STRUCTURAL AND STRATIGRAPHIC ARCHITECTURE OF AUSTRALIA S FRONTIER ONSHORE SEDIMENTARY BASINS: THE ARCKARINGA, OFFICER, AMADEUS, AND GEORGINA BASINS

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STRUCTURAL AND STRATIGRAPHIC ARCHITECTURE OF AUSTRALIA S FRONTIER ONSHORE SEDIMENTARY BASINS: THE ARCKARINGA, OFFICER, AMADEUS, AND GEORGINA BASINS L.K. Carr 1, R.J. Korsch 1, W.V. Preiss 2, S. A. Menpes 2, J. Holzschuh 1 and R.D. Costelloe 1. 1 Geoscience Australia, 2 Primary Industries and Resources South Australia (PIRSA)

Onshore Energy Security Program 5 year program established in 2006 Precompetitive geoscience data and assessments on petroleum, geothermal & uranium New deep seismic reflection data across frontier basins to document basin architecture, internal geometries Assess resource potential

Arckaringa Basin Seismic line 08GA-OM1 Detailed interpretation available in: Geoscience Australia Record 2010/39

Arckaringa Basin Permian Stratigraphy Permian coal and hydrocarbon system After Pirsa: http://www.pir.sa.gov.au/ data/assets/pdf_file/0006/26907/prospectivity_arckaringa.pdf

Arckaringa Basin West Trough V:H 2:1

Arckaringa Basin

Officer Basin Seismic line 08GA-OM1 Officer Basin MOORILYANNA GRABEN Moorilyanna Graben Detailed interpretation available in Geoscience Australia Record 2010/39

Officer Basin - Stratigraphy 2 Cambrian hydrocarbon systems 2 Neoproterozoic hydrocarbon systems http://www.pir.sa.gov.au/ data/assets/ pdf_file/0019/26911/prospectivity_office r.pdf

Officer Basin full line

Officer Basin Southern Section V:H=2:1

Officer Basin Northern Section V:H=2:1

Amadeus and Georgina Basins Amadeus Basin Imaged on two seismic lines Shale gas study

Results of Preliminary Shale Gas Analysis Amadeus Basin: TOC = 3.16-3.42% (HVSlt) and HI =62-353 mg/g TOC Georgina Basin: TOC = 9.04-15.8% (Mid C Shale) and HI=~600mg/g TOC Both basins have high potential for gas shale Geoscience Australia Record 2011/10 (available at booth) http://www.ga.gov.au/energy

Amadeus Basin 09GA-GA1 (Georgina- Arunta) seismic line; two sections 08GA-OM1 (GOMA) seismic line Neoproterozoic to Devonian Oil and gas producing basin Exploration from 1950s Heavitree Quartzite

Amadeus Basin - Stratigraphy Source: Beck L, 2002. The Amadeus Basin, Northern Territory Australia. Northern Territory Geological Survey, Record 2002-002.

Amadeus Basin - South of Casey Inlier Flat lying sediments with no growth strike section?

Amadeus Basin - North of Casey Inlier Northeastern margin of basin Only Neoproterozoic succession preserved South-directed shortening Basement-cored nappe Basement nappe

GOMA Seismic Line (08GA-OM1) Sparse basement outcrop Cenozoic and Mesozoic cover Geological control limited

outh Amadeus Basin GOMA 08GA-OM1 Basement Basement nappe Basin North Neoproterozoic Devonian Amadeus Basin - southern margin GOMA data available from GA web page Geoscience Australia Record 2010/39

Amadeus Basin Photos Neoproterozoic Heavitree FM, Heavitree Gap Neoproterozoic Cyclops Member, Pertatataka FM Neoproterozoic Julie FM Structural Cambrian and Shannon Stratigraphic FM Architecture of Australian Amadeus Basin

Georgina Basin Neoproterozoic to Devonian Poorly exposed in vicinity of seismic line Exploration from 1950s Phillip 2 well located near the deepest part of seismic section

Georgina Basin - Stratigraphy Several Cambrian Petroleum System Source: Ambrose, 2002. The Georgina Basin, Northern Territory Australia. Northern Territory Geological Survey, Record 2002-002.

Phillip 2 Well Used to control stratigraphy 1489 m to basement (granite) 1802 ± 6 Ma (U-Pb zircon SHRIMP age, Kositcin et al., in prep.) + + + + + + + Frontier Onshore + Sedimentary Basins, APPEA 2011 +

Georgina Basin Phillip 2 + + + + + + + V:H= 3:1

Georgina Basin Dulcie Syncline Phillip 2 1 Second Two-Way-Time 1 Second Two-Way-Time

Georgina Basin - Outcrop Photos Devonian Dulcie Sandstone Cambrian Chabalowe Formation Cambrian Arthur Creek Formation Cambro-Ordovician Tomahawk Formation

Conclusion Deep seismic reflection profiles across several frontier sedimentary basins, collected as part of the OESP, provide new information on basin architecture and internal geometries Geometries will form basis for ongoing work to assess the petroleum potential of these basins http://www.ga.gov.au/energy

Thankyou