Exploring for unconventional hydrocarbon plays in the Glyde Basin, Northern Territory, using FALCON® airborne gravity gradiometry (AGG) data
Peter Kovac A , Luke Titus B , Carlos Cevallos A and Josh Bluett BA CGG Aviation Australia.
B Armour Energy.
The APPEA Journal 54(2) 519-519 https://doi.org/10.1071/AJ13092
Published: 2014
Abstract
A FALCON® AGG and magnetic survey in the Glyde Sub-basin aims to define the structural pattern to identify unconventional hydrocarbon plays. The survey area consists of variable thick fluvial and lacustrine to shallow marginal marine carbonate-siliciclastic sequences and lesser volcanic rocks. The dominant tectonic feature identified on the AGG data is the Emu Fault Zone: a major structure of the central-southern part of the McArthur Basin. Seismic and surface geology suggest its overall sub-vertical strike-slip nature with positive flower structure geometry. In the north, a regional size pop-up structure, reverse, transpressional and strike-slip faults, and abundant synclines and anticlines identified in the AGG data indicate sinistral transpression. In the south, a transtensional segment of the Emu Fault Zone formed several regularly oriented, fault-controlled depocentres. A geological cross-section across the Glyde Sub-basin supported by gravity modelling indicates a system of inverted transtensional faults. Offsets and bifurcations are common, forming local-scale transtensional or transpressional areas. The relationship between dolomitic carbonaceous siltstone, fault-related hydrothermal dolomite (HTD) and the tectonic pattern strongly suggests that the Emu Fault Zone controlled fluid migration and fault-related HTD deposition. Brecciated HTD reservoirs are best developed where a combination of strike-slip movement and extension allowed dolomitising and porosity-generating fluids to migrate along fracture networks, especially in transtensional pull-apart structures and along the principal faults bounding elevated parts of the basement. This is consistent with the results of the Glyde–1 ST1 exploration well, which drilled 122 m of gas charged dolomitic breccia.
Peter Kovac is a Senior Interpreting Geologist at CGG Aviation Pty Ltd in Perth, Australia. His primary field of interest is structural geology and compilation of regional and prospect scale geological models. He holds an MSc in geology and palaeontology and a PhD in structural geology from the Comenius University at Bratislava, Slovakia. Member: PESA and AusIMM. |
Luke Titus is the Chief Geologist for Armour Energy. Luke received a Bachelor of Science in geology in 1997 from Fort Lewis College in Colorado. He has 16 years of exploration and development experience in major US and international petroleum basins. Luke has worked carbonate, tight sands, coalbed methane plays and shale plays throughout the Rocky Mountain and Mid-Continent Basins in the US before being hired in 2010 with QGC as a Principal Geologist in Upstream Subsurface Developments where he was responsible for reserve growth in the Surat Basin in Queensland, Australia. Member: AAPG. |
Carlos Cevallos is a Senior Interpreting Geophysicist at CGG Aviation Pty Ltd in Perth, Australia. His previous work was at the Geological Survey of NSW, Noranda and The University of Queensland. He is a physicist whose interests are to integrate geological and geophysical data and find new ways to interpret potential field data. He holds a BSc degree from UNAM, Mexico, a MSc degree from CICESE, Mexico, and a PhD degree from Macquarie University in Australia. |
Josh Bluett is a Petroleum Geologist at Armour Energy and holds a Bachelor degree in geoscience from the Queensland University of Technology. He has four years’ petroleum exploration experience, working for MBA Petroleum Consultants (now AWT International) before joining Armour Energy. Josh has undertaken geological and geophysical analysis on a large number of Australian onshore hydrocarbon plays, and has been involved with the definition and maturation of Armour Energy’s exploration portfolio since the company’s inception. Member: PESA, AAPG and SPE. |
References
Bull, S., and Scott, R. 1998—Geology of the BCDC in the Myrtle Basin area, southern McArthur Basin, Northern Territory. CODES/AMIRA/ARC Project P384A, Final Report. Proterozoic sediment-hosted base metal deposits, 2, 9–39.Cevallos, C., Kovac, P., and Lowe, S. (2013). Application of curvatures to airborne gravity gradient data in oil exploration. Geophysics 79, 81–8.
Davidson, G.J., and Dashlooty, S.A. (1993). The Glyde Sub-basin: A volcaniclastic-bearing pull-apart basin coeval with the McArthur River base-metal deposit, Northern Territory. Australian Journal of Earth Sciences 40, 527–43.
Etheridge, M., and Wall, V., 1994—Tectonic and structural evolution of the Australian Proterozoic. In: 12th Australian Geological Convention, Geological Society of Australia, Abstracts, 17, 131–47.
Harding, T.P., and Dashlooty, S.A. (1974). Petroleum traps associated with wrench faults. American Association of Petroleum Geologists Bulletin 58, 1290–304.
Hinman, M., 1995—Base metal mineralisation at McArthur River: structure and kinematics of the HYC-Co0ley zone at McArthur River. Australian Geological Survey Organisation, Record 1995/5. Canberra: Australian Geological Survey Organisation.
Hinman, M., 1996—Timing and processes of formation of the McArthur River Zn-Pb-Ag deposit, McArthur River. In: Baker, T., Rotherham, J.F., Richmond, J.M., Mark, G., and Williams, P.J., (ed.) New Developments in Metallogenic Research: The McArthur-Mount Isa-Cloncurry Minerals Province, James Cook University, Economic Geology Research Unit, Extended Abstracts, EGRU Contribution, 55, 56–9.
Korsch, R.J., Goleby, B.R, Rawlings, D.J., Gibson, G.M., and Johnstone, D.W., 2005—The 2002 Southern McArthur Basin Seismic Reflection Survey: The Anglo American Seismic Traverse (02GA-BT2). Geoscience Australia, Record 2005/01, 1–37. Canberra: Geoscience Australia.
Leaman, D.E. (1998). Structure, contents and setting of Pb-Zn mineralisation in the McArthur Basin, northern Australia. Australian Journal of Earth Sciences 45, 3–20.
MBA Petroleum Consultants, 2011—Armour Energy Conventional and Unconventional Prospective Resource Estimate EP 171 & EP 176. 1–58. Queensland: MBA Petroleum Consultants.
Pietsch, B.A., Rawlings, D.J., Creaser, P.M., Kruse, P.D., Ahmad, M., Ferenczi, P.A., and Findhammer, T.L.R., 1991—Explanatory notes to Bauhinia Downs SE53–3 1:250 000 Geological map series. Northern Territory Geological Survey, 1–78. NT: Northern Territory Geological Survey.
Plumb, K.A. (1979). Structure and tectonic style of the Precambrian shields and platforms of northern Australia. Tectonophysics 58, 291–325.
Rawlings, D.J., Korsch, R.J., Goleby, B.R., Gibson, G.M., Johnstone, D.W., and Barlow, M., 2004—The 2002 Southern McArthur Basin Seismic Reflection Survey. Geoscience Australia, Record 2004/17, 1–78. Canberra: Geoscience Australia.
Scott, D.L., Rawlings, D.J., Page, R.W., Tarlowski, C.Z., Indrum, M., Jackson, M.J., and Southgate, P.N., 2000—Basement framework and geodynamic evolution of the Palaeoproterozoic superbasins of north-central Australia; an integrated review of geochemical, geochronological and geophysical data. In: Southgate P.N. (ed.) Carpentaria-Mt. Isa Belt; Basement Framework, Chronostratigraphy and Geodynamic Evolution of Proterozoic Successions. Australian Journal of Earth Sciences, 47, 341–80.
Selley, D., Winefield, P., Bull, S., Scott, R., and McGoldrick, P. (2001). Sub-basins, depositional cycles and the tectono-sedimentary setting of the HYC Zn-Pb-Ag deposit. Geological Society of America, Abstracts 33, 270–1.