Project A1-Abstracts and pubs
Type of resources
Keywords
Publication year
Topics
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Orogenic gold deposits and major fault zones: Targeting tools applied to the Eastern Goldfields, Yilgarn Craton, Western Australia. Mineralium Deposita.
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Deformation history and multiple gold mineralisation events within the Bardoc Tectonic Zone, Eastern Goldfields, Western Australia. In Mao, J., and Bierlein, F.P. (eds.), Mineral Deposit Research: Meeting the Global Challenge, Springer Verlag, Heidelberg.
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Why is the Menzies- Boorara Shear Zone not as well-endowed as the Boulder-Lefroy Shear Zone? In: Muhling, J., Goldfarb, R, Vielreicher, N., Bierlein, F.P., Stumpfl, E, Groves, D.I. and Kenworthy, S., SEG 2004: Predictive Mineral Discovery Under Cover; Extended Abstracts. Centre for Global Metallogeny, The University of Western Australia, Publication No 33, pp. 448.
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Structural and mineralogical characteristics of the Menzies-Boorara Shear Zone, Yilgarn Craton implications for variations in the gold potential of a major fault system. In Barnicoat, A.C., Korsch, R.J. (editors), Predictive Mineral Discovery Cooperative Research Centre - Extended Abstracts from the June 2004 Conference, Geoscience Australia, Record 2004/09, p. 143-146.
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Final progress report for A1 to April 2005.
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Crustal fluids in tectonic evolution and mineral systems: evidence from the Yilgarn Craton. In Barnicoat, A.C., Korsch, R.J. (editors), Predictive Mineral Discovery Cooperative Research Centre - Extended Abstracts from the June 2004 Conference, Geoscience Australia, Record 2004/09, p. 33-37.
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The effects of out-ofplane seismic energy on reflections in crustal-scale 2D seismic sections. Tectonophysics 388: 213-224.
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Mapping fluid pathways using seismic methods. Final report for A1 Project, 6pp.
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The role of crustal fluids in the tectonic evolution of the Eastern Goldfields Province of the Archaean Yilgarn Craton, Western Australia. Earth Planets Space 56: 1163-1169.
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Advanced methodologies for the analysis of databases of mineral deposits and major faults. Australian Journal of Earth Sciences, 55; 79-99.