Predictive mineral discovery is concerned with the application of a whole of system process understanding to mineral exploration as opposed to an empirical deposit type approach. A mineral system process understanding can be derived from a consideration of five key questions, namely what is/are the: 1) geodynamic setting; 2) architecture; 3) sources and reservoirs; 4) drivers and pathways, and; 5) depositional mechanisms. The answers to these questions result in the identification of critical processes necessary for the function of a mineral system within a particular terrane, and permit the development of a targeting model. In this contribution we identify district scale critical orogenic gold mineral system processes for the late Archaean eastern Yilgarn Craton of Western Australia. During the geodynamic history of a terrane the critical processes which result in mineralisation change with time resulting in variations in mineralisation style. Proxies for critical processes have been mapped in an integrated GIS and are termed mappable mineral system process proxies (or MMSPP). In recognition of this, three separate time slices and a geochemical theme were analysed. Each MMSPP is given a weighting factor (WF) which reflects the spatial accuracy/coverage of the data and process criticality. For each theme/time-slice, a separate prospectivity map was created by summing the overlay or union of the spatial extent of each MMSPP, and adding the WF. A final target or prospectivity map was generated by a union of the four theme/time-slice prospectivity maps, and is tested against the known major deposits. The map 'discovered' the main gold camps and accounts for over 75% of the known gold in 5% of the area. This test verifies the process-based understanding and the appropriate mapping of the critical proxies. A further outcome from the map was the identification of a number of new target areas not known for significant gold mineralisation in what otherwise is thought to represent a mature terrane for gold exploration. The approach taken here has been to consider the Late Archaean gold deposits as a holistic system. Despite the recurring areas of uncertainty, this systems view has resulted in new findings that have generic applications to other mineral systems.

Fluids overview presentation

Cleverley J.S & Oliver N.H.S, 2004. Geochemical models (and preliminary geophysical correlations) pertinent to magmatic contriubtions to ore system hydrology at Wallaby & elsewhere in the Yilgarn

Cleverley J.S. & Olver N.H.S., 2005. JCU/EGRU/CRC Masters Program at JCU. Geochemical Modelling

Fisher, L., 2005. Fluid inclusion compositions and conditions at Osborne; preliminary results.

Mustard, R., Mark, G., Ulrich, T., Foster, D., and Gillen, D., 2005. Geochemsitry of magmatic fluids from intrusions in the Williams-Naraku batholith, Cloncurry district, NW Queensland: preliminary results from laser ablation ICPMS analysis.

Annual Review Nov 2003

H4 - Yilgarn delivery workshop Nov 2005

H4 - Barossa Presentation 2004

H4 - Mt Isa Workshop