oa Geophysical vectors to IOCG mineralisation in the Gawler Craton

References

1. Austin, J., Foss, C., 2012, Rich, attractive and extremely dense: A geophysical review of Australian IOCGs, ASEG Extended Abstracts 2012 , 1-4.
2. Bastrakov, E.N., Skirrow, R.G. and Davidson, G.J., 2007, Fluid evolution and origins of iron oxide Cu-Au prospects in the Olympic Dam district, Gawler craton, South Australia; conomic Geology, v. 102, 1415-1440.
3. Belperio, A., Flint, R. and Freeman, H., 2007 - Prominent Hill: A Hematite-Dominated, Iron Oxide Cu-Au System; Economic Geology, v. 102, 1499-1510
4. Davidson, G.J., Paterson, H., Meffre, S. and Berry, R.F., 2007, Characteristics and origin of the Oak Dam East breccia- hosted, iron oxide-Cu-U-(Au) deposit: Olympic Dam region, Gawler craton, South Australia; Economic Geology, v. 102, 1471-1498
5. Drexel, J.F., Preiss, W.V. and Parker, A.J., 1993, The Geology of South Australia, Vol 1, The Precambrian, South Australia, Geological Survey, Bulletin 54.
6. Esdale, D., Pridmore, D.F., Fritz, F., Muir, P., Williams, P., Coggon, J., (2003) The Olympic Dam copper-uranium-gold- silver-rare earth element deposit, South Australia: A geophysical case history.ASEG Extended Abstracts 2003 , 147-168.
7. Gow, P. A., Wall, V. J., and Valenta, R. K., 1993, The regional geophysical response of the Stuart Shelf, South Australia: Exploration Geophysics, v. 24, 513-520.
8. Groves, D.I., Bierlein, F.P., Meinert, L.D. and Hitzman, W.M, 2010, Iron Oxide Copper-Gold (IOCG) Deposits through Earth History: Implications for Origin, Lithospheric Setting, and Distinction from Other Epigenetic Iron Oxide Deposits: Economic Geology, 105, 641-654.
9. Harris, T.M., Funk, C.W., Murphy, F.C., Betts, P.G., submitted, Mt Woods 2D Seismic Reflection Survey, Gawler Craton, South Australia: An Integrated Minerals Exploration Case Study. Australian Society of Exploration Geophysicists, Extended Abstract
10. Hart, J. and Freeman, H., 2003, Geophysics of the Prominent Hill prospect, South Australia; in Dentith, M.C., (ed.), Geophysical Signatures of South Australian Mineral Deposits, Australian Society of Exploration Geophysicists, Special Publication 12, 93-100.
11. Heinson, G.S., Direen, N.G., Gill, R.M., 2006, Magnetotelluric evidence for a deep-crustal mineralizing system beneath the Olympic Dam iron oxide copper-gold deposit, southern Australia, Geology. 34(7), 573-576
12. Reynolds, L.J., 2000, Geology of the Olympic Dam Cu-Au- Ag-REE deposit, in Porter, T.M., ed., Hydrothermal iron- oxide copper-gold and related deposits: A global perspective: Adelaide, Australian Mineral Foundation, v. 1, 33-48.
13. Smith, R.S., 2002, Geophysics of Iron-Oxide Copper-Gold Systems, in - Porter, T.M. (Ed), Hydrothermal Iron Oxide Copper-Gold and Related Deposits: A Global Perspective, PGC Publishing, Adelaide, v.2, 357-367.
14. Vella, L., 1997, Interpretation and modelling, based on petrophysical measurements, of the Wirrda Well potential fi eld anomaly, South Australia; Exploration Geophysics, v. 28, 299-306.
15. Vella, L. and Cawood, M., 2012, Geophysical Characteristics of the Carrapateena Iron-Oxide Copper-Gold Deposit, ASEG Extended Abstracts, Vol. 2012 No. 1, 1-4.