Mineral Systems in the Mount Isa Inlier

Northwest Queensland contains several world class mineral deposits, being one of the worlds leading producers of Zn, Pb, Cu and Ag. Rather than focus on mineral deposit models, as has been done in the past, we are using the mineral system approach (Barnicoat, 2008), where the whole system is studied at a variety of scales and a variety of processes, which culminate in the deposition of mineralisation. Seven Mineral Systems are identified, namely: 1. Shale/siltstone/dolomite hosted Zn-Pb-Ag systems - Western Fold Belt. 2. Ag-Pb-Zn in high-grade metamorphic terrains - Eastern Fold Belt Province. 3. Structurally-controlled epigenetic iron oxide-Cu-Au - Eastern Fold Belt and Kalkadoon-Ewen Provinces. 4. Structurally-controlled epigenetic Cu±Au mineralising system - Western Fold Belt Province. 5. Phosphate Mineralisation in the basal Georgina Basin sequence. 6. U and Rare Earth element (REE) mineralisation. 7. Fe Ore - South Nicholson Group.

[1]  P. Henson,et al.  Paleoproterozoic–earliest Mesoproterozoic basin evolution in the Mount Isa region, northern Australia and implications for reconstructions of the Nuna and Rodinia supercontinents , 2012 .

[2]  Klaus Gessner,et al.  Mineral system analysis of the Mt Isa–McArthur River region, Northern Australia , 2011 .

[3]  M. Hitzman,et al.  A New Geochronological Framework for Mineralization and Alteration in the Selwyn-Mount Dore Corridor, Eastern Fold Belt, Mount Isa Inlier, Australia: Genetic Implications for Iron Oxide Copper-Gold Deposits , 2011 .

[4]  N. Oliver,et al.  Distinguishing basinal- and magmatic-hydrothermal IOCG deposits, Cloncurry District, Northern Australia , 2010 .

[5]  D. Groves,et al.  RECOGNITION OF THE HYDROTHERMAL FEEDER TO THE STRUCTURALLY INVERTED, GIANT BROKEN HILL DEPOSIT, NEW SOUTH WALES, AUSTRALIA , 2008 .

[6]  M. Kendrick,et al.  Noble gas and halogen constraints on mineralizing fluids of metamorphic versus surficial origin: Mt Isa, Australia , 2006 .

[7]  V. Wall Unconformity-related uranium systems: Downunder and over the top , 2006 .

[8]  Peter A. Jones,et al.  A geochemical process model for the Mount Isa copper orebodies , 2006 .

[9]  M. Jackson,et al.  The Role of Sandstone Diagenesis and Aquifer Evolution in the Formation of Uranium and Zinc-Lead Deposits, Southern McArthur Basin, Northern Territory, Australia , 2006 .

[10]  L. Wyborn,et al.  Australian Zn-Pb-Ag Ore-Forming Systems: A Review and Analysis , 2006 .

[11]  Geordie Mark,et al.  Insights into the genesis and diversity of epigenetic Cu – Au mineralisation in the Cloncurry district, Mt Isa Inlier, northwest Queensland , 2006 .

[12]  T. K. Kyser,et al.  A Paragenetic and Isotopic Study of the Proterozoic Westmoreland Uranium Deposits, Southern McArthur Basin, Northern Territory, Australia , 2005 .

[13]  R. Large,et al.  Stratiform and Strata-Bound Zn-Pb-Ag Deposits in Proterozoic Sedimentary Basins, Northern Australia , 2005 .

[14]  T. Driesner,et al.  Is the Mount Isa copper deposit the product of forced brine convection in the footwall of a major reverse fault , 2004 .

[15]  G. Davidson,et al.  Soldiers Cap Group iron-formations, Mt Isa Inlier, Australia, as windows into the hydrothermal evolution of a base-metal-bearing Proterozoic rift basin , 2004 .

[16]  P. Betts,et al.  Tectonic Environment of Shale-Hosted Massive Sulfide Pb-Zn-Ag Deposits of Proterozoic Northeastern Australia , 2003 .

[17]  Peter G. Betts,et al.  Geodynamically indicated targeting strategy for shale‐hosted massive sulfide Pb–Zn–Ag mineralisation in the Western Fold Belt, Mt Isa terrane , 2002 .

[18]  S. Walters,et al.  Discovery and geology of the Cannington Ag-Pb-Zn Deposit, Mount Isa Eastern Succession, Australia: Development and application of an exploration model for Broken Hill-type deposits , 2002 .

[19]  Shiqi Wang,et al.  Geochemistry and origin of Proterozoic skarns at the Mount Elliott Cu–Au(–Co–Ni) deposit, Cloncurry district, NW Queensland, Australia , 2001 .

[20]  S. Bull,et al.  The Kamarga deposit: a large, low grade, stratabound zinc resource in the Proterozoic 'Carpentaria Zinc Belt' of northern Australia , 1999 .

[21]  L. Wyborn,et al.  Age of Cu‐Au mineralisation, Cloncurry district, eastern Mt Isa Inlier, Queensland, as determined by 40Ar/39Ar dating∗ , 1998 .

[22]  J. Clarke,et al.  Geological setting, paragenesis and fluid history of the Walford Creek Zn‐Pb‐Cu‐Ag prospect, Mt Isa Basin, Australia* , 1998 .

[23]  R. Large,et al.  Proterozoic copper-gold deposits , 1998 .

[24]  R. Large,et al.  Proterozoic stratiform sediment-hosted Zn-Pb-Ag deposits , 1998 .

[25]  D. Berkman,et al.  Geology of Australian and Papua New Guinean mineral deposits , 1998 .

[26]  G. Xu Structural geology of the Dugald River ZnPbAg deposit, Mount Isa Inlier, Australia , 1996 .

[27]  G. Davidson,et al.  Stable isotope evidence for thermochemical sulfate reduction in the Dugald river (Australia) strata-bound shale-hosted zinclead deposit , 1996 .

[28]  Sb Bodon Paragenetic relationships at the Cannington Ag-Pb-Zn deposit, Mt Isa Inlier, northwest Queensland , 1996 .

[29]  T. Mernagh,et al.  Fluid and mass transfer during metabasalt alteration and copper mineralization at Mount Isa, Australia , 1995 .

[30]  Reto M. Burkhalter Ooidal ironstones and ferruginous microbialites: origin and relation to sequence stratigraphy (Aalenian and Bajocian, Swiss Jura mountains) , 1995 .

[31]  D. Singer World Class Base and Precious Metal Deposits A Quantitative Analysis , 1995 .

[32]  D. Groves,et al.  The Geology and Origin of Australia's Mineral Deposits , 1994 .

[33]  C. Heinrich,et al.  Br/Cl geochemistry of hydrothermal brines associated with Proterozoic metasediment-hosted copper mineralization at Mount Isa, northern Australia , 1993 .

[34]  P. Southgate,et al.  Application of sequence stratigraphic concepts to middle cambrian phosphogenesis georgina basin australia , 1991 .

[35]  P. Southgate A model for the development of phosphatic and calcareous lithofacies in the Middle Cambrian Thorntonia Limestone, northeast Georgina Basin, Australia , 1988 .