' haying off ', and reduced grain yields. A strong negative linear relationship was established between WUE of grain production by wheat and increasing soil NO [subscript 3] - N at sowing in 2000 and 2002, which conflicts with results from experiments in semi - arid Mediterranean climates in other regions of the world where applications of N increased water use efficiency of grain. Estimates of proportional dependence on N [subscript 2] fixation ( % N [subscript dfa] ) for annual medics and vetch from this study ( 43 - 80 % ) are comparable to others for environments in southern Australia ( < 450mm average annual rainfall ). Such estimates of fixation are considered low ( < 65 % ) to adequate ( 65 - 80 % ). Nevertheless, the amount of plant available N present at sowing for subsequent wheat crops, and the occurrence of ' haying off ', suggests that WUE is not N - limited per se, as implied by some reports, but constrained by the capacity of a soil to balance the co - limiting factors of water and nitrogen.Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2005.
40
Nicholson, Ann Florence. "Archaeology on an arid coast : environmental and cultural influences on subsistence economies on the West Coast of South Australia." Master's thesis, 1994. http://hdl.handle.net/1885/109999.
Повний текст джерелаАнотація:
This thesis examines the archaeological record on the West Coast of the Eyre Peninsula in
South Australia with a view to identifying the pattern of behaviour associated with sites
present on this coast. The sites are notable in that they are extensive and feature high
proportions of stone artefacts but contain little or no shell material. This thesis seeks to
explain the virtual absence of shells by considering a number of environmental, behavioural,
demographic and cultural issues. Is the archaeological record a product of post-depositional
disturbance or resource availability, or did other environmental influences such as a shortage
of water restrict adaptive behaviour so as to exclude or minimize interaction with the sea.
Alternatively, is the subsistance strategy indicated by the archaeological record a result of
other cultural influences. Ethnohistorical evidence is examined to investigate the subsistence
patterns which operated on this coastline. Linguistic, technological and social factors which
may have influenced the economic choices made by these coastal people are considered and
compared with the archaeological record. The thesis then examines the interpretation of the
West Coast evidence in the context of other coastal studies both in Australia and overseas to
contribute to the current debate regarding the role of the sea in the evolution of hunter-gatherer
subsistence economies.
41
Atkinson, Victoria. "Mine and industrial site revegetation in the semi-arid zone, North-Eastern Eyre Peninsula, South Australia." 2005. http://arrow.unisa.edu.au:8081/1959.8/46701.
Повний текст джерелаАнотація:
This research aims to develop the present knowledge of arid zone rehabilitation by scientifically testing topsoiling and seeding treatments on the Eyre Peninsula, South Australia, in a way that enables the widest application and comparison to other mining leases throughout the arid lands.
42
Kontonikas-Charos, A. "Albitization and REE-U-enrichment in IOCG systems: insights from Moonta-Wallaroo, Yorke Peninsula, South Australia." Thesis, 2013. http://hdl.handle.net/2440/106289.
Повний текст джерелаАнотація:
This item is only available electronically.Iron Oxide Copper Gold (IOCG) deposits are the products of crustal-scale metasomatic alteration, generally considered to be associated with the emplacement of large felsic intrusions. These systems are typified by zoned, broad alteration haloes comprising the products of an early, barren albitization event, and late, ore-hosting potassic/calcic (skarn) alteration associated with mineralization. Yttrium and rare earth elements (REY), and also uranium, are prominent components of most IOCG systems. The REY-signatures of feldspars and accessory apatite, Fe-(Ti)-oxides and other minerals are geochemical tracers of alteration stages within a magmatic-hydrothermal system. This study sets out to identify links between magmatism and initiation of hydrothermal activity, and to test the hypothesis that albitization is a pre-requisite stage for REE-U enrichment in magmatically-derived IOCG systems. The compositions and trace element concentrations in key minerals have been analysed using scanning electron microscopy, electron probe microanalysis and laser-ablation inductively-coupled plasma mass spectrometry in a varied range of magmatic to metasedimentary lithologies from the Moonta-Wallaroo region, an area in which broad regional-scale alkali alteration is recognised. Results confirm a strong link between albitization and REE-U-enrichment. The process of albitization is seen to consume, redistribute and lock-in REY, LILE and HFSE via complex fluid-rock reactions dependent on the pre-existing mineral assemblages and fluid characteristics, providing a holistic model for IOCG-driven alkali metasomatism. The trace element signatures recorded by K-feldspar reflect a transition from magmatic to hydrothermal stages within an evolving IOCG system. Although further constraints on these signatures are required, they could prove invaluable in mineral exploration as they suggest a quantifiable distinction between alteration associated with mineralization, and regional background. This hypothesis requires testing elsewhere in the Olympic Province and in analogous terranes.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
43
Thomas, L. M. "Regolith-landforms and plant biogeochemical expression of buried mineralisation targets in the northern Middleback Ranges, (“Iron Knob South”) South Australia." Thesis, 2011. http://hdl.handle.net/2440/97938.
Повний текст джерелаАнотація:
This item is only available electronically.South of the town Iron Knob on the northern Eyre Peninsula, a tenement scale plant biogeochemical survey and regolith-landform mapping, combined to define areas with elevated Cu, Zn and Au contents that are worthy of follow-up exploration. Plant biogeochemistry was conducted within a 6 Km2 area with 1 Km spacing between each E-W trending transect and 200 m spacing between each sample. A regolith-landform map presents the distribution of regolith materials and associated landscape processes to help constrain geochemical dispersion. A Philips XL30 SEM provided insight into how the plants uptake certain elements and distribute them within the organs structure. Two zones of elevated trace metals (e.g. Cu, Au and Zn) were defined either side of a NW-SE structure crossing over the N-S trending “Katunga‟ ridge. Both targets were located on similar regolith-landform units of sheet-flood fans and alluvial plains. Copper and Zn results were best represented by the western myall species while the bluebush species was best at detecting Au. A follow up study targeting the NW-SE structure with closer sample spacing is recommended in further constraining drilling targets. For the tenement holding company, Onesteel Ltd, these results are significant as they define two new areas of interest for possible IOCG mineralisation. For research purposes the results confirm that plant biogeochemistry can be used as an effective tool for detecting mineralisation along buried structures providing the use of the right species in the area.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
44
Roache, MW. "The geology, timing of mineralisation, and genesis of the Menninnie Dam Zn-Pb-Ag deposit, Eyre Peninsula, South Australia." Thesis, 1998. https://eprints.utas.edu.au/14507/13/Roache_whole_thesis.pdf.
Повний текст джерелаАнотація:
The Menninnie Dam Pb - Zn - Ag deposit is located on the northern Eyre Peninsula of South Australia, approximately 1-2 km south of the main mass of the Gawler Range Volcanics. The deposit has no surface expression and was located by drilling of aeromagnetic anomalies in deeply weathered, flat lying terrain. Mineralisation occurs over ≈ 3 km strike and is hosted by upper amphibolite facies (≈ 700°C and 7 kbars) marbles and diopside-rich calc-silicate lithologies, correlated with the Katunga Dolomite and lower units of the Cook Gap Schist of the Middleback Subgroup, a subdivision of the Hutchison Group (1964- 1845 Ma.). The Katunga Dolomite is bound to the west by a shear zone(> 50 m wide) formed during the latter stages of the Kimban Orogeny (1740- 1710 Ma.). Syn-deformation granite dykes intruded into the shear zone, and, to a lesser extent, into the Katunga Dolomite and Cook Gap Schist. Late tectonic pegmatite dykes intruded into the Katunga Dolomite and lower units of the Cook Gap Schist, where they produced zones of K-feldspar- calc-silicate metasomatism.
Previous researchers have incorrectly suggested that the Menninnie Dam Pb - Zn - Ag deposit is a Broken Hill-type. However, Pb - Zn - Ag mineralisation post-dates metamorphism, deformation and metasomatism and has replaced the host marble, and to a lesser extent, diopside-rich calc-silicate lithologies. On the basis of lithologic relationships, most mineralisation formed within 100 - 600m of the palaeosurface, and resulted in a central zone of stockwork and matrix to marble and calc-silicate breccias, flanked by veins. Sulphide and gangue minerals consist of a simple assemblage of pyrite, quartz, sphalerite, galena and CaMn-Mg-Fe carbonate, with accessory chalcopyrite, chlorite, adularia, sericite, fluorite, rhodonite, talc, phlogopite, dolomite, hematite and matildite. Three paragenetic stages of mineralisation are present with an early pyrite stage, followed by a sphalerite galena, and late pyrite stages. Metal abundances have a bell-shaped distribution along the length of the deposit and the highest values are associated with the zone of stockwork and breccia mineralisation.
Post metamorphic, porphyritic rhyolite intruded the Hutchison Group, and interacted with (heated?) groundwater resulting in explosive fragmentation of the host rocks and formation of polymictic breccia pipes. Some of these erupted onto the palaeosurface and formed layered polymictic breccias. Rhyolite continued to intrude through polymictic breccia pipes, and resulted in formation of peperite at the margins. Some rhyolite intrusions erupted onto the palaeosurface and formed volcanic breccias and rhyolite lavas. Polymictic breccias contain clasts of paragenetically early sulphide and gangue minerals, and have an altered matrix that includes paragenetically late sulphide minerals, indicative of syn-mineralisation emplacement. U-Pb zircon dating of the rhyolite intrusions constrains the timing of mineralisation to 1594 ± 7 Ma. which is indistinguishable from that determined for the Hiltaba Suite granitoids and comagmatic Gawler Range Volcanics.
Modelling of regional gravity and aeromagnetic data indicates the Menninnie Dam deposit lies near the north-western margin of a ≈ 20 km diameter Hiltaba Suite granite that intruded to within I - 3 km of the palaeo-surface. Lead was derived from the underlying Hiltaba Suite granite and leached from Cook Gap Schist. Lead isotope ratios have a spatial distribution on a prospect scale, and the least radiogenic ratios correspond with the highest metal values and the central zone of stockwork and breccia style mineralisation, consistent with a single zone of fluid up-flow. Carbonate gangue is interpreted to have precipitated via interaction of the mineralising fluid (δ\(^{18}\)O = -2.0‰; δ\(^{13}\)C = -6.9‰) in equilibrium with H\(_2\)CO\(_3\)\(_{(aq)}\) (> 0.01 molal) and the host marbles (δ\(^{18}\)O = 15.5 to 21.09‰; δ\(^{13}\)C = -1.1 to 1.6‰) between 200° and 125°C. Hydrous phyllosilicates associated with mineralisation have calculated fluid values of δ\(^{18}\)O = -0.7 to -2.0‰ and δD = -43 to -48‰, indicative of a mixed meteoric - magmatic origin for the mineralising fluids. Sulphide δ\(^{34}\)S values range from -3.0 to 8.2‰, with most between 4 to 6‰. The lack of evidence for sulphur isotope fractionation between different sulphide minerals is consistent with non-equilibrium precipitation of sulphides from a reduced fluid, low temperature kinetic effects and / or a H\(_2\)S : metal ratio ≥ 1. Sulphur was sourced from either the magma, the country rocks, or a combination of both.
Primary fluid inclusions hosted by sphalerite and quartz have a range of trapping temperatures and salinities interpreted to have resulted from mixing of ≈ 140°C and =27 wt.% NaCI equivalent Na-Ca-K-Cl brine with a ≈ 180°C dilute chloride water. Thermodynamic modelling has shown that sufficient concentrations of Pb and Zn (> 1 ppm) can be transported together with reduced sulphur ∑S = 0.002 molal) in a low temperature (150°C) saline brine (≈ 6 molal) to form the Menninnie Dam deposit. The physiochemical attributes of the mineralising fluid at 150°C are estimated to have been log \(f\)O\(_2\) = -46 and pH= 4.6. Dilution through mixing with heated groundwater was a possible base metal depositional mechanism but is predicted to have been less effective than the pH increase that resulted from dissolution of the host marbles.
Soon after cessation of the mineralising event, the stratigraphy was mantled by a single cooling unit> 260m thick of lithic-rich ( ≈ 45% and up to 20m across) welded ignimbrite (MD ignimbrite). The thickness, abundance and size of lithic clasts in the MD ignimbrite, and shallow intrusion of granite are consistent with an intracaldera setting. Following welding and cooling of the MD ignimbrite, the lower part of the MD ignimbrite and the Hutchison Group near the southern end of the Menninnie Dam deposit were partially altered to a texturally destructive quartz - chlorite - carbonate - calc-silicate assemblage by a hot, low salinity water (190- 356°C and 0- 3 wt. % NaCI equiv.). Carbon, hydrogen, and oxygen isotopes are consistent with a meteoric water that had undergone partial isotopic exchange with igneous rocks. Mineral textures, whole rock geochemistry, lead and sulphur isotope data are consistent with the Menninnie Dam Pb- Zn- Ag mineralisation being partially dissolved and reprecipitated by this event, with no addition of metals or sulphur.
45
Brotodewo, A. "Constraints on Mesoproterozoic magmatism and deformation in the southern Gawler Craton, South Australia: magmatism and deformation in Yorke Peninsula." Thesis, 2016. http://hdl.handle.net/2440/120548.
Повний текст джерелаАнотація:
This item is only available electronically.The ca. 1600–1580 Ma time slice is recognised as a significant period of magmatism and deformation throughout eastern Proterozoic Australia. Within the northern Yorke Peninsula, this period was associated with the emplacement of multiple phases of the Tickera Granite; an intensely foliated orange granite, a white leucogranite and a red granite. These granites belong to the broader Hiltaba Suite that was emplaced at shallow crustal levels, throughout the Gawler Craton. Geochemical and isotopic analysis suggests these granite phases were derived from a heterogeneous source region. The orange and red granites were derived from the Donington Suite and/or the Wallaroo Group metasediments with slight contamination from an Archean basement. The white leucogranite is sourced from a similar but slightly more mafic/lower crustal source. Phases of the Tickera Granite were emplaced synchronously with deformation that resulted in development of a prominent northeast trending structural grain throughout the Yorke Peninsula region. This fabric is a composite of two fold generations; early isoclinal folds that were refolded by later open upright folds. Isoclinal folding may have occurred during the ca. 1730–1690 Ma Kimban Orogeny, or just prior to emplacement of the Tickera Granite at ca. 1597–1577 Ma. The upright fold generation was contemporaneous with the emplacement of the Tickera Granite. The Yorke Peninsula shares a common geological history with the Curnamona Province, which was deformed during the ca. 1600–1585 Ma Olarian Orogeny, and resulted in development of early isoclinal (recumbent) folds overprinted by an upright fold generation, a dominant northeast–trending structural grain and spatially and temporally related intrusions. This suggests an apparent correlation with the geological history of the Curnamona Province, and that the Olarian Orogeny may have also affected the southeastern Gawler Craton. Constraint on the timing of the earlier isoclinal fold generation in the Yorke Peninsula will allow further understanding of the similarities between the two regions.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
46
Ismail, Roniza. "Spatial-temporal evolution of skarn alteration in IOCG systems: evidence from petrography, mineral trace element signatures and fluid inclusion studies at Hillside, Yorke Peninsula, South Australia." Thesis, 2016. http://hdl.handle.net/2440/112582.
Повний текст джерелаАнотація:
Hillside is a newly-discovered, undeveloped copper resource related to Mesoproterozoic Hiltaba Suite intrusives along the crustal-scale Pine Point fault on the eastern margin of the Yorke Peninsula, South Australia. Mineralogical and petrographic study was undertaken on ~100 samples representative of all lithologies, parts of the deposit, and evolution from magmatic through prograde and retrograde skarn to late-stage hydrothermal overprint. Emphasis was placed on distributions of REE+Y and other trace elements in main minerals, and on the constraints these patterns provide for processes associated with alteration and mineralization. Alteration at Hillside is defined by diverse skarn assemblages. Most are readily interpreted as exoskarns formed onto (Moonta-Wallaroo Group) sedimentary protoliths. Two granitoids and associated pegmatites are indicative of composite (multiphase?) felsic magmatism. Granitoid emplacement and alkali-metasomatism pre-date skarn formation; the same initial alteration is recorded in coeval gabbros. The main prograde and retrograde associations [garnetite, garnet-(epidote-allanite-(Ce)) skarn, garnet-feldspar skarn and (pyroxenedominant) multi-component skarn] are defined by mineral associations and replacement relationships among calc-silicates and replacement of calc-silicates by secondary calcite±quartz±chlorite assemblages. Andradite-dominant garnet and diopside-dominant pyroxene are prograde minerals in this (magnetite-pyrite stable) association. Clinozoisite and amphibole are retrograde and co-exist with sulphides. Hematite-chalcopyrite+pyrite assemblages and advanced replacement of skarn minerals by calcite+quartz are associated with the late-retrograde stage. Skarnoid, at the skarn margin, contains the main skarn minerals, feldspars, grossular-rich garnet and minor wollastonite. LA-ICP-MS trace element datasets show that skarn minerals are rich in REY, Sn, HFSE and incompatible elements. Temporal (prograde-to-retrograde) evolution is recognised in terms of chondrite-normalised REY fractionation trends for garnet, with predictable patterns from sample to sample. Trace element concentrations in garnet represent the best guide to deposit-scale zonation patterns: Sn increases in garnet from N to S, and ΣREY increases from E to W. Trends for retrograde garnet are more varied, attributable to cycles of replacement, overgrowth and recrystallization. Nanoscale FIB-SEM-TEM investigation of feldspar and garnet allows distinction of whether key trace elements are lattice-bound or occur as nanoscale mineral inclusions. Preliminary fluid inclusion data provide evidence for early high-T, high-salinity fluids (~23 wt.% NaCl equiv., ~600 ºC, ~2 kbar) and the destructive influence of retrogression and reaction with later fluids tied to skarn collapse during uplift/fault reactivation (~1 wt.% NaCl equiv., <300 ºC, ~0.15 kbar). The study shows the potential value of LA-ICP-MS trace element signatures in garnet and accessories as petrogenetic tools and, potentially, as exploration vectors. The extraordinary petrographic and geochemical complexity implies that routine application of these patterns as an exploration tool is dependent upon recognition of underlying trends specific to protolith and spatial-temporal evolution. Hillside is defined as a Fe-Cu-(Au)-skarn that includes key features of an IOCG system. The deposit formed in a deep skarn setting (~6 km) and records a late-stage overprint during uplift and fault reactivation. The data can underpin sustainable genetic models for the Hillside deposit and contribute towards a metallogenic framework for the Olympic Cu-Au province, particularly with respect to the diversity of mineralization styles as an expression of ore formation at different crustal levels.Thesis (Ph.D.) -- University of Adelaide, School of Physical Sciences, 2016.
47
Krichauff, Skye. "The Narungga and Europeans: cross-cultural relations on Yorke Peninsula in the nineteenth century." 2008. http://hdl.handle.net/2440/50133.
Повний текст джерелаАнотація:
The Narungga are the Aboriginal people of Yorke Peninsula, South Australia. This thesis explores cross-cultural encounters and relations between the Narungga and Europeans in the nineteenth century. Contemporary Narungga people, hoping to learn about the lives of their forebears, instigated this research. The Narungga have not previously been the focus of serious historical or anthropological investigation. This thesis therefore fills a significant gap in the historiography. This thesis seeks to re-imagine the past in a way which is empathetic and realistic to Narungga people who lived in the nineteenth century. To understand the impact of the arrival and permanent settlement of Europeans upon the lives of the Narungga, it is necessary to look closely at the cultural systems which orientated and encompassed both the Narungga and the newcomers. The two groups impacted on and shaped the lives of the other and neither can be looked at in isolation. This work has been inspired by the writings of historical anthropologists and ethno-historians. The findings of anthropologists, linguists, geographers, botanists and archaeologists are drawn upon. First hand accounts which provide graphic and immediate depictions of events have been closely analysed. The primary sources that have been examined include local and Adelaide newspapers, official correspondence between settlers, police, the Protector of Aborigines, the Governor and the Colonial Secretary, and private letters, diaries, paintings, photographs and sketches. The archives continuously reveal great injustices committed against the Narungga, and this thesis does not seek to minimize the brutality of ‘white’ settlement nor the devastating outcomes of British colonialism on the Narungga. But the records also reveal the majority of Narungga people living in the nineteenth century were not helpless victims being pushed around by autocratic pastoralists or disengaged bureaucrats. On Yorke Peninsula in the nineteenth century, the future was unknown; the Narungga were largely able to maintain their autonomy while Europeans were often in a vulnerable and dependent position. The Narungga were active agents who adapted to and incorporated the new circumstances as they were able and as they saw fit. Rather than living in a closed or static society, the Narungga readily accommodated and even welcomed the Europeans, with their strange customs and exotic animals, plants and goods. The Narungga responded to the presence of Europeans in a way which made sense to them and which was in keeping with their customs and beliefs.http://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1339729
Thesis (M.A.) - University of Adelaide, School of History and Politics, 2008
48
Krichauff, Skye Mary Jean. "The Narungga and Europeans: cross-cultural relations on Yorke Peninsula in the nineteenth century." Thesis, 2008. http://hdl.handle.net/2440/50133.
Повний текст джерелаАнотація:
The Narungga are the Aboriginal people of Yorke Peninsula, South Australia. This thesis explores cross-cultural encounters and relations between the Narungga and Europeans in the nineteenth century. Contemporary Narungga people, hoping to learn about the lives of their forebears, instigated this research. The Narungga have not previously been the focus of serious historical or anthropological investigation. This thesis therefore fills a significant gap in the historiography.
This thesis seeks to re-imagine the past in a way which is empathetic and realistic to Narungga people who lived in the nineteenth century. To understand the impact of the arrival and permanent settlement of Europeans upon the lives of the Narungga, it is necessary to look closely at the cultural systems which orientated and encompassed both the Narungga and the newcomers. The two groups impacted on and shaped the lives of the other and neither can be looked at in isolation. This work has been inspired by the writings of historical anthropologists and ethno-historians. The findings of anthropologists, linguists, geographers, botanists and archaeologists are drawn upon. First hand accounts which provide graphic and immediate depictions of events have been closely analysed. The primary sources that have been examined include local and Adelaide newspapers, official correspondence between settlers, police, the Protector of Aborigines, the Governor and the Colonial Secretary, and private letters, diaries, paintings, photographs and sketches.
The archives continuously reveal great injustices committed against the Narungga, and this thesis does not seek to minimize the brutality of ‘white’ settlement nor the devastating outcomes of British colonialism on the Narungga. But the records also reveal the majority of Narungga people living in the nineteenth century were not helpless victims being pushed around by autocratic pastoralists or disengaged bureaucrats. On Yorke Peninsula in the nineteenth century, the future was unknown; the Narungga were largely able to maintain their autonomy while Europeans were often in a vulnerable and dependent position. The Narungga were active agents who adapted to and incorporated the new circumstances as they were able and as they saw fit. Rather than living in a closed or static society, the Narungga readily accommodated and even welcomed the Europeans, with their strange customs and exotic animals, plants and goods. The Narungga responded to the presence of Europeans in a way which made sense to them and which was in keeping with their customs and beliefs.Thesis (M.A.) - University of Adelaide, School of History and Politics, 2008
49
Pavils, Janice Gwenllian. "ANZAC culture : a South Australian case study of Australian identity and commemoration of war dead / Janice Gwenllian Pavils." Thesis, 2004. http://hdl.handle.net/2440/22186.
Повний текст джерелаАнотація:
"December 2004"Bibliography: leaves 390-420.
vii, 420 leaves : ill., maps, photos. (col.) ; 30 cm.
Thesis (Ph.D.)--University of Adelaide, School of History and Politics, Discipline of History, 2005
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Pavils, Janice Gwenllian. "ANZAC culture : a South Australian case study of Australian identity and commemoration of war dead / Janice Gwenllian Pavils." 2004. http://hdl.handle.net/2440/22186.
Повний текст джерелаАнотація:
"December 2004"Bibliography: leaves 390-420.
vii, 420 leaves : ill., maps, photos. (col.) ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, School of History and Politics, Discipline of History, 2005