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Thematische Bibliographien / Structural South Australia Flinders Ranges / Dissertationen

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Dissertationen zum Thema „Structural South Australia Flinders Ranges“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 2. Februar 2022

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1

Mendis, Premalal J. „The origin of the geological structures, diapirs, grabens, and barite veins in the Flinders Ranges, South Australia“. Title page, abstract and contents only, 2002. http://web4.library.adelaide.edu.au/theses/09PH/09phm5389.pdf.

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Bibliography: leaves [156-167] Map 1. Parachilna, sheet SH 54-13 / compiled by P. Reid and W.V. Preiss. 2nd ed. [Adelaide] : Primary Industries & Resources SA, 1999. 1 map : col ; 69 x 100 cm. (South Australia. Geological Survey. Geological atlas 1:250 000 series ; sheet SH 54-13) -- map 2. Geology of the Flinders Ranges National Park. Parkside, S. Aust. : Mines and Energy South Australia, 1994. 1 map : col. ; 84 x 60 cm. Scale: 1:75 000.

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2

Jansyn, Joanne. „Strato-tectonic evolution of a large subsidence structure associated with the late Proterozoic Wonoka Formation at Wilpena Pound, central Flinders Ranges, South Australia /“. Title page, table of contents and abstract only, 1990. http://web4.library.adelaide.edu.au/theses/09SB/09sbj35.pdf.

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Thesis (B. Sc. (Hons))--University of Adelaide, Dept. of Geology and Geophysics, 1991.
One col. map + one col. chart in pocket. National grid reference : Parachilna sheet H54-13 (1:250 000). Includes bibliographical references.

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3

Higgins, Jonathan. „The Pamatta Pass Canyon Complex : Neoproterozoic Wonoka Formation, Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09SB/09sbh636.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
National Grid Reference:-Orroroo Sheet SI 54-1 (1:250,000 Geological Series). One col. folded map in pocket on back cover. Includes bibliographical references (8 leaves ).

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4

Fuller, Margaret. „Early Cambrian corals from the Moorowie Formation, Eastern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SM/09smf967.pdf.

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5

Chow, Angie N. C. „Geomorphic evolution of the Mt. Arden Creek Valley, southern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbc552.pdf.

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Thesis (B. Sc. (Hons.))--University of Adelaide, Dept. of Geology, 1993.
On title page: National grid reference Orroroo SI 54-1 6533-4 (1:250 000). Includes bibliographical references (leaves 8-11).

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6

Meredith, Kirsten. „Geological history of the Waukarie Creek Canyon complex, southern Flinders Ranges, South Australia /“. Title page and contents only, 1997. http://web4.library.adelaide.edu.au/theses/09SB/09sbm559.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
National Grid reference Port Augusta SI 53-4 Orroroo SI 54-1. Includes bibliographical references (leaves 41-43).

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7

Nitschke, Nicholas Leigh. „Identification of aeolian dust mantles in the semi-arid Flinders Ranges, South Australia /“. Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09ENVSH/09envshn732.pdf.

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8

Chor, Carly Choi-Choo. „Palaeohydrology of a late Pleistocene wetland in the central Flinders Ranges, South Australia /“. Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SB/09sbc5511.pdf.

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9

Greene, Susan J. „A geomorphological and sedimentological study of a climbing dune, Northern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09AR/09arg8118.pdf.

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10

Dorjgurhem, Batbold. „Regional biodiversity management strategy : case study on the Flinders Ranges“. Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09AS/09asd699.pdf.

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Bibliography: leaves 107-117. This thesis examines the rationale for managing biological diversity on a regional basis and develops recommendations for the use of two computational methods in biodiversity management planning by conducting a case study in the Flinders Ranges, centred on the Yellow-footed Rock Wallaby (abstract)

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11

Tunbridge, Dorothy, und n/a. „Mammals of the dreaming : an historical ethnomammalogy of the Flinders Ranges“. University of Canberra. Resource, Environmental & Heritage Sciences, 1996. http://erl.canberra.edu.au./public/adt-AUC20061113.161511.

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This work is a linguistically based historical ethnography of the mammal species of the Flinders Ranges, South Australia, from pre-European times to the present day. The research was motivated by linguistic evidence in the Adnyamathanha people's language, Yura Ngawarla, for the recent existence of a number of mammals in the Flinders Ranges region. The work aims firstly to identify each species represented by those language terms and to discover the identity of other species also present in the past 200 years. Secondly, it aims to present an exhaustive ethnography of mammals for that region. This work is essentially cross-disciplinary, with research extending into the often overlapping fields of linguistics, anthropology, archaeology, applied science, historical zoology and history. Comparative linguistics, oral tradition, historical records, scientific data and sub-fossil material are used to identify the species present at European occupation and their role in traditional Aboriginal life, and in passing, to establish the former existence and distribution of those species throughout the region of the two South Australian gulfs. An inventory of extant and extinct Flinders Ranges species is established. Linguistic, ethnographic, zoological and historical data are used to estimate when species extinction occurred, and what may (or may not) have been the main factors involved. A significant outcome of this work is the documentation of a part of Aboriginal knowledge which itself was on the verge of extinction, and the affirmation of well attested Aboriginal oral tradition as an authentic 'authoritative source'. Conclusion: Prior to European occupation the Flinders Ranges had a rich mammalian fauna comprising around 60 native species. These played a significant part in Aboriginal people's diet, manufacturing industry and cultural and spiritual life. By the end of the first half century of European occupation or soon after around two thirds of the terrestrial species had vanished. The effect of these events on Aboriginal people's ability to survive in their own territory was devastating and irreversible.

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12

Grgurich, Mark. „Denudation chronology and drainage patterns of the Arden-Yarrah Vale region, southern Flinders Ranges, South Australia /“. Title page, abstract and contents only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbg8452.pdf.

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Thesis (B. Sc. (Hons.))--University of Adelaide, Dept. of Geology and Geophysics, not conferred 1992.
On title page: National Grid reference; Orroroo S1 54-1 6533-4 (1:250,000). Three coloured, folded maps in pocket on back cover. Includes bibliographical references (leaves 31-34).

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13

St, John Barbara J. „Ecology and management of the Little Corella (cacatua sanguinea) in the southern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09SM/09sms143.pdf.

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14

Bourne, Jennifer A. „Landform development and stream behaviour in the western piedmont zone of the Flinders Ranges of South Australia“. Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09phb7753.pdf.

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Six folded maps in pocket inside back cover. Includes bibliographies. Pediments and alluvial fans coexist in the piedment of the Flinders Ranges in the arid to semi-arid interior of South Australia, which thus affords the opportunity to study them in identical geological, climatic and topographic contexts.

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15

Hart, John. „Lower Cambrian corals from archaeocyathan - Epiphyton clasts within the Moorowie Formation megabreccia northern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09SB/09sbh325.pdf.

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16

Chalklen, Andrew John. „Managing public access to arid lands in South Australia : a case study of the north Flinders Ranges /“. Title page, contents and abstract only, 1990. http://web4.library.adelaide.edu.au/theses/09ENV/09envc436.pdf.

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17

Cooper, Andrew McGregor. „Late Proterozoic hydrocarbon potential and its association with diapirism in Blinman #2, Central Flinders Ranges, South Australia /“. Title page, abstract and contents only, 1991. http://web4.library.adelaide.edu.au/theses/09SB/09sbc776.pdf.

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Thesis (B. Sc.(Hons))--National Centre for Petroleum Geology and Geophysics, University of Adelaide, 1991.
"National grid reference 1:250 000 - Parachilna SH54-13." Includes bibliographical references (leaves 45-47).

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18

McFarlane, Kylie. „Mississippi Valley-type lead-zinc mineralisation at Donkey Bore and Old Wirrealpa Springs, central Flinders Ranges, South Australia /“. Title page, abstract and table of contents only, 1993. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bm143.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1994?
Two coloured maps and overlay in pocket inside back cover. National grid reference SH54-13. Includes bibliographical references (leaves 34-38).

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19

Rule, Beau Brenton. „Ediacaran biodiversity : palaeoecological assessment of successive latest Proterozoic (Neoproterozoic) faunal assemblages in the Western Flinders Ranges, South Australia /“. Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SB/09sbr9352.pdf.

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20

Gregory, Christopher T. „The geology and origin of sedimentary manganese from the Boolcunda, Etna and Muttabee Deposits, central Flinders Ranges, South Australia /“. Title page, table of contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09SB/09sbg822.pdf.

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21

Singh, Updesh. „Late Precambrian and Cambrian carbonates of the Adelaidean in the Flinders Ranges, South Australia : a petrographic, electron microprobe and stable isotope study /“. Title page, abstract and contents only, 1986. http://web4.library.adelaide.edu.au/theses/09PH/09phs1792.pdf.

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22

Hearon, IV Thomas E. „Analysis of salt-sediment interaction associated with steep diapirs and allochthonous salt| Flinders and willouran ranges, south australia, and the deepwater northern gulf of Mexico“. Thesis, Colorado School of Mines, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3602617.

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The eastern Willouran Ranges and northern Flinders Ranges, South Australia contain Neoproterozoic and Cambrian outcrop exposures of diapiric breccia contained in salt diapirs, salt sheets and associated growth strata that provide a natural laboratory for testing and refining models of salt-sediment interaction, specifically allochthonous salt initiation and emplacement and halokinetic deformation. Allochthonous salt, which is defined as a sheet-like diapir of mobile evaporite emplaced at younger stratigraphic levels above the autochthonous source, is emplaced due to the interplay between the rate of salt supply to the front of the sheet and the sediment-accumulation rate, and may be flanked by low- to high-angle stratal truncations to halokinetic folds. Halokinetic sequences (HS) are localized (<1000 m) unconformity-bound successions of growth strata adjacent to salt diapirs that form as drape folds due to the interplay between salt rise rate (R) and sediment accumulation rate (A). HS stack to form tabular and tapered composite halokinetic sequences (CHS), which have narrow and broad zones of thinning, respectively. The concepts of CHS formation are derived from outcrops in shallow water to subaerial depositional environments in La Popa Basin, Mexico and the Flinders Ranges, South Australia. Current models for allochthonous salt emplacement, including surficial glacial flow, advance above subsalt shear zones and emplacement along tip thrusts, do not address how salt transitions from steep feeders to low-angle sheets and the model for the formation of halokinetic sequences has yet to be fully applied or tested in a deepwater setting. Thus, this study integrates field data from South Australia with subsurface data from the northern Gulf of Mexico to test the following: (1) current models of allochthonous salt advance and subsalt deformation using structural analysis of stratal truncations adjacent to outcropping salt bodies, with a focus on the transition from steep diapirs to shallow salt sheets in South Australia; and (2) the outcrop-based halokinetic sequence model using seismic and well data from the Auger diapir, located in the deepwater northern Gulf of Mexico. Structural analysis of strata flanking steep diapirs and allochthonous salt in South Australia reveals the transition from steep diapirs to shallowly-dipping salt sheets to be abrupt and involves piston-like breakthrough of roof strata, freeing up salt to flow laterally. Two models explain this transition: 1) salt-top breakout, where salt rise occurs inboard of the salt flank, thereby preserving part of the roof beneath the sheet; and 2) salt-edge breakout, where rise occurs at the edge of the diapir with no roof preservation. Shear zones, fractured or mixed `rubble zones' and thrust imbricates are absent in strata beneath allochthonous salt and adjacent to steep diapirs. Rather, halokinetic drape folds, truncated roof strata and low- and high-angle bedding intersections are among the variety of stratal truncations adjacent to salt bodies in South Australia. Interpretation and analysis of subsurface data around the Auger diapir reveals similar CHS geometries, stacking patterns and ratios of salt rise and sediment accumulation rates, all of which generally corroborate the halokinetic sequence model. The results of this study have important implications for salt-sediment interaction, but are also critical to understanding and predicting combined structural-stratigraphic trap geometry, reservoir prediction and hydrocarbon containment in diapir-flank settings.

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23

Nedin, Christopher. „The nature of the Precambrian-Cambrian transition in the northern Flinders Ranges, South Australia ; The dietary niche of the extinct Australian marsupial lion Thylacoleo carnifex Owen /“. Title page, abstract and contents only, 1990. http://web4.library.adelaide.edu.au/theses/09SB/09sbn371.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1991?
Two col. maps in pocket. National grid reference: Coply SH54-9 1:250 000. Includes bibliographical references.

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24

Yassaghi, Ali. „Geometry, kinematics, microstructure, strain analysis, and P-T conditions of the shear zones and associated ductile thrusts in the southern Mt. Lofty Ranges/Adelaide Hills area, South Australia /“. Title page, contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phy29.pdf.

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25

Lau, Ian Christopher. „Lithological, structural and lineament analysis of the Southern Mount Lofty Ranges, South Australia, using remote sensing and geographical information system techniques /“. Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SB/09sbl3662.pdf.

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26

Ayliffe, Damien. „Geological setting of the late Proterozoic Wonoka Formation carbonate ramp and canyon sequence at Pichi Ric hi Pass Southern Flinders Ranges, South Australia : geoch emical, stable isotope, and diagenetic analysis /“. Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09S.B/09s.ba978.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1992?
On title page: "National Grid reference: Port Augusta sheet SI 53-4 (1:250000) Onnoroo sheet SI 54-1 (1:250 00 0)." One map in pocket inside back cover. Includes bibliographical references (leaves 52-60).

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27

Dare, David L. „The anatomy of a fold and thrust terrane in the northern Mt. Lofty Ranges, South Australia : an appraisal of the structural evolution and the implications for gold and base metal mineralization in the region of the Ulooloo Gold Reserve /“. Title page, contents and introduction only, 1995. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bd217.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1996.
Australian National Grid reference Hallett 6631-11 1:50 000 sheet Caroona 6731-111 1:50 000 sheet. Includes bibliographical references.

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28

Mendis, Premalal J., Primary Industries and Resources SA Parachilna [cartographic material] und Mines and Energy South Australia Geology of the Flinders Ranges National Park [cartographic material]. „The origin of the geological structures, diapirs, grabens, and barite veins in the Flinders Ranges, South Australia / by Premalal J. Mendis“. 2002. http://hdl.handle.net/2440/21925.

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Bibliography: leaves [156-167]
155, [156-184] leaves : ill. (some col.), maps (some col.) ; 30 cm. + 2 maps in back pocket
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 2003

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29

Wulser, Pierre-Alain. „Uranium metallogeny in the North Flinders Ranges region of South Australia“. 2009. http://hdl.handle.net/2440/57970.

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The geological province of the Mount Painter in the North Flinders Ranges (South Australia) is well-known for its uranium mineralisation, and uraniferous granites. The presence in the nearby Cenozoic sediments of the Lake Frome basin of uranium mineralisations (Beverley deposit) and the recent discovery of the Four Mile deposit has triggered the interest of explorers. Based on extensive laser-ablation inductively-coupled-plasma-mass-spectrometry (LA-ICPMS) U-Pb geochronological data and mineralogy of U-Th-bearing minerals, rock geochemistry and petrography, we present a global study on the mobility of U, Th and REE in the Mount Painter Domain, including a detailed reconstitution of the Beverley deposit genesis. Seven significant stages of U-Th-REE mobility are recognised: 1. The possible presence U-enriched ~1600 Ma lower crust under the MPD 2. Intrusion of two A-type Mesoproterozoic granites suites (~1575, and ~1560 Ma respectively) with high HFSE contents and crustal origin; the porphyritic biotite K-rich highly-enriched Yerila granite belongs to the youngest suite and hosts magmatic allanite-(Ce), potassic-hastingsite, ilmenite, fergusonite-(Y), chevkinite, molybdenite, zircon, uranothorite, uraninite and titanite and fluorite 3. Late-magmatic or post-magmatic metasomatism in the same granites; evidenced by F-rich annite, zircon, Y-bearing Al-F-titanite (< 6 kbar, >400°C), Y-rich fluorapatite, synchysite-(Ce) and fluorite. Early ilmenite, molybdenite, allanite-(Ce) and oligoclase reacted with an alkaline oxidising F-rich melt or fluid. The latemagmatic to post-magmatic metasomatism is also recorded at the intrusion contact in regional rocks, forming allanite-, magnetite-, uranothorite-, zircon- (1501 ± 6 Ma), and uraninite-bearing calcsilicate skarns. The spreading of zircon ages in the Yerila granite (~1565 to ~1521) relates to the mixing of magmatic and metasomatic crystals. 4. the MPD was subject to the Delamerian orogeny and related metamorphism (amphibolite facies); most Mesoproterozoic granitic assemblages present signs of recrystallisation or stress; recrystallisation of monazite-(Ce) and xenotime-(Y) during Paleozoic (Cambrian) (490-495 Ma). U-Th-rich minerals also bear Delamerian ages (polycrase-(Y), euxenite-(Y), davidite-(La) and uraninite). 5. Anatexis of local basement during Ordovician and generation of peraluminous granite (British Empire granite) with low Th/U. The granite is enriched in U and Y. We provide the first robust ages on it: 456 ± 9 and 459 ± 9 Ma on zircon, 453.3 ± 4.6 on xenotime-(Y). 6. Very active hydrothermal/pegmatitic uranium remobilisation along active faults; brannerite-quartz veins formation (367 ± 13 Ma), further signs of remobilisation or hydrothermal event during Permian (284 ± 25 Ma in thorite) and around the Mt Gee (~290 Ma radiogenic gain in davidite) which agrees with the previous data (paleomagnetic ages of 250-300 Ma). 7. Cenozoic supergene uranium remobilisation in MPD and migration of U-rich oxidised groundwaters into the Lake Frome. The uranium is precipitated in the sandy formation of the lake and in the top layer of the underlying organic-matter-rich clays and silts. The micro-environment of reduction efficiently trap U but also REE, fingerprinting the REE-rich MPD granite source. Coffinite and carnotite give concordant Pliocene ages (6.7 to 3.4 Ma). Provenance studies on the sands hosting the Beverley mineralisations suggest a reworking of Early Cretaceous glacial or glacio-lacustrine sediments originally sourced in Eastern Australia (Lachlan Fold Belt). The youngest recorded zircon (130 Ma) doesn’t constrain the sediment age but refines the provenance region (New England Orogen).
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Thesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2009

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30

Moskwa, Emily Claire. „Ecotourism as a means of encouraging ecological recovery in the Flinders Ranges, South Australia“. 2008. http://hdl.handle.net/2440/50481.

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Some of Australia’s most pressing conservation problems are found in the arid and semi-arid rangelands where the traditional major land-use is extensive pastoralism. Yet with the emergence of a change in resource values, the rangelands of Australia have started to move away from a strict production land-use towards a multifunctional land-use where pastoralism, tourism and the environment have an influence on one another. With the present mixture of consumption and protection values in the rangelands, ecotourism represents a model for achieving a symbiotic relationship between tourism activity and conservation in a pastoral setting. This study develops a theoretical framework for understanding the relationships between ecotourism, pastoralism and ecological recovery efforts in the Flinders Ranges through employing mixed qualitative and quantitative research techniques to examine the perceptions and practices of tourism operators, local landholders and visitors to the study site. The study finds that while pastoralism and its level of success often remain variable, the strength and stability of tourism is increasing. Because economics is a central component of the concept of sustainability, and because we must manage the environment while accommodating tourists, ecotourism is one way to help reach rangeland sustainability goals, provided that there are adequate levels of agreement amongst the local community and other land users. The results indicate that the vast majority of stakeholders are currently in a state of co-existence with each other rather than one of conflict, suggesting ecotourism has the potential to assist ecological recovery. However, many landholders are constrained in their ability to integrate ecotourism operations and conservation due to economic difficulties and market barriers. There are also conflicting results among visitors who claim to be interested in ecotourism but do not necessarily act accordingly, highlighting the need for a greater focus on environmental education. Ecotourism should be incorporated into a regional sustainability plan where the public are able to assist decision makers through collaborative planning. The thesis concludes that when well-managed, ecotourism can be a business supporting conservation in the Flinders Ranges. It contributes to knowledge of the role that ecotourism can play in encouraging ecological recovery in the rangelands and explores the complex interrelationships involved through consultation with the primary stakeholders of landholders, tourism operators and visitors.
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Thesis (Ph.D.) - University of Adelaide, School of Social Sciences, 2008

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31

Tokarev, Victor. „Neotectonics of the Mount Lofty Ranges (South Australia) / Victor Tokarev“. 2005. http://hdl.handle.net/2440/22225.

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"February, 2005"
Bibliography: leaves 259-272.
ix, 272 leaves : ill. (some col.), maps (col.), plates (col.) ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
"The Mount Lofty Ranges and flanking St Vincent and Western Murray Basins preserve a rich record of Australian intraplate neotectonic movements and their effects of landscape evolution and sedimentary basin development in this region of South Australia." "The major goal of this study is to develop a new tectonic model that contributes to our fundamental understanding of how neotectonic motions and deformations operate within this sector of the southern Australian Earth crust. The other main aim of this thesis is to provide a better understanding of the effects those neotectonic movements imposed on landscape evolution and sedimentation." --Introd.
Thesis (Ph.D.)--University of Adelaide, Faculty of Science, School of Earth and Environmental Sciences, Discipline of Geology and Geophysics, 2005

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32

Lemon, Nicholas M. „Diapir recognition and modelling with examples from the late proterozoic Adelaide Geosyncline, Central Flinders Ranges, South Australia / Nicholas M. Lemon“. 1988. http://hdl.handle.net/2440/18825.

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1v. / 2 maps
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1988

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