Academic literature on the topic 'Structural Western Australia Roebuck Basin'

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Journal articles on the topic "Structural Western Australia Roebuck Basin"

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Abbott, Steve, Claire Orlov, George Bernardel, et al. "Stratigraphic and structural architecture across the central North West Shelf – implications for Triassic petroleum systems." APPEA Journal 59, no. 2 (2019): 832. http://dx.doi.org/10.1071/aj18154.

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The Triassic succession in the Roebuck Basin and parts of the adjacent sub-basins is the subject of a regional mapping program at Geoscience Australia that addresses stratigraphic and structural aspects of exploration risk. Seismic horizons of regional significance are integrated into a new tectonostratigraphic framework that also includes lithostratigrapy, gross depositional facies and tectonic extension phases. The main Triassic depocentre extends over the Beagle Sub-basin and north-east Exmouth Plateau, with a re-entrant into the Bedout Sub-basin. A smaller north-east oriented depocentre is
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Bradshaw, Marita. "Review of the 2008 offshore petroleum exploration release areas." APPEA Journal 48, no. 1 (2008): 359. http://dx.doi.org/10.1071/aj07025.

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Each year the Australian Government releases new offshore opportunities for petroleum exploration. Thirty-five new exploration areas located across five of Australia’s offshore sedimentary basins are offered in the 2008 Release. All the areas are available through a work program bidding system with closing dates for bids at six and 12 months from the date of release. Acreage in the first round closes on 9 October 2008 and includes the more explored areas. The second closing round on 9 April 2009 comprises acreage located in less well explored and frontier regions. The 2008 exploration areas ar
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Baillie, P. W., and E. Jacobson. "STRUCTURAL EVOLUTION OF THE CARNARVON TERRACE, WESTERN AUSTRALIA." APPEA Journal 35, no. 1 (1995): 321. http://dx.doi.org/10.1071/aj94020.

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The under-explored Carnarvon Terrace is situated offshore of the Cape Range area in the Carnarvon Basin near the boundary of the Gascoyne and Exmouth Sub-basins. The stratigraphy of the area is controlled by only two wells (Pendock-1, Yardie East-1), but several onshore wells aid interpretation of seismic data.Understanding of the structural evolution of the region is facilitated by interpretation of a high-resolution non-exclusive seismic survey acquired by Geco-Prakla in 1993 (GPCTR-93 Survey).Three major tectonic stages are responsible for the structural configuration of the region:Late Pal
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Harris, L. B. "STRUCTURAL AND TECTONIC SYNTHESIS FOR THE PERTH BASIN, WESTERN AUSTRALIA." Journal of Petroleum Geology 17, no. 2 (1994): 129–56. http://dx.doi.org/10.1111/j.1747-5457.1994.tb00123.x.

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5

Carr, Lidena, Russell Korsch, Arthur Mory, et al. "Structural and stratigraphic architecture of Australia's frontier onshore sedimentary basins: the Western Officer and Southern Carnarvon basins, Western Australia." APPEA Journal 52, no. 2 (2012): 670. http://dx.doi.org/10.1071/aj11084.

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During the past five years, the Onshore Energy Security Program, funded by the Australian Government and conducted by Geoscience Australia, in conjunction with state and territory geological surveys, has acquired deep seismic reflection data across several frontier sedimentary basins to stimulate petroleum exploration in onshore Australia. This extended abstract presents data from two seismic lines collected in Western Australia in 2011. The 487 km long Yilgarn-Officer-Musgrave (YOM) seismic line crossed the western Officer Basin in Western Australia, and the 259 km long, Southern Carnarvon Se
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Bernecker, Thomas. "Petroleum geological summary of the 2012 offshore acreage release for petroleum exploration." APPEA Journal 52, no. 1 (2012): 7. http://dx.doi.org/10.1071/aj11002.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. In 2012, 27 areas in nine offshore basins are being released for work program bidding. Closing dates for bid submissions are either six or twelve months after the release date, i.e. 8 November 2012 or 9 May 2013, depending on the exploration status in these areas and on data availability. As was the case in 2011, this year’s Release again covers a total offshore area of about 200,000 km2. The Release Areas are located in Commonwealth waters offshore Northern Territory, Western Australia,
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7

Bernecker, Tom. "The 2010 Australian offshore release for petroleum exploration." APPEA Journal 50, no. 1 (2010): 5. http://dx.doi.org/10.1071/aj09002.

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The Australian Government formally releases new offshore exploration areas at the annual APPEA conference. In 2010, thirty-one areas in five offshore basins are being released for work program bidding. Closing dates for bid submissions are either six or twelve months after the release date—i.e. 11 November 2010 and 12 May 2011—depending on the exploration status in these areas and on data availability. The 2010 release areas are located in Commonwealth waters offshore Northern Territory, Western Australia and South Australia, comprising intensively explored areas close to existing production a
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8

Olierook, H. K. H., N. E. Timms, J. F. Wellmann, S. Corbel, and P. G. Wilkes. "3D structural and stratigraphic model of the Perth Basin, Western Australia: Implications for sub-basin evolution." Australian Journal of Earth Sciences 62, no. 4 (2015): 447–67. http://dx.doi.org/10.1080/08120099.2015.1054882.

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9

Molyneux, Stephen, Jeff Goodall, Roisin McGee, George Mills, and Birgitta Hartung-Kagi. "Observations on the Lower Triassic petroleum prospectivity of the offshore Carnarvon and Roebuck basins." APPEA Journal 56, no. 1 (2016): 173. http://dx.doi.org/10.1071/aj15014.

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Why are the only commercial hydrocarbon discoveries in Lower Triassic and Permian sediments of the western margin of Australia restricted to the Perth Basin and the Petrel Sub-basin? Recent regional analysis by Carnarvon Petroleum has sought to address some key questions about the Lower Triassic Locker Shale and Upper Permian Chinty and Kennedy formations petroleum systems along the shallow water margin of the Carnarvon and offshore Canning (Roebuck/Bedout) basins. This paper aims to address the following questions:Source: Is there evidence in the wells drilled to date of a working petroleum s
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10

Carlsen, G. M., A. P. Simeonova, and S. N. Apak. "PETROLEUM SYSTEMS AND EXPLORATION POTENTIAL IN THE OFFICER BASIN, WESTERN AUSTRALIA." APPEA Journal 43, no. 1 (2003): 473. http://dx.doi.org/10.1071/aj02025.

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The Officer Basin in Western Australia contains a variety of hydrocarbon plays associated with compressional, halokinetic, unconformity and stratigraphic traps. Five distinct structural zones have been defined in the basin—a northeastern Marginal Overthrusted Zone, a northeastern Salt-ruptured Zone, a central Thrusted Zone, a Western Platform and a complex salt-dominated Minibasins Zone. These zones, together with salt-associated and sub-salt structure, are well delineated on about 2,900 km of reprocessed 1980s vintage seismic data, now publicly released.Neoproterozoic rocks are marginally to
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Dissertations / Theses on the topic "Structural Western Australia Roebuck Basin"

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Hull, Jonathan N. F. "Sequence stratigraphic evolution of the Albian to recent section of the Dampier Sub-basin, North West Shelf, Australia." Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phh9128.pdf.

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Four folded maps in pocket on back cover. Copy of author's previously published work inserted. Includes bibliographical references (9 leaves). An integrated biostratigraphic, wireline, seismic, lithological and 3D-Chronostrat sequence stratigraphic study has been conducted to investigate the evolution of the Albian to recent section of the Dampier Sub-basin on Australia's North West Shelf,.
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Smith, Stuart A. (Stuart Andrew). "The phanerozoic basin-fill history of the Roebuck Basin." 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phs6615.pdf.

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3

Waclawik, Victor G. "Landscape evolution of the Umbum Creek Catchment, Western Lake Eyre, Central Australia." 2006. http://hdl.handle.net/2440/42833.

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Landscape evolution is important for mineral and petroleum exploration concepts, especially in dryland continental settings. This study seeks to understand the main issues and controls on landscape evolution that have produced the regolith and young sediments around the western side of Lake Eye, in the arid heart of Australia. Several methods were employed including satellite image analysis, geomorphometry, geological mapping, regolith mapping and surveying. Outcomes indicate that the underlying structural fabric of the basement has controlled the development of the surface morphology of the U
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Books on the topic "Structural Western Australia Roebuck Basin"

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Iasky, R. P. A structural study of the southern Perth Basin, Western Australia. Geological Survey of Western Australia, 1993.

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2

Lockwood, A. M. Geophysical investigation of the Bernier Ridge and surrounding area, Southern Carnarvon Basin, Western Australia. Dept. of Industry and Resources, 2003.

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3

Crostella, A. (Angelo). Structural evolution and hydrocarbon potential of the Merlinleigh and Byro sub-basins, Carnarvon Basin, Western Australia. Geological Survey of Western Australia, 1995.

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4

R, Vearncombe J., ed. Tectonic, structural, and depositional controls on zinc-lead mineralisation on the Lennard Shelf, Canning Basin: Results of research carried out as MERIWA Project No. M201 in the Key Centre for Strategic Mineral Deposits, Department of Geology and Geophysics, the University of Western Australia. Minerals and Energy Research Institute of Western Australia, 1995.

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