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Journal articles on the topic 'Curnamona Province'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

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.

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2

Clark, 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.

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3

Baker, 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.

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4

Mauger, 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.

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5

Fabris, 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.

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6

Kay, 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.

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7

Ganne, 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.

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8

Hewson, 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.

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9

Williams, 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.

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10

Korsch, 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.

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11

Dentith, Mike, Philip Hawke, and Duncan Cowan. "Geophysical characteristics of some Proterozoic base-metal deposits in the Curnamona province of South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 101–20. http://dx.doi.org/10.1071/asegspec12_09.

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12

Dutch, Rian A., Martin Hand, and Chris Clark. "Cambrian reworking of the southern Australian Proterozoic Curnamona Province: constraints from regional shear-zone systems." Journal of the Geological Society 162, no. 5 (September 2005): 763–75. http://dx.doi.org/10.1144/0016-764904-102.

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13

Reid, Anthony. "The Olympic Cu-Au Province, Gawler Craton: A Review of the Lithospheric Architecture, Geodynamic Setting, Alteration Systems, Cover Successions and Prospectivity." Minerals 9, no. 6 (June 20, 2019): 371. http://dx.doi.org/10.3390/min9060371.

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Abstract:

The Olympic Cu-Au Province is a metallogenic province in South Australia that contains one of the world’s most significant Cu-Au-U resources in the Olympic Dam deposit. The Olympic Cu-Au Province also hosts a range of other iron oxide-copper-gold (IOCG) deposits including Prominent Hill and Carrapateena. This paper reviews the geology of the Olympic Cu-Au Province by investigating the lithospheric architecture, geodynamic setting and alteration systematics. In addition, since the province is almost entirely buried by post-mineral cover, the sedimentary cover sequences are also reviewed. The Olympic Cu-Au Province formed during the early Mesoproterozoic, ca. 1.6 Ga and is co-located with a fundamental lithospheric boundary in the eastern Gawler Craton. This metallogenic event was driven in part by melting of a fertile, metasomatized sub-continental lithospheric mantle during a major regional tectonothermal event. Fluid evolution and multiple fluid mixing resulted in alteration assemblages that range from albite, magnetite and other higher temperature minerals to lower temperature assemblages such as hematite, sericite and chlorite. IOCG mineralisation is associated with both high and low temperature assemblages, however, hematite-rich IOCGs are the most economically significant. Burial by Mesoproterzoic and Neoproterozoic-Cambrian sedimentary successions preserved the Olympic Cu-Au Province from erosion, while also providing a challenge for mineral exploration in the region. Mineral potential modelling identifies regions within the Olympic Cu-Au Province and adjacent Curnamona Province that have high prospects for future IOCG discoveries. Exploration success will rely on improvements in existing potential field and geochemical data, and be bolstered by new 3D magnetotelluric surveys. However, drilling remains the final method for discovery of new mineral resources.

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14

Godsmark, Bruce, Michael Hudson, Neil Hughes, David Mclnnes, and Graham Teale. "Geophysical exploration for copper-gold mineralisation in the Benagerie Ridge Magnetic Complex, Curnamona Province, South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 135–46. http://dx.doi.org/10.1071/asegspec12_12.

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15

Rutherford, L., M. Hand, and K. Barovich. "Timing of Proterozoic metamorphism in the southern Curnamona Province: implications for tectonic models and continental reconstructions ∗." Australian Journal of Earth Sciences 54, no. 1 (February 2007): 65–81. http://dx.doi.org/10.1080/08120090600981459.

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16

Clark, Chris, Andreas Schmidt Mumm, and Alan S. Collins. "A coupled micro- and macrostructural approach to the analysis of fluid induced brecciation, Curnamona Province, South Australia." Journal of Structural Geology 28, no. 5 (May 2006): 745–61. http://dx.doi.org/10.1016/j.jsg.2006.01.005.

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17

Heimann, Adriana, Paul G. Spry, Graham S. Teale, Wolfgang R. Leyh, Colin H. H. Conor, Germán Mora, and Joshua J. O'Brien. "Geochemistry and genesis of low-grade metasediment-hosted Zn–Pb–Ag mineralization, southern Proterozoic Curnamona Province, Australia." Journal of Geochemical Exploration 128 (May 2013): 97–116. http://dx.doi.org/10.1016/j.gexplo.2013.02.007.

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18

Rutherford, Lachlan, Martin Hand, and Joanna Mawby. "Delamerian-aged metamorphism in the southern Curnamona Province, Australia: implications for the evolution of the Mesoproterozoic Olarian Orogeny." Terra Nova 18, no. 2 (March 21, 2006): 138–46. http://dx.doi.org/10.1111/j.1365-3121.2006.00673.x.

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19

De Vries Van Leeuwen, Alexander T., Laura J. Morrissey, Tom Raimondo, and Martin Hand. "Prolonged high thermal gradient metamorphism in the Curnamona Province, south-central Australia, during the latter stages of Nuna assembly." Precambrian Research 378 (August 2022): 106775. http://dx.doi.org/10.1016/j.precamres.2022.106775.

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20

Conor, Colin H. H., and Wolfgang V. Preiss. "Understanding the 1720–1640Ma Palaeoproterozoic Willyama Supergroup, Curnamona Province, Southeastern Australia: Implications for tectonics, basin evolution and ore genesis." Precambrian Research 166, no. 1-4 (October 2008): 297–317. http://dx.doi.org/10.1016/j.precamres.2007.08.020.

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21

Armistead, Sheree E., Peter G. Betts, Laurent Ailleres, Robin J. Armit, and Helen A. Williams. "Cu-Au mineralisation in the Curnamona Province, South Australia: A hybrid stratiform genetic model for Mesoproterozoic IOCG systems in Australia." Ore Geology Reviews 94 (March 2018): 104–17. http://dx.doi.org/10.1016/j.oregeorev.2018.01.024.

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22

Barovich, K., and M. Hand. "Tectonic setting and provenance of the Paleoproterozoic Willyama Supergroup, Curnamona Province, Australia: Geochemical and Nd isotopic constraints on contrasting source terrain components." Precambrian Research 166, no. 1-4 (October 2008): 318–37. http://dx.doi.org/10.1016/j.precamres.2007.06.024.

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23

Rutherford, L., K. Barovich, M. Hand, and J. Foden. "Continentalca1.7 – 1.69 Ga Fe-rich metatholeiites in the Curnamona Province, Australia: a record of melting of a heterogeneous, subduction-modified lithospheric mantle." Australian Journal of Earth Sciences 53, no. 3 (June 2006): 501–19. http://dx.doi.org/10.1080/08120090600632466.

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24

Page, R. W., C. H. H. Conor, B. P. J. Stevens, G. M. Gibson, W. V. Preiss, and P. N. Southgate. "Correlation of Olary and Broken Hill Domains, Curnamona Province: Possible Relationship to Mount Isa and Other North Australian Pb-Zn-Ag-Bearing Successions." Economic Geology 100, no. 4 (June 1, 2005): 663–76. http://dx.doi.org/10.2113/100.4.663.

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25

Heimann, A., P. G. Spry, G. S. Teale, C. H. H. Conor, and W. R. Leyh. "Geochemistry of Garnet-Rich Rocks in the Southern Curnamona Province, Australia, and Their Genetic Relationship to Broken Hill-Type Pb-Zn-Ag Mineralization." Economic Geology 104, no. 5 (August 1, 2009): 687–712. http://dx.doi.org/10.2113/gsecongeo.104.5.687.

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26

Heimann, Adriana, Paul G. Spry, Graham S. Teale, Colin H. H. Conor, and Norman J. Pearson. "The composition of garnet in garnet-rich rocks in the southern Proterozoic Curnamona Province, Australia: an indicator of the premetamorphic physicochemical conditions of formation." Mineralogy and Petrology 101, no. 1-2 (October 6, 2010): 49–74. http://dx.doi.org/10.1007/s00710-010-0130-x.

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27

Williams, H. A., and P. G. Betts. "Imaging links between lithospheric architecture and surface geology in the Proterozoic Curnamona Province, Australia." Journal of Geophysical Research 112, B7 (July 19, 2007). http://dx.doi.org/10.1029/2007jb004966.

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