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Uranium ore-forming systems of the - Geoscience Australia

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<strong>Uranium</strong> <strong>ore</strong>-<strong>forming</strong> <strong>systems</strong> <strong>of</strong> <strong>the</strong> Lake Frome region1000(A)9900.4 YEARSPaleo fluid-flow model at ~ 6Ma1000(C)9900.4 YEARS5000log_permeability: -17 -16 -15 -14 -13WillawortinaFormation5000Darcy_flux: 1.2E-08 4.8E-08 8.4E-08 1.2E-07Y-500-1000MtPainterNamba Formation-500Eyre FormationY-1000-1500-1500-2000ParalanaFLTZ-20000 10000 20000X0 10000 20000X1000500(B)9900.4 YEARST (oC): 25 50 75 100 125 150 175 2001000500(D)9900.4 YEARStracer: 5 10 15 20 25 30 35 4000Y-500-500-1000Y-1000-1500-1500-20000 10000 20000X-20000 10000 20000XFigure 7.4: Paleo fluid-flow Post-Paralana Fault reference model. A – distribution <strong>of</strong> <strong>the</strong> assigned permeabilities; B – distribution <strong>of</strong> temperature; C – Darcy fluxes andvectors; D – distribution <strong>of</strong> <strong>the</strong> tracer. A, B, and D show fluid flow lines. The red box in (C) outlines <strong>the</strong> area <strong>of</strong> <strong>the</strong> maximal fluid flow that is pertinent for all <strong>the</strong> subsequentfigures. The model does not represent <strong>the</strong> present-day hydrogeological regime in areas proximal to <strong>the</strong> Four Mile and Beverley deposits.Page 90 <strong>of</strong> 151

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