Academic literature on the topic 'Curnamona Province'
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Journal articles on the topic "Curnamona Province"
Kay, Ben, Graham Heinson, and Kate Brand. "Crustal magnetotelluric imaging of a Paleoproterozoic graphitic suture zone, Curnamona Province, Australia." Gondwana Research 106 (June 2022): 1–14. http://dx.doi.org/10.1016/j.gr.2021.12.005.
Full textClark, Chris, Andreas Schmidt Mumm, Martin Hand, and Kevin Faure. "Episodic shear zone associated fluid flow in the Curnamona Province, South Australia." Journal of Geochemical Exploration 89, no. 1-3 (April 2006): 69–72. http://dx.doi.org/10.1016/j.gexplo.2005.11.090.
Full textBaker, D., J. Joseph, A. Fabris, and M. Tingay. "Electromagnetic Soundings of the Regolith at Kalkaroo Mineral Prospect, Curnamona Province, South Australia." ASEG Extended Abstracts 2007, no. 1 (December 1, 2007): 1. http://dx.doi.org/10.1071/aseg2007ab009.
Full textMauger, A. "Mapping regional alteration patterns in the Curnamona Province using hyperspectral core scanning technology." ASEG Extended Abstracts 2009, no. 1 (2009): 1. http://dx.doi.org/10.1071/aseg2009ab099.
Full textFabris, Adrian J., John L. Keeling, and Roger W. Fidler. "Surface geochemical expression of bedrock beneath thick sediment cover, Curnamona Province, South Australia." Geochemistry: Exploration, Environment, Analysis 9, no. 3 (July 21, 2009): 237–46. http://dx.doi.org/10.1144/1467-7873/09-196.
Full textKay, Ben, Kate Robertson, Stephan Thiel, and Graham Heinson. "Resistivity structure of the Link East MT transect in the Southern Curnamona Province." ASEG Extended Abstracts 2019, no. 1 (November 11, 2019): 1–4. http://dx.doi.org/10.1080/22020586.2019.12072995.
Full textGanne, Jérôme, P. G. Betts, R. Weinberg, and M. Noble. "RETRACTED: Structural complexity in the Curnamona Province (South Australia): Polyphase strain partitioning and reactivation." Precambrian Research 143, no. 1-4 (December 2005): 50–74. http://dx.doi.org/10.1016/j.precamres.2005.09.010.
Full textHewson, R. D., T. J. Cudahy, S. Mizuhiko, K. Ueda, and A. J. Mauger. "Seamless geological map generation using ASTER in the Broken Hill-Curnamona province of Australia." Remote Sensing of Environment 99, no. 1-2 (November 2005): 159–72. http://dx.doi.org/10.1016/j.rse.2005.04.025.
Full textWilliams, H. A., P. G. Betts, L. Ailleres, and A. Burtt. "Characterization of a proposed Palaeoproterozoic suture in the crust beneath the Curnamona Province, Australia." Tectonophysics 485, no. 1-4 (April 2010): 122–40. http://dx.doi.org/10.1016/j.tecto.2009.12.008.
Full textKorsch, R. J., B. R. Goleby, A. C. Burtt, W. V. Preiss, T. Fomin, C. H. H. Conor, and R. S. Robertson. "Deep seismic reflection data from the Curnamona Province, South Australia: crustal architecture and tectonic implications." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–2. http://dx.doi.org/10.1071/aseg2006ab088.
Full textDissertations / Theses on the topic "Curnamona Province"
Ellershaw, Angus. "Fluid inclusion, petrographic and sulphur isotope investigations into Luxemburg mineral deposits, Curnamona Province, South Australia /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbe457.pdf.
Full textHeimann, Ríos Adriana. "Geochemical keys for the genesis of Proterozoic garnet-rich rocks and minor metasediment-hosted Pb-Zn-Ag mineralization, southern Curnamona Province, Australia." [Ames, Iowa : Iowa State University], 2006. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3244372.
Full textKay, B. V. "Testing the uncover paradigm: crustal fluid pathways in the Curnamona Province." Thesis, 2017. http://hdl.handle.net/2440/128253.
Full textIn July 2017, scale-reduction was undertaken to improve the bandwidth and resolution of the AusLAMP defined Curnamona Conductor (Robertson et al., 2016) by way of a broadband magnetotelluric profile with site spacing of 2 km, extending from the Erudina Domain across the Mudguard and Quinyambie Domains in the Curnamona Province. A fossil fluid pathway has been identified from the lower mid crustal conductor to the near surface situated near a topographic basement high. The upper crustal conductor has been further delineated beneath the Quinyambie Domain to within 5 km of the surface situated alongside a major crustal feature.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2017
Clark, Christopher F. P. "Fluid-rock systems in the Southern Curnamona Province Australia/ Christopher F.P. Clark." 2005. http://hdl.handle.net/2440/22329.
Full textBibliography: pages 109-121.
xii, 121 pages : ill., maps (1 col.), plates, photographs (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 Earth and Environmental Sciences, Discipline of Geology and Geophysics, 2006
Clark, Christopher Francis Paul. "Fluid-rock systems in the Southern Curnamona Province Australia/ Christopher F.P. Clark." Thesis, 2005. http://hdl.handle.net/2440/22329.
Full textBibliography: pages 109-121.
xii, 121 pages : ill., maps (1 col.), plates, photographs (some col.) ; 30 cm.
Thesis (Ph.D.)--University of Adelaide, School of Earth and Environmental Sciences, Discipline of Geology and Geophysics, 2006
Rutherford, Lachlan Stuart. "Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications." 2006. http://hdl.handle.net/2440/37818.
Full textThesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.
Wittwer, P. D. "Geology and geochemistry of regolith carbonate accumulations of the southwestern Curnamona Province, SA: Implications for mineral exploration." Thesis, 2004. http://hdl.handle.net/2440/123526.
Full textAlthough regolith carbonate accumulations (RCAs) have been extensively used in mineral exploration programs in the regolith-dominated terrains of the Yilgarn and Gawler Cratons, their use has so far been limited within the Curnamona Province, SA. This study shows how the detailed characterisation of RCAs in the southwestern Curnamona Province enhances their use in mineral exploration programs at the regional to prospect scales. A regional RCA distribution map for the study area shows that RCAs are generally widespread, although certain RCA morphological facies are dominant in different parts of the landscape, and in some areas RCAs are absent or at best a very minor component of the regolith. A dataset of whole rock geochemical assays of RCAs provides the basis of graphical presentations and geochemical maps that highlight the chemical characteristics of RCAs proximal to areas of known Au mineralisation in contrast to more distal samples. Several Au pathfinder elements in RCA assays were found to include As, W, Bi, and Mo, and greatly assist in further anomaly definition when used in conjunction with Au assays. Major element composition (e.g. Ca, Mg, Fe) showed little relationship to local landform setting, however, landscape setting appears to be a more important control on Au assay results both at the regional and prospect scales. Gold distribution in the area was independent of the presence of major elements such as calcium and magnesium. Microprobe analysis showed that Au was rare and invisible at the resolution of the analysis and existed in the calcium carbonate matrix as well as in detrital material. The composition of the underlying rock lithologies was also compared to the whole rock chemistry of the RCAs and showed the possibilities of this technique to aid geological mapping in regolith-dominated terrains and to assist in locating mineralised systems.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2004
Shearer, A. "The application of ground based and airborne radiometric methods to aid geological mapping in the Olary Province, South Australia." Thesis, 1999. http://hdl.handle.net/2440/112811.
Full textThe Late Palaeoproterozoic Olary Domain, in the east of South Australia, has been extensively surveyed using airborne geophysical methods, including 256 channel radiometries. This detailed data set over outcropping areas is potentially a valuable aid to geological mapping. Ground-based radiometric data was obtained along profiles through the eastern Weekeroo Inlier and Ninnerie Hill areas in order to relate radioelement concentrations to lithological units. The Weekeroo Inlier traverse sampled all stratigraphic units present in the Olary Domain. The Ninnerie Hill traverse sampled Early Mesoproterozoic granitoids, migmatites and host metasediments. Two acquisition styles were attempted when collecting the ground-based data, with continuous recording to provide results that better replicate the airborne data than discrete sampling. The discrete sampling method was found to be heavily influenced by single point anomalies and not representative of the lithological average. Relative peaks and troughs on all three channels and total count data correspond well between the ground and airborne data. Correlation between the airborne data and the ground-based data was best for the K channel. For the Th channel the ground-based data was similar to the airborne data in wavelength and amplitude but was bulk shifted below the airborne data. The U channel data from the ground-based data detected the same anomalies as the airborne data but was an order of magnitude higher. The differences between the airborne and ground-based data could be due to errors in the calibration process that was performed for part of this project or due to the time difference in acquisition of the ground based and airborne data. Comparison of ground-based data with the geology of the survey areas revealed that radiometric data can provide useful lithological discrimination. Within the survey area some differences between metasediments, intrusive lithologies, and alteration types are determinable. The radiometric data can successfully differentiate between potasic and sodic granites. The low levels in all three measured radioelement channels can reflect occurrences of amphibolites. The data discriminates between pelites and psammites in that the pelites contain significantly higher levels of K, the difference between levels of Th and U are less extreme but are still discernable. As well as providing a mapping tool on the lithology scale, the interpretation of radiometric data can resolve sub-lithology scale variations.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1999
Conway, D. J. "A numerical study on the distortion of magnetotelluric data from topography, near-surface conductors and basins." Thesis, 2013. http://hdl.handle.net/2440/100070.
Full textMagnetotelluric (MT) data may be distorted by a variety of structures, including near-surface inhomogeneities, topographic gradients and large conductive bodies. A synthetic study is undertaken to analyse these three factors in the Curnamona Province, South Australia. Firstly, the effect of topography in the northern Flinders Ranges is investigated by the use of forward models. The results show both a galvanic and an inductive distortion concentrated at high topographic gradients. The effect of near-surface conductors is also investigated with forward models, using data from Lake Frome as input. The models show a small area of galvanic distortion around the circumference of the lake, but no regional effect. These results are compared with distortion analyses of real data. Finally, thin-sheet modelling is used to determine the effect of a synthetically calculated conductance using data from the eastern Arrowie Basin. Results from the thin-sheet model show that the Arrowie Basin has the potential to inductively distort MT data on a regional scale. Using this result as motivation, two three-dimensional (3-D) inversions are undertaken on the Geoscience Australia "08GA-C1 MT" line; one incorporating the Arrowie Basin as a prior model and the other starting from a homogeneous half-space. The results of these inversions are overlain with interpretations from seismic data collected along the same line. The best agreement between the seismic and MT data is achieved with the prior-model inversion, supporting the hypothesis that basin scale conductivity structures distorts MT data and showing that this effect is alleviated by incorporating basin structure as a prior model during inversion.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2013
Payne, J. L. "The Poodla Granite in the Olary Domain, South Australia: Intrusive relationships, alteration and implications for Cu-Au mineralisation." Thesis, 2003. http://hdl.handle.net/2440/112941.
Full textThe Palaeoproterozoic Poodla Granite within the Olary Domain, Curnamona Province, South Australia, has been suggested as a direct contributor to Cu-Au mineralisation within the region on the basis of age correlations. Alteration present within the Poodla Granite consists of four styles that have been interpreted as two events. The first event includes pervasive potassic alteration followed by pervasive Na-Ca alteration. Sm/Nd isotope analysis indicates fluids for this event were sourced from the Willyama Supergroup sediments. The second event consists of fracture-controlled sodic and Ca-Na-Si alteration with associated actinolite/clinopyroxene brecciation. Utilisation of magmatic major element trends obtained from a natural analogue (Mt Angelay Complex, Cloncurry District) has allowed greater accuracy in chemical characterisation of alteration. Fluid inclusion analysis has identified two distinct fluids involved in the later fracture-controlled sodic and Ca-Na-Si alteration event. Namely, a low salinity (18-26wt% NaCl equivalent) and a high salinity (35-45wt% NaCl equivalent) fluid. A later fluid mobilisation event related to the Palaeozoic Delamerian Orogeny is indicated by re-equilibration of the Rb/Sr isotopic system. New age constraints from other granites in the I-type suite, to which Poodla Granite belongs, suggest the Poodla Granite did not have direct hydrothermal input into regional Cu-Au mineralisation. Analysis of alteration chemistry suggests that Cu and Au mobilisation occurred during the first alteration event. These results offer evidence for previously untested Cu-Au mineralising models within the region and may encourage exploration for Cu-Au resources.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2003
Conference papers on the topic "Curnamona Province"
Ware, Bryant, Janne Liebmann, Chris Kirkland, Svetlana Tessalina, David Mole, Kathryn Waltenberg, David Huston, Geoffrey Fraser, and David Champion. "Pb Isotopes of the Curnamona Province, an example of extreme crustal fractionation in the Proterozoic." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12786.
Full textAlexander, Elinor. "Natural hydrogen exploration in South Australia." In PESA Symposium Qld 2022. PESA, 2022. http://dx.doi.org/10.36404/putz2691.
Full textReports on the topic "Curnamona Province"
Wade, C., A. Reid, A. Fabris, S. Hore, and K. Robertson. Curnamona Province: IOCG frontier between Olympic Cu-Au Province-Mt Isa. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329164.
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