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PALEOCHANNEL URANIUM PROSPECTIVITY PALEO CHANNEL URANIUM PROSPECTIVITY AUGUST 2011 SOUTH AUSTRALIA ENERGY SYSTEMS ASSESSMENT SOUTH AUSTRALIA ENERGY SYSTEMS ASSESSMENT PLATE 3.1 ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! (! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! (! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ! ! ! ! ! ! ! ! ! OLARY MARREE HAWKER WHYALLA ARKAROOLA PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA WOOMERA Oban Oak Dam Beverley Billeroo Weekeroo Four Mile Honeymoon Olympic Dam Radium Hill Crocker Well Mount Painter Low High ! ! ! ! PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA 138° 138° 136° 136° 140° 140° 30° 30° 32° 32° Reliability km 0 200 SPENCER GULF ! ! ! ! PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA 138° 138° 136° 136° 140° 140° 30° 30° 32° 32° Driver km 0 200 SPENCER GULF Low High Driver Prospectivity ! ! ! ! PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA 138° 138° 136° 136° 140° 140° 30° 30° 32° 32° Depositional Mechanism km 0 200 SPENCER GULF Low High Depositional Mechanism Prospectivity ! ! ! ! PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA 138° 138° 136° 136° 140° 140° 30° 30° 32° 32° km 0 200 SPENCER GULF Low High Fluid Pathway/Architecture Prospectivity ! ! ! ! PORT PIRIE LEIGH CREEK ROXBY DOWNS PORT AUGUSTA SPENCER GULF 138° 138° 136° 136° 140° 140° 30° 30° 32° 32° Source km 0 200 Low High Source Prospectivity Prospectivity based on sources of uranium, mineralising fluids and other components needed for ore transport. Prospectivity based on favourable lithologies and structures that will enable movement of fluids to the site of ore deposition. Prospectivity based on favourable lithologies and structures to focus fluids and deposit uranium and other metals via physical and/or chemical processes. Prospectivity based on energy gradients that will mobilise sufficient quantities of ore-bearing fluids to the site of deposition. Data coverage displaying geographical data completeness. Note: Data coverage is separate to data confidence. Potential for uranium deposits based on summation and normalisation of mineral system parameters shown in inserts. See text for more information and references. Sandstone hosted Uranium Prospectivity SPENCER GULF Transverse Mercator Projection; Central Meridian 138 o E; Geocentric Datum of Australia (GDA94) km 0 200 100 Energy Assessment Prospectivity The uranium system assessment is a function of four key mineral system components a) source, b) driver, c) fluid pathway/architecture, and (d) depositional mechanism. Each mineral system component is comprised of a varying number of inputs specific to the targeted mineral system assessment. This assessment is confined to Cenozoic basins. Source Potential for sources of uranium and other metals, mineralising fluids and other components needed for ore transport. The source weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Presence of uranium-rich rocks as determined from radiometric imagery Driver Prospectivity based on energy gradients that will mobilise sufficient quantities of ore-bearing fluids to the site of deposition. The driver weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Topographic slope in basement as derived from 9 second DEM and buffered into Cenozoic basins Fluid Pathway/Architecture Potential for favourable lithologies and structures that will enable movement of fluids to the site of ore deposition. The fluid pathway/architecture weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Distribution of Cenozoic basins 2) Distribution of regional paleochannels 3) Distribution of detailed paleochannels Depositional Mechanism Potential for favourable lithologies and structures to focus fluids and deposit uranium and other metals via physical and/or chemical processes. The depositional mechanism weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Distribution of redox gradients in groundwater 2) Distribution of pH gradients in groundwater 3) Location of EC anomalies in groundwater 4) Presence of Uranium rich sediments derived from radiometric imagery 5) Distribution of coal - and petroleum-bearing basins Reliability Index Data coverage displaying geographical data completeness. Note: Data coverage is separate to data confidence. 138°00' 138°00' 136°30' 136°30' 139°30' 139°30' 30°00' 30°00' 31°00' 31°00' 32°00' 32°00' 33°00' 33°00' SOUTH AUSTRALIA WESTERN AUSTRALIA NORTHERN TERRITORY QUEENSLAND NEW SOUTH WALES VICTORIA TASMANIA ACT MAP LOCALITY Fluid Pathway/Architecture Prospectivity Assessment Workflow Mappable Criteria System Assessment System Component Uranium System Assessment Source Input 1 Input 1 Input 1 2 3 Input 1 2 3 4 5 Driver Fluid Pathway/ Architecture Depostional Mechanism Compiled by S.E. van der Wielen, Geoscience Australia Data analysis by S.E. van der Wielen and D.L. Huston Geoprocessing and Cartography by D.P. Connolly Produced by GIS Services Group, Onshore Energy and Minerals Division, Geoscience Australia. This map forms part of Geoscience Australia’s Onshore Energy Security Program It is recommended that this map be referred to as: van der Wielen S.E., Connolly D.P., 2011. Paleo Channel Uranium Prospectivity. In: Huston D.L and van der Wielen S.E. (editor), 2011. South Australia, Energy Assessment. Geoscience Australia, Canberra, GA Record 2011/34. Geocat # 72666. ISBN web 978-1-921954-38-2, ISBN hardcopy 978-1-921954-37-5. Published by Geoscience Australia, Department of Resources, Energy and Tourism, Canberra, Australia. Issued under the authority of the Minister for Resources, Energy and Tourism © Commonwealth of Australia (Geoscience Australia) 2011 With the exception of the Commonwealth Coat of Arms and where otherwise noted, all material in this publication is provided under a Creative Commons Attribution 3.0 Australia Licence (http://creativecommons.org/licenses/by/3.0/au/) Copies of the GA Record containing this map can be downloaded from the Geoscience Australia internet site at: http://www.ga.gov.au or by contacting: Sales Centre, Geoscience Australia GPO Box 378 Canberra ACT 2601 Phone (02) 6249 9966, Facsimile (02) 6249 9960 Email: [email protected] Data used in system components Highway Data used in final assessment Uranium deposit Uranium occurrence ! ( ! ( Mesozoic and Cenozoic basin boundary

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PALEOCHANNEL URANIUM PROSPECTIVITY

PALEO CHANNEL URANIUMPROSPECTIVITY

AUGUST 2011

SOUTH AUSTRALIA ENERGY SYSTEMS ASSESSMENT

SOUTH AUSTRALIA ENERGY SYSTEMS ASSESSMENT

PLATE 3.1

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OLARY

MARREE

HAWKER

WHYALLA

ARKAROOLA

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

WOOMERA Oban

Oak Dam

Beverley

Billeroo

Weekeroo

Four Mile

Honeymoon

Olympic Dam

Radium Hill

Crocker Well

Mount Painter

Low High

!

!

!

!

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

138°

138°

136°

136°

140°

140°

30° 30°

32° 32°

Reliability

km0 200

SPENCER GULF

!

!

!

!

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

138°

138°

136°

136°

140°

140°

30° 30°

32° 32°

Driver

km0 200

SPENCER GULF

Low HighDriver Prospectivity

!

!

!

!

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

138°

138°

136°

136°

140°

140°

30° 30°

32° 32°

Depositional Mechanism

km0 200

SPENCER GULF

Low HighDepositional Mechanism Prospectivity

!

!

!

!

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

138°

138°

136°

136°

140°

140°

30° 30°

32° 32°

km0 200

SPENCER GULF

Low HighFluid Pathway/Architecture Prospectivity

!

!

!

!

PORT PIRIE

LEIGH CREEK

ROXBY DOWNS

PORT AUGUSTA

SPENCER GULF

138°

138°

136°

136°

140°

140°

30° 30°

32° 32°

Source

km0 200 Low HighSource Prospectivity

Prospectivity based on sources of uranium, mineralising fluids and other components needed for oretransport.

Prospectivity based on favourable lithologies and structures that will enable movement of fluids to the siteof ore deposition.

Prospectivity based on favourable lithologies and structures to focus fluids and deposit uranium and othermetals via physical and/or chemical processes.

Prospectivity based on energy gradients that will mobilise sufficient quantities of ore-bearing fluids to thesite of deposition.

Data coverage displaying geographical data completeness. Note: Data coverage is separate to dataconfidence.

Potential for uranium deposits based on summationand normalisation of mineral system parameters shown ininserts. See text for more information and references.

Sandstone hosted Uranium Prospectivity

SPENCER GULF

Transverse Mercator Projection; Central Meridian 138o E; Geocentric Datum of Australia (GDA94)

km0 200100

Energy Assessment ProspectivityThe uranium system assessment is a function of four key mineral system components a) source, b)driver, c) fluid pathway/architecture, and (d) depositional mechanism. Each mineral system componentis comprised of a varying number of inputs specific to the targeted mineral system assessment. Thisassessment is confined to Cenozoic basins. Source Potential for sources of uranium and other metals, mineralising fluids and other components needed for ore transport. The source weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Presence of uranium-rich rocks as determined from radiometric imagery Driver Prospectivity based on energy gradients that will mobilise sufficient quantities of ore-bearing fluids to the site of deposition. The driver weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Topographic slope in basement as derived from 9 second DEM and buffered into Cenozoic basins Fluid Pathway/Architecture Potential for favourable lithologies and structures that will enable movement of fluids to the site of ore deposition. The fluid pathway/architecture weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Distribution of Cenozoic basins 2) Distribution of regional paleochannels 3) Distribution of detailed paleochannels Depositional Mechanism Potential for favourable lithologies and structures to focus fluids and deposit uranium and other metals via physical and/or chemical processes. The depositional mechanism weighting is calculated by combining the constituent mappable criteria listed below and normalised to the total number of mappable criteria. The input data are: 1) Distribution of redox gradients in groundwater 2) Distribution of pH gradients in groundwater 3) Location of EC anomalies in groundwater 4) Presence of Uranium rich sediments derived from radiometric imagery 5) Distribution of coal - and petroleum-bearing basinsReliability IndexData coverage displaying geographical data completeness. Note: Data coverage is separate todata confidence.

138°00'

138°00'

136°30'

136°30'

139°30'

139°30'

30°00' 30°00'

31°00' 31°00'

32°00' 32°00'

33°00' 33°00'

SOUTHAUSTRALIA

WESTERNAUSTRALIA

NORTHERNTERRITORY

QUEENSLAND

NEW SOUTHWALES

VICTORIA

TASMANIA

ACT

MAP LOCALITY

Fluid Pathway/Architecture

Prospectivity Assessment Workflow

MappableCriteria

SystemAssessment

SystemComponent

Uranium SystemAssessment

Source Fluid Pathway/Architecture

DepositionalMechanism Driver

Input1

Input1

Input1 2 3

Input1 2 3 4 5

Driver Fluid Pathway/Architecture

DepostionalMechanism

Compiled by S.E. van der Wielen, Geoscience AustraliaData analysis by S.E. van der Wielen and D.L. HustonGeoprocessing and Cartography by D.P. ConnollyProduced by GIS Services Group, Onshore Energy and Minerals Division, Geoscience Australia.This map forms part of Geoscience Australia’s Onshore Energy Security ProgramIt is recommended that this map be referred to as: van der Wielen S.E., Connolly D.P., 2011. PaleoChannel Uranium Prospectivity. In: Huston D.L and van der Wielen S.E. (editor), 2011. South Australia,Energy Assessment. Geoscience Australia, Canberra, GA Record 2011/34. Geocat # 72666.ISBN web 978-1-921954-38-2, ISBN hardcopy 978-1-921954-37-5.Published by Geoscience Australia, Department of Resources, Energy and Tourism, Canberra,Australia. Issued under the authority of the Minister for Resources, Energy and Tourism © Commonwealth of Australia (Geoscience Australia) 2011With the exception of the Commonwealth Coat of Arms and where otherwise noted, all material in thispublication is provided under a Creative Commons Attribution 3.0 Australia Licence(http://creativecommons.org/licenses/by/3.0/au/)Copies of the GA Record containing this map can be downloaded from the Geoscience Australia internetsite at: http://www.ga.gov.au or by contacting: Sales Centre, Geoscience Australia GPO Box 378 Canberra ACT 2601 Phone (02) 6249 9966, Facsimile (02) 6249 9960 Email: [email protected]

Data used insystem componentsHighway Data used in

final assessment

Uranium depositUranium occurrence!(

!(

Mesozoic and Cenozoicbasin boundary