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Fracture control of bleaching, Salt Anticline, Utah

PARADOX BASIN – UTAH (Thorson Model) • MULTIPLE FLUID EVENTS NECESSARY FOR DEPOSIT FORMATION • 1 sT STAGE - Diagenetic Fluids Form Iron Oxides – “RED BEDS” • 2 nd STAGE - Reducing Fluids “Prepare” host sandstone by converting hematite to pyrite , hydrocarbons important as source of reductant • 3 rd STAGE - Epigenetic Cu-Bearing saline fluids introduced along structural feeder zones. Ppt Cu on contact with reductants in “Grey Beds”

Page 1 and 2: Sediment-hosted Copper Exploration
Page 3 and 4: Cu Mining in South Australia - a br
Page 5 and 6: Sedimentary-Cu deposits; SUB-TYPES
Page 7 and 8: Thorson, 2008
Page 9: Thorson, 2008
Page 13 and 14: Broad Scale Alteration — Bleachin
Page 15 and 16: AFB B - SIGNS of SSC MINERALISATION
Page 17: TARGET SELECTION • BREACHED ANTIC

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