Basin architecture and evolution in the Mount Isa mineral province,northern Australia: Constraints from deep seismic reflection profiling and implications for ore genesis |
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| Institution: | 1. Geoscience Australia, Canberra, ACT 2601, Australia;2. Research School of Earth Sciences, Australian National University, Canberra 2601, Australia;3. Geological Survey of Queensland, Brisbane, Australia;1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;2. Open Laboratory of Orogenic and Crustal Evolution, Peking University, Beijing 100871, China;3. Henan Provincial Non-ferrous Metals Geological and Mineral Resources Bureau, Zhengzhou 450016, China;1. Centre for Exploration Targeting, The University of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, Australia;2. Economic Geology Research Centre, James Cook University, Townsville, Queensland 4814 Australia;3. Geological Survey of Western Australia, 100 Plain Street, East Perth, WA 6004, Australia;4. Geology Department, Ministry of Mineral Resources, Imaneq 1A 201, 3900 Nuuk, Greenland;1. CSIRO Mineral Resources, Australian Resources Research Centre, 26 Dick Perry Avenue, Kensington, WA 6151, Australia;2. Armour Energy Limited, Level 27, 111 Eagle Street, Brisbane, QLD 4000, Australia;1. CSIRO Mineral Resources, 26 Dick Perry Avenue, Kensington WA 6151, Australia;2. Geology Department, Faculty of Science, Cairo University, Giza 12613, Egypt;3. School of Geography, Environment and Earth Science, Victoria University of Wellington, PO Box 600, Wellington, New Zealand;4. CST Minerals Lady Annie Pty. Ltd., PO Box 2029, Mount Isa, QLD, 4825, Australia |
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| Abstract: | Deep seismic reflection profiling confirms that the Paleo- to Mesoproterozoic Mount Isa mineral province comprises three vertically stacked and partially inverted sedimentary basins preserving a record of intracontinental rifting followed by passive margin formation. Passive margin conditions were established no later than 1655 Ma before being interrupted by plate convergence, crustal shortening and basin-wide inversion at 1640 Ma in both the 1730–1640 Ma Calvert and 1790–1740 Ma Leichhardt superbasins. Crustal extension and thinning resumed after 1640 Ma with formation of the 1635–1575 Ma Isa Superbasin and continued up to ca. 1615 Ma when extensional faulting ceased and a further episode of basin inversion commenced. The 1575 Ma Century Pb–Zn ore-body is hosted by syn-inversion sediments deposited during the initial stages of the Isan Orogeny with basin inversion accommodated on east- or northeast-dipping reactivated intrabasinal extensional faults and footwall shortcut thrusts. These structures extend to considerable depths and served as fluid conduits during basin inversion, tapping thick syn-rift sequences of immature siliciclastic sediments floored by bimodal volcanic sequences from which the bulk of metals and mineralising fluids are thought to have been sourced. Basin inversion and fluid expulsion at this stage were entirely submarine consistent with a syn-sedimentary to early diagenetic origin for Pb–Zn mineralisation at, or close to, the seafloor. Farther east, a change from platform carbonates to deeper water continental slope deposits (Kuridala and Soldiers Cap groups) marks the position of the original shelf break along which the north–south-striking Selwyn-Mount Dore structural corridor developed. This corridor served as a locus for strain partitioning, fluid flow and iron oxide–copper–gold mineralisation during and subsequent to the onset of basin inversion and peak metamorphism in the Isan Orogeny at 1585 Ma. An episode of post-orogenic strike-slip faulting and hydrothermal alteration associated with the subvertical Cloncurry Fault Zone overprints west- to southwest-dipping shear zones that extend beneath the Cannington Pb–Zn deposit and are antithetic to inverted extensional faults farther west in the same sub-basin. Successive episodes of basin inversion and mineralisation were driven by changes in the external stress field and related plate tectonic environment as evidenced by a corresponding match to bends in the polar wander path for northern Australia. An analogous passive margin setting has been described for Pb–Zn mineralisation in the Paleozoic Selwyn Basin of western Canada. |
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