Academic literature on the topic 'Northern Gawler Craton'

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Journal articles on the topic "Northern Gawler Craton"

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Armit, R., P. G. Betts, B. F. Schaefer, K. Yi, Y. Kim, R. A. Dutch, A. Reid, L. Jagodzinski, D. Giles, and L. Ailleres. "Late Palaeoproterozoic evolution of the buried northern Gawler Craton." Precambrian Research 291 (April 2017): 178–201. http://dx.doi.org/10.1016/j.precamres.2017.01.023.

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Reid, Anthony, and Marnie Forster. "Mesoproterozoic thermal evolution of the northern Gawler Craton from 40Ar/39Ar geochronology." Precambrian Research 358 (June 2021): 106180. http://dx.doi.org/10.1016/j.precamres.2021.106180.

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3

Baines, G., D. Giles, P. Betts, and G. Backe. "Geophysically imaging Paleoproterozoic terrane boundaries in the unexposed northern Gawler Craton, Marla region." ASEG Extended Abstracts 2009, no. 1 (2009): 1. http://dx.doi.org/10.1071/aseg2009ab097.

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4

Payne, Justin L., Karin M. Barovich, and Martin Hand. "Provenance of metasedimentary rocks in the northern Gawler Craton, Australia: Implications for Palaeoproterozoic reconstructions." Precambrian Research 148, no. 3-4 (August 2006): 275–91. http://dx.doi.org/10.1016/j.precamres.2006.05.002.

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Hall, James W., Stijn Glorie, Anthony J. Reid, Samuel C. Boone, Alan S. Collins, and Andrew Gleadow. "An apatite U–Pb thermal history map for the northern Gawler Craton, South Australia." Geoscience Frontiers 9, no. 5 (September 2018): 1293–308. http://dx.doi.org/10.1016/j.gsf.2017.12.010.

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Wise, Tom, Mark Pawley, Stephan Thiel, and Rian Dutch. "Geology, geophysics, geochemistry of a hidden Palaeoproterozoic ocean-continent transition in the northern Gawler Craton." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–5. http://dx.doi.org/10.1071/aseg2018abm3_1g.

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Fomin, T., A. Nakamura, J. Maher, J. Duan, and P. R. Milligan. "Acquisition and processing of seismic reflection, refraction and magnetotelluric data, northern Eyre Peninsula, Gawler Craton." ASEG Extended Abstracts 2010, no. 1 (December 2010): 1–4. http://dx.doi.org/10.1081/22020586.2010.12041957.

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Hall, James W., Stijn Glorie, Anthony J. Reid, Alan S. Collins, Fred Jourdan, Martin Danišík, and Noreen Evans. "Thermal history of the northern Olympic Domain, Gawler Craton; correlations between thermochronometric data and mineralising systems." Gondwana Research 56 (April 2018): 90–104. http://dx.doi.org/10.1016/j.gr.2018.01.001.

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Tiddy, Caroline J., Peter G. Betts, Mitchell R. Neumann, Finbarr C. Murphy, John Stewart, David Giles, Mick Sawyer, Hamish Freeman, and Fred Jourdan. "Interpretation of a ca. 1600–1580 Ma metamorphic core complex in the northern Gawler Craton, Australia." Gondwana Research 85 (September 2020): 263–90. http://dx.doi.org/10.1016/j.gr.2020.04.008.

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Betts, Peter G., Rick K. Valenta, and Jim Finlay. "Evolution of the Mount Woods Inlier, northern Gawler Craton, Southern Australia: an integrated structural and aeromagnetic analysis." Tectonophysics 366, no. 1-2 (May 2003): 83–111. http://dx.doi.org/10.1016/s0040-1951(03)00062-3.

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Dissertations / Theses on the topic "Northern Gawler Craton"

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Reddy, M. C. "Low-temperature thermochronologic insight into the exhumation of the Northern Gawler craton (South Australia)." Thesis, 2014. http://hdl.handle.net/2440/110559.

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The Gawler Craton (South Australia) records a complex thermal history during the Phanerozoic. Previous work has indicated that the central Gawler Craton was largely exhumed during the Carboniferous as a far-field effect of the Alice Springs Orogeny. Besides this widespread exhumation event, localised Mesozoic and Tertiary thermal events have been documented for the central Gawler Craton as well. The extent of these events into the northern Gawler Craton is not well understood as low-temperature thermochronological data is lacking for this region. For this study, granitoid samples along a roughly north-south transect through the northern and central Gawler Craton were analysed using the apatite fission track (AFT) and apatite (AHe) and zircon (ZHe) U-Th-Sm/He methods. Results from these low-temperature methods yield Neoproterozoic through to Cretaceous AFT, AHe and ZHe ages. Cumulative AFT age plots reveal a multi-phase Phanerozoic cooling history for the central and northern Gawler Craton. Significant AFT age peaks were found at ~480-450 Ma and ~350-300 Ma. The Ordovician age peak is thought to be related with the final stages of the Delamerian Orogeny, while the Carboniferous age peak is interpreted as being a far field response to the Alice Springs Orogeny. This is consistent with previous interpretations throughout South Australia. Additionally, localised Jurassic and Cretaceous AFT and ZHe ages were obtained which are thought to be related with rifting at the southern Australian margin and river incision respectively.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2014
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2

Owen, N. D. "Characteristics of K-Fe alteration in relation to IOCG(U) mineralisation in the northern Yorke Peninsula." Thesis, 2015. http://hdl.handle.net/2440/118209.

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The Moonta-Wallaroo area in the Northern Yorke Peninsula (NYP) is inferred to have been associated with the major deformation, metamorphic and magmatic event at ca. 1600-1575 Ma that affected much of eastern Proterozoic Australia. Widespread K-Fe (biotite-magnetite) alteration is genetically linked with the main pyrite ±chalcopyrite mineralising event within the Doora Member of the Wandearah Formation. Zones of high mineralisation were seen to correspond with coarsening grain size of biotite in petrological and hand samples and were supported by geochemical trends between Fe2O3, S and Cu. Later stage hematite bearing phases of alteration resulted in intense alteration and pyrite-chalcopyrite mineralisation locally within carbonate bearing zones. It is suggested that uranium enrichment is also associated with biotite-magnetite alteration but was later stripped from the highly mineralised zones by less pervasive hydrothermal fluids. U-Pb isotope analysis of zircon grains constrain the age of formation of the basement in which mineralisation occurs. The Moonta Porphyry revealed an age of 1752 ±6Ma. Based on its interdigitising relationship with the Moonta Porphyry a maximum age of sedimentation of the Doora Member is proposed at ca. 1752 Ma. The protolithic material of the Harlequin Stone was determined to be similar to that of the Doora Member and was sourced mainly from the ca. 1850 Ma Donington Suite Granitoids. A Pb207/Pb206 age of ca. 1708 Ma suggests a wider age of formation of the Wallaroo Group than previously reported in the literature. Alteration within the Oorlano Metasomatite metasediment samples showed a clear deviation in chemical characteristics from the Doora Member suggesting different styles of alteration in relation to their proximity to the Arthurton and Tickera Granites.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
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