AUSTRALIA 2013 – Offshore Petroleum Exploration...

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AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release RELEASE AREAS NT13-1, NT13-2 AND NT13-3, NORTHERN PETREL SUB-BASIN AND MALITA GRABEN, BONAPARTE BASIN, NORTHERN TERRITORY Figure 1 Location of the 2013 Release Areas in the northern Petrel Sub-basin and Malita Graben of the Bonaparte Basin HIGHLIGHTS BIDS CLOSE - 22 May 2014 Under-explored gas province, with potential charge from Paleozoic and Mesozoic sources Shallow water depths, 40–200 m Close to the Evans Shoal, Greater Sunrise, Caldita and Barossa gas fields, and Darwin (Wickham Point) LNG plant supplied by the Bayu–Undan gas pipeline Faulted anticlines, tilted fault blocks and stratigraphic traps Special Notices apply, refer to Guidance Notes Release Areas NT13-1, NT13-2 and NT13-3 are located in the northeastern Bonaparte Basin in the Timor Sea. Release Areas NT13-1 and NT13-2 are in the Malita Graben, with NT13-1 also partly overlapping the Darwin Shelf. Release Area NT13-3 is mostly situated in the northern Petrel Sub-basin. Release Areas NT13-1 and NT13-2 are located entirely within the marine reserve Multiple Use Zone (IUCN VI), Oceanic Shoals, and NT13-3 is located partly within this marine reserve. The Malita Graben is a northeast-trending dominantly Mesozoic–Cenozoic depocentre in the northern Bonaparte Basin that lies between the Sahul Platform to the north and the Petrel Sub-basin and Darwin Shelf to the south. The active petroleum system in the region of the Release Areas has been defined as the Jurassic Plover-Plover(.) Petroleum System (Barrett et al, 2004). The active source pod within the Plover Formation is interpreted to extend throughout the Malita Graben and onto the marginal areas of the Sahul Platform (Heron Terrace). Modelling suggests it is gas-prone with moderate liquids, but with little or no oil potential. The southern part of Release Area NT13-3 falls within the gas-prone Permian Hyland Bay/Keyling-Hyland Bay(.) Petroleum System. The main structural plays are broad faulted anticlinal structures over tilted fault blocks at the base of the regional seal. Tilted horst blocks are attractive targets on faulted terraces and stratigraphic traps include pinch-outs and truncations across unconformities. Expanding infrastructure in the region will facilitate development of new discoveries. AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 1 WESTERN AUSTRALIA NORTHERN TERRITORY SOUTH AUSTRALIA QUEENSLAND NEW SOUTH WALES VICTORIA TASMANIA Areas NT13-1 to 3 Bonaparte Basin 12-6769-1

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AUSTRALIA 2013Offshore Petroleum Exploration Acreage Release

RELEASE AREAS NT13-1, NT13-2 AND NT13-3, NORTHERN PETREL SUB-BASIN AND MALITA GRABEN, BONAPARTE BASIN, NORTHERN TERRITORY

Figure 1 Location of the 2013 Release Areas in the northern Petrel Sub-basin and Malita Graben of the Bonaparte Basin

HIGHLIGHTS

BIDS CLOSE - 22 May 2014• Under-explored gas province, with potential

charge from Paleozoic and Mesozoic sources

• Shallow water depths, 40–200 m

• Close to the Evans Shoal, Greater Sunrise, Caldita and Barossa gas fields, and Darwin (Wickham Point) LNG plant supplied by the Bayu–Undan gas pipeline

• Faulted anticlines, tilted fault blocks and stratigraphic traps

• Special Notices apply, refer to Guidance Notes

Release Areas NT13-1, NT13-2 and NT13-3 are located in the northeastern Bonaparte Basin in the Timor Sea. Release Areas NT13-1 and NT13-2 are in the Malita Graben, with NT13-1 also partly overlapping the Darwin Shelf. Release Area NT13-3 is mostly situated in the northern Petrel Sub-basin. Release Areas NT13-1 and NT13-2 are located entirely within the marine reserve Multiple Use Zone (IUCN VI), Oceanic Shoals, and NT13-3 is located partly within this marine reserve.

The Malita Graben is a northeast-trending dominantly Mesozoic–Cenozoic depocentre in the northern Bonaparte Basin that lies between the Sahul Platform to the north and the Petrel Sub-basin and Darwin Shelf to the south. The active petroleum system in the region of the Release Areas has been defined as the Jurassic Plover-Plover(.) Petroleum System (Barrett et al, 2004). The active source pod within the Plover Formation is interpreted to extend throughout the Malita Graben and onto the marginal areas of the Sahul Platform (Heron Terrace). Modelling suggests it is gas-prone with moderate liquids, but with little or no oil potential. The southern part of Release Area NT13-3 falls within the gas-prone Permian Hyland Bay/Keyling-Hyland Bay(.) Petroleum System. The main structural plays are broad faulted anticlinal structures over tilted fault blocks at the base of the regional seal. Tilted horst blocks are attractive targets on faulted terraces and stratigraphic traps include pinch-outs and truncations across unconformities. Expanding infrastructure in the region will facilitate development of new discoveries.

AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 1

WESTERNAUSTRALIA

NORTHERNTERRITORY

SOUTHAUSTRALIA

QUEENSLAND

NEWSOUTHWALES

VICTORIA

TASMANIA

Areas NT13-1 to 3Bonaparte Basin

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AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 2

Figure 2 Structural elements of the Malita Graben, Darwin Shelf and northern Petrel Sub-basin (after West and Passmore, 1994) showing petroleum fields and discoveries, the location of regional cross-sections and the 2013 Release Areas

LYN

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Bathurst Terrace

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Bayu/Undan pipeline

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Jura 1

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AUSTRALIA

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SahulPlatform

MONEY SHOAL BASIN

TroubadourTerrace

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FlamingoSyncline

Sahul Syncline

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NT13-2

NT13-1

Evans ShoalBarossa

Troubadour

Caldita

Evans Shoal South

Gull 1

Fohn 1

Newby 1

Marsi 1

Heron 1, 2

Curlew 1

Beluga 1

Wonarah 1Sikatan 1

Wallaroo 1

Nabarlek 1

Flat Top 1

Durville 1Darwinia 1

Chuditch 1

Schilling 1

Laperouse 1

Kelp Deep 1

Jacaranda 1

Shearwater 1

Blackwood 1

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SA

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NSW

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Well symbol information is sourced either from "open file" data from titleholders where this is publicly available as at 1 December 2012 or from other public sources. Field outlines are provided by EncomGPinfo, a Pitney Bowes Software (PBS) Pty Ltd product. Whilst all care is taken in the compilation of the field outlines by PBS, no warranty is provided re the accuracy or completeness of theinformation, and it is the responsibility of the Customer to ensure, by independent means, that those parts of the information used by it are correct before any reliance is placed on them.

10°

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Petroleum exploration well - Dry holePetroleum exploration well - Gas show

Petroleum exploration well - Not classified

Petroleum exploration well - Gas discoveryPetroleum exploration well - Oil show

2013 Offshore PetroleumAcreage Release Area

Gas field

Mesozoic

Paleozoic

Platform/shelf

FaultHingeBasin outlineSub-basin outlineSeismic lineGas pipelineGas pipeline (proposed)Scheduled area boundary (OPGGSA 2006)

AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 3

Figure 3 Stratigraphy and hydrocarbon discoveries of the Malita Graben and Petrel Sub-basin based on the Bonaparte Basin Biozonation and Stratigraphy Chart (Nicoll et al, 2009). Geologic Time Scale after Gradstein et al (2012)

Age(Ma) Period Epoch Stage Shows

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Ascalon 1A, Tern 3

Torrens 1Tern 2, Tern 3

Turtle 2

Petrel 2Turtle 1Petrel 2, Penguin 1, Polkadot 1

Blacktip 1, Bougainville 1, Tern 2Cambridge 1, Torrens 1Blacktip 1, Polkadot 1

Turtle 2Barnett 1, Shakespeare 1, Turtle 1

Tern 1Turtle 1

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Tern 1, Tern 2Tern 3, Tern 4

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Bashkirian

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Formation equivalent)

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AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 4

Figure 4 AGSO seismic line 116/11 across the Sahul Platform, Malita Graben and Darwin Shelf (AGSO, 2001). Location of the line is shown in Figure 2. Regional seismic horizons are shown in Figure 3

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)NW SEShearwater 1

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Mid Oligocene Late MioceneWater bottom

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12-6769-4Line 116/11

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AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 5

Figure 5 Northern part of AGSO seismic line 100/05 across the Malita Graben and Petrel Sub-basin (AGSO, 2001). Location of the line is shown in Figure 2. Regional seismic horizons are shown in Figure 3

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0 25 km

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Petrel Sub-basinMalita Graben

AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 6

PETROLEUM SYSTEMS ELEMENTS

Northern Petrel Sub-basin and Malita Graben

Sources • Lower–Middle Jurassic fluvio-deltaic Plover Formation (gas-prone)

• Middle–Upper Jurassic deltaic to marine Elang Formation (gas-prone, possible oil)

• Upper Jurassic marine Frigate Shale (gas-prone, possible oil)

• Lower Cretaceous marine Echuca Shoals Formation (oil-prone)

• Permian (Lopingian–Guadalupian) pro-delta, shoreface and open marine Hyland Bay Subgroup (gas-prone)

Reservoirs • Middle–Upper Jurassic deltaic to marine Elang Formation

• Upper Jurassic–Lower Cretaceous marine Sandpiper Sandstone

• Upper Cretaceous marine Wangarlu Formation

• Upper Cretaceous Puffin Formation submarine fans

• Lower–Middle Jurassic fluvio-deltaic Plover Formation

• Permian–Lower Triassic marginal marine Mount Goodwin Subgroup

• Permian shoreface to marine Hyland Bay Subgroup

Seals Regional seals

• Lower Cretaceous marine Echuca Shoals Formation

• Upper Jurassic marine Frigate Shale

• Triassic marine Mount Goodwin SubgroupIntraformational seals

• Lower–Middle Jurassic fluvio-deltaic Plover Formation

Traps • In the Malita Graben large faulted anticlinal structures occur at the base of the Lower Cretaceous regional seal (Barossa, Caldita, Heron, Sunrise).Tilted fault blocks and broad, low-relief anticlinal drape over tilted fault blocks (Evans Shoal and Lynedoch)

• Structural/stratigraphic plays (Beluga)

• On the Bathurst Terrace south of the Malita Graben there are structural play fairways and the possibility of hanging wall fault-dependent trap.

• In the northern Petrel Sub-basin, large-scale inversion anticlines (e.g. Petrel) formed during the Middle-Late Triassic Fitzroy Movement; commonly associated with salt mobilisation, faulted anticlines (Curlew, Gull, Tern, Blacktip and Frigate) and tilted fault blocks (Fishburn)

• Stratigraphic pinch-out plays of Jurassic (Newby) and Permian (Flat Top) sandstones occur at the basin margin

INFRASTRUCTURE AND MARKETSThe 2013 Release Areas are proximal to the Greater Sunrise, Caldita and Barossa gas fields and Darwin (Wickham Point) LNG plant supplied by the Bayu–Undan gas pipeline.

CRITICAL RISKSKey risks in the Release Areas are the lack of a viable oil-prone petroleum system in the central to northern Petrel Deep, since no known liquids-prone source rocks have been intersected, and in the Malita Graben where high geothermal gradients preclude likely generation or preservation of liquid hydrocarbons below about 2.5 km. There are also few suitably sized trap closures for economic gas accumulations. Reservoir quality is variable, with the quality of the Plover Formation sandstones becotming poorer towards the depocentre. Most gas accumulations in the Malita Graben contain high concentrations of non-combustible gases including nitrogen (N2), carbon dioxide (CO2) and hydrogen sulphide (H2S).

AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 7

DATA SETSFor the Wells Data Listing go to http://www.petroleum-acreage.gov.au/2013/support/geo.html

For the Seismic Surveys Listing go to http://www.ga.gov.au/energy/projects/acreage-release-and-promotion/2013.html#data-packages

GEOSCIENCE AUSTRALIA PRODUCTS

Regional Geology and Seismic• Petrel Sub-basin Study 1995–1996: Summary Report. Australian Geological Survey Organisation Record 1996/40.

GEOCAT 22670

• Line Drawings of AGSO – Geoscience Australia’s Regional Seismic Profiles, Offshore Northern and Northwestern Australia, Australian Geological Survey Organisation Record 2001/36. GEOCAT 36353

• Interpreted Horizons and Faults for Seismic Surveys 100, 116 and 118 (2001)—Digital Horizon and Fault Data in ASCII Format. (2001) GEOCAT 35239, 35249 and 35243, respectively.

• Deep Structure of the Eastern Malita Graben and Adjacent Areas in the Timor and Western Arafura Seas: Survey 118 Operational Report. Australian Geological Survey Organisation Record 1993/47. GEOCAT 14645

Stratigraphy• Bonaparte Basin Biozonation and Stratigraphy Chart 33 (2009). GEOCAT 70371

Petroleum Systems and Accumulations• Bonaparte Basin, NT, WA, AC and JPDA, Australian Petroleum Accumulations Report 5, 2nd Edition, (2004).

GEOCAT 60865

• Petroleum Prospectivity of the East Malita Graben Area, Bonaparte Basin Australian Geological Survey Organisation Record 1992/24. GEOCAT 14535

• Light Hydrocarbon Geochemistry of the Bonaparte Basin: Including the Sahul Syncline, Malita Graben and Northern Petrel Sub-basin: Rig Seismic Survey 99: Project 121.24. Australian Geological Survey Organisation Record 1992/50. GEOCAT 14559

• The Petroleum Systems of the Bonaparte Basin. 2004. GEOCAT 61365

• Source Rock Time-slice Maps, Offshore Northwest Australia—1:3,000,000 Scale. (2004). GEOCAT 61179

• Oils of Western Australia II: Regional Petroleum Geochemistry and Correlation of Crude Oils and Condensates from Western Australia and Papua New Guinea, 2005. Geoscience Australia and GeoMark Research. GEOCAT 37512

• Characterisation of Natural Gases from West Australian Basins, Bonaparte Basin Module AGSO and Geotechnical Services non-exclusive study, 2000. GEOCAT 33569

Contact Geoscience Australia’s Sales Centre for more information or to order these reports or products, phone 61 (0)2 6249 9966, email [email protected]

AUSTRALIA 2013 Offshore Petroleum Exploration Acreage Release 8

KEY REFERENCESAGSO, 2001—Line Drawings of AGSO – Geoscience Australia’s Regional Seismic Profiles, Offshore Northern and Northwestern Australia. Australian Geological Survey Organisation Record 2001/36.

AMBROSE, G.J., 2004—Jurassic pre-rift and syn-rift sedimentation in the Bonaparte Basin – new models for reservoir and source rock development. In: Ellis, G.K., Baillie, P.W. and Munson, T.J. (eds), Timor Sea Petroleum Geoscience, Proceedings of the Timor Sea Symposium, Darwin Northern Territory, 19–20 June 2003, 125–142. Northern Territory Geological Survey, Special Publication 1.

ANDERSON, A.D., DURHAM, M.S. AND SUTHERLAND, A.J., 1993—The integration of geology and geophysics to post-well evaluations – example from Beluga-1, offshore northern Australia.

BARBER, P., CARTER, P., FRASER, T., BAILLIE, P.W. AND MYERS, K., 2004—Under-explored Palaeozoic and Mesozoic petroleum systems of the Timor and Arafura seas, northern Australian continental margin. In: Ellis, G.K., Baillie, P.W. and Munson, T.J. (eds), Timor Sea Petroleum Geoscience, Proceedings of the Timor Sea Symposium, Darwin, Northern Territory, 19–20 June 2003, 143–154. Northern Territory Geological Survey, Special Publication 1.

BARRETT, A.G., HINDE, A.L. AND KENNARD, J.M., 2004—Undiscovered resource assessment methodologies and application to the Bonaparte Basin. In: Ellis, G.K., Baillie, P.W. and Munson, T.J. (eds), Timor Sea Petroleum Geoscience, Proceedings of the Timor Sea Symposium, Darwin, 19–20 June 2003. Northern Territory Geological Survey, Special Publication 1, 353–372.

BOYD, R., KRIEGER, F., RYER, M. AND MATHERS, G., 2009—Integrating sedimentology, sequence stratigraphy and ichnology for improved reservoir prediction in the Bayu-Undan Field, Bonaparte Basin, NW Australia. Abstracts: Annual Meeting - American Association of Petroleum Geologists 2009.

KEEP, M., CLOUGH, M. AND LANGHI, L., 2002—Neogene tectonic and structural evolution of the Timor Sea region, NW Australia. In: Keep, M. and Moss, S. (eds), The Sedimentary Basins of Western Australia 3, Proceedings of the Petroleum Exploration Society of Australia Symposium, Perth, 2002, 341–353.

KENNARD, J.M., DEIGHTON, I., EDWARDS, D.S., BOREHAM, C.J. AND BARRETT, A.G., 2002—Subsidence and thermal history modelling: new insights into hydrocarbon expulsion from multiple petroleum systems in the Petrel Sub-basin, Bonaparte Basin. In: Keep, M. and Moss, S. (eds), The Sedimentary Basins of Western Australia 3, Proceedings of the Petroleum Exploration Society of Australia Symposium, Perth, 2002, 409–437.

LONGLEY, I.M., BRADSHAW, M.B. AND HEBBERGER, J., 2002—Australian Petroleum Provinces of the 21st Century. In: Downey, M.W. and Morgan, W.A. (eds), Petroleum Provinces of the Twenty-First Century, American Association of Petroleum Geologists Memoir, 74, 287–317.

LOWE, Y.B.S., RUTLEY, D., SPICER, R.D. AND KLOSS, O., 2004—The Evans Shoal Field, northern Bonaparte Basin. In: Ellis, G.K., Baillie P.W. and Munson, T.J. (eds), Timor Sea petroleum geoscience; proceedings of the Timor Sea symposium, Darwin, Northern Territory, 2003. Northern Territory Geological Survey Special Publication 1.

MORY, A.J., 1991—Geology of the Offshore Bonaparte Basin, Northwestern Australia. Geological Survey of Western Australia Report, 29.

ROBINSON, P.H., STEAD, H.S., O’REILLY, J.B. AND GUPPY, N.K., 1994—Meanders to fans: a sequence stratigraphic approach to Upper Jurassic – Early Cretaceous sedimentation in the Sahul Syncline, north Bonaparte Basin. In: Purcell, P.G. and Purcell, R.R. (eds), The Sedimentary Basins of Western Australia, Proceedings of the Petroleum Exploration Society of Australia Symposium, Perth, 1994, 223–242.

SEGGIE, R.J., AINSWORTH, R.B., JOHNSON, D.A., KONINX, J.P.M., MARSHALL, N., MURRAY, A.P., PHILLIPS, S.E., SPAARGAREN, R. AND STEPHENSON, P.M., 2003—The Sunrise-Troubadour gas-condensate fields, Timor Sea, Australasia. In: Halbouty, M.T. (ed), Giant Oil and Gas Fields of the Decade 1990–1999, AAPG Memoir 78, 189–209.

SHUSTER, M.W., CASTILLO, D. A. AND SIMON, E., 2000—A Neogene-Recent tectonic model for the Timor Sea area, offshore Australia; geomechanical implications for charge, trap and retention. AAPG Bulletin, 84(9), 1491.

WEST, B. AND PASSMORE, V.L., 1994—Hydrocarbon potential for the Bathurst Island Group, Northeast Bonaparte Basin: implication for future exploration. The APEA Journal, 34(1), 626–643.

ZHIXIN, W., GUANGHUI, Z., LIN’AN, P. AND WENLIAN, T., 2012—An oil and gas resource assessment of the Bonaparte Basin, northwest shelf of Australia. Bulletin of Canadian Petroleum Geology, 60(3), 218-226.